Article(id=1149781954989613976, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1149781952959574654, articleNumber=null, orderNo=null, doi=10.12404/j.issn.1671-1815.2403118, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=research-article, receivedDate=1714060800000, receivedDateStr=2024-04-26, revisedDate=1734537600000, revisedDateStr=2024-12-19, acceptedDate=null, acceptedDateStr=null, onlineDate=1752058979985, onlineDateStr=2025-07-09, pubDate=1743091200000, pubDateStr=2025-03-28, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1752058979985, onlineIssueDateStr=2025-07-09, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1752058979985, creator=13701087609, updateTime=1752058979985, updator=13701087609, issue=Issue{id=1149781952959574654, tenantId=1146029695717560320, journalId=1146123166801305609, year='2025', volume='25', issue='9', pageStart='3529', pageEnd='3967', issueExtLink='null', onlineDate='null', pubDate='null', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=0, createTime=1752058979501, creator=13701087609, updateTime=1776333392421, updator=13701087609, preIssue=null, nextIssue=null, ext={EN=IssueExt(id=1251596220226027613, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1149781952959574654, language=EN, specialIssueTitle=, coverIllustrator=, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1251596220226027614, tenantId=1146029695717560320, journalId=1146123166801305609, issueId=1149781952959574654, language=CN, specialIssueTitle=, coverIllustrator=, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null}, startPage=3555, endPage=3572, ext={EN=ArticleExt(id=1149781955295798171, articleId=1149781954989613976, tenantId=1146029695717560320, journalId=1146123166801305609, language=EN, title=Molybdenite Re-Os and Zircon U-Pb Chronology of Tanshuling Molybdenum Deposits from Jingxian County, Southern Anhui Province and Its Geological Significance, columnId=1156262729351549255, journalTitle=Science Technology and Engineering, columnName=Papers·Astronomy and Geosciences, runingTitle=null, highlight=null, articleAbstract=

The Tanshuling molybdenum deposit is located in the Jiangnan Uplift zone along south part of the Jiangnan Fault. Its main lithology type is granodiorite. With the aim to constrain their magma and ore-forming ages and deposit genesis, combined zircon U-Pb and molybdenite Re-Os geochronology together with whole-rock major and trace element geochemistry have been carried out. The result suggest that the content of SiO2 is 64.5%~66.8%, Al2O3 is 14.4%~16.0%, K2O is 3.92%~4.86%, Na2O is 2.90%~3.91%, CaO is 1.56%~2.8%, MgO is 1.24%~1.53%, A/CNK value of 1.02~1.10, and A/NK value of 1.37~1.59. The characteristics of major elements show that the granites belong to metaaluminium to weak peraluminous high potassium calc-alkaline pot-assium series with I-type granite nature. The chondrite-normalized REE patterns are evidently right-declined, with relatively LREE enrichment and slight Eu negative anomalies. The molybdenite Re-Os age of the Tanshuling molybdenite is (133.09±0.86) Ma, and the U-Pb dating of the Maolin granodiorite is (140.4±0.62) Ma, (139.9±0.66) Ma, (139.6±0.63) Ma, all belong to the Early Cretaceous. Integrated chronological and geochemical characteristics show that the main magmatic activity of the Tanshuling molybdenum deposit belong to the Pacific tectonic system, and the alternation of extrusion and extensional has led to large-scale magmatic and mineralization in this area.

, correspAuthors=An-dong WANG, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, authorCompany=null, fund=null, authors=null, authorsList=Jiu-qing MU, An-dong WANG, Fang-yue WANG, Yun WANG), CN=ArticleExt(id=1149781996056043594, articleId=1149781954989613976, tenantId=1146029695717560320, journalId=1146123166801305609, language=CN, title=皖南泾县檀树岭钼矿床辉钼矿Re-Os和锆石U-Pb年代学及其地质意义, columnId=1156262730077163858, journalTitle=科学技术与工程, columnName=论文·天文学、地球科学, runingTitle=null, highlight=null, articleAbstract=

檀树岭钼矿床处于江南隆起带内,位于江南断裂的南侧,其主体岩性为花岗闪长岩。为限定其成岩成矿时代和矿床成因,对其开展了锆石U-Pb年代学、辉钼矿Re-Os年代学和全岩主微量元素地球化学研究。结果表明:檀树岭花岗岩SiO2含量为64.5%~66.8%,Al2O3含量为14.4%~16.0%,K2O含量为3.92%~4.86%,Na2O含量为2.90%~3.91%,CaO含量为1.56%~2.8%,MgO含量为1.24%~1.53%,A/CNK为1.02~1.10,A/NK为1.37~1.59,主量元素特征显示其属于准铝质-弱过铝质高钾钙碱性-钾玄岩系列的I型花岗岩。稀土元素球粒陨石标准化曲线明显右倾,轻稀土相对富集,Eu负异常。檀树岭辉钼矿的Re-Os定年结果为(133.09±0.86) Ma,茂林岩体花岗闪长岩的U-Pb定年结果为(140.4±0.62) Ma、(139.9±0.66) Ma、(139.6±0.63) Ma,均属于早白垩世。综合年代学和地球化学结果可见檀树岭钼矿床主要岩浆活动属于太平洋构造体制,挤压与伸展的相互交替使该地区发生了大规模的岩浆与成矿作用。

, correspAuthors=王安东, authorNote=null, correspAuthorsNote=
* 王安东(1985—),男,汉族,安徽安庆人,博士,副教授。研究方向:同位素地球化学、地热学。E-mail:
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穆玖清(1999—),男,汉族,河北唐山人,硕士研究生。研究方向:同位素地球化学。E-mail:

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Geological Review, 2016, 62(6): 1549-1564., articleTitle=Zircon LA-ICP-MS U-Pb ages and geochemical features of tai ping Pluton in south Anhui: enlightment of mesozoic lithospheric thinning for south China, refAbstract=null)], funds=[Fund(id=1251249374941102672, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, awardId=41763005, language=CN, fundingSource=国家自然科学基金(41763005), fundOrder=null, country=null), Fund(id=1251249375050154583, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, awardId=2018YFA0404104, language=CN, fundingSource=国家重点研发计划(2018YFA0404104), fundOrder=null, country=null), Fund(id=1251249375159206495, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, awardId=RGET2209, language=CN, fundingSource=放射性地质与勘探技术国防重点学科实验室项目(RGET2209), fundOrder=null, country=null)], companyList=[AuthorCompany(id=1251249361150231304, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, xref=1, ext=[AuthorCompanyExt(id=1251249361158619913, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361150231304, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=1 State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China), AuthorCompanyExt(id=1251249361171202826, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361150231304, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=1 东华理工大学核资源与环境省部共建国家重点实验室培育基地, 南昌 330013)]), AuthorCompany(id=1251249361322197791, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, xref=2, ext=[AuthorCompanyExt(id=1251249361330586400, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361322197791, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=2 School of Earth Sciences, East China University of Technology, Nanchang 330013, China), AuthorCompanyExt(id=1251249361338975009, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361322197791, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=2 东华理工大学地球科学学院, 南昌 330013)]), AuthorCompany(id=1251249361468998451, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, xref=3, ext=[AuthorCompanyExt(id=1251249361473192756, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361468998451, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=3 The Fifth Geological Brigade of Hebei Bureau of Geology and Mineral Resources, Tangshan 063006, China), AuthorCompanyExt(id=1251249361481581366, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361468998451, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=3 河北省地矿局第五地质大队, 唐山 063006)]), AuthorCompany(id=1251249361586438982, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, xref=4, ext=[AuthorCompanyExt(id=1251249361594827590, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361586438982, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=4 School of Resource and Environmental Engineering, Hefei University of Technology, Hefei 230009, China), AuthorCompanyExt(id=1251249361599021897, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, companyId=1251249361586438982, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=4 合肥工业大学资源与环境工程学院, 合肥 230009)])], figs=[ArticleFig(id=1251249366460219537, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Fig.1, caption=Tectonic location and geological sketch map of the study area[20], figureFileSmall=geAo87gaixKZWznk4xm0sg==, figureFileBig=2rCe3gEbPue7uXpBdIrTxw==, tableContent=null), ArticleFig(id=1251249366602825887, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=图1, caption=研究区位置图及分布简图[20]

GTF为高坦断裂;ZWF为周王断裂;JNF为江南断裂;GBF为赣东北—白际山断裂;JSF为江绍断裂;QQF为祁门—潜江断裂

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Qz为石英;Pl为斜长石;Bt为黑云母;Py为黄铁矿;Ap为磷灰石;Mol为辉钼矿

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稀土元素标准值参考文献[32]

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底图及往年数据参考文献[19,59-61]

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Re-Os isotope data of molybdenite from Tanshuling molybdenum deposit

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样品 样重/g Re/10-6 普Os/10-9 187Re/10-6 187Os/10-9 模式年龄/Ma
测定值 不确定度 测定值 不确定度 测定值 不确定度 测定值 不确定度 测定值 不确定度
M-1-1 0.010 21 46.162 0.447 0.379 6 0.106 2 29.014 0.281 64.09 0.54 132.4 2.1
M-1-2 0.010 18 49.285 0.508 0.421 6 0.026 6 30.977 0.319 69.00 1.28 133.6 3.1
M-1-3 0.020 31 22.406 0.214 0.161 9 0.005 3 14.083 0.135 31.28 0.35 133.2 2.4
M-2 0.010 04 49.358 0.486 0.469 3 0.000 9 31.022 0.306 68.40 1.03 132.2 2.7
M-3 0.010 09 50.294 0.510 2.514 5 0.238 5 31.611 0.321 70.27 0.82 133.3 2.4
M-4 0.350 22 0.601 0.004 6 0.017 3 0.003 8 3.781 0.002 9 0.841 6 0.018 1 133.4 3.3
M-6 0.010 06 91.486 1.333 0.532 8 0.039 6 57.501 0.838 127.2 0.80 132.6 2.5
M-8 0.010 19 27.002 0.255 0.600 0 0.058 7 16.971 0.160 37.92 0.27 134.0 2.1
), ArticleFig(id=1251249371573076405, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表1, caption=

檀树岭钼矿床辉钼矿Re-Os同位素结果

, figureFileSmall=null, figureFileBig=null, tableContent=
样品 样重/g Re/10-6 普Os/10-9 187Re/10-6 187Os/10-9 模式年龄/Ma
测定值 不确定度 测定值 不确定度 测定值 不确定度 测定值 不确定度 测定值 不确定度
M-1-1 0.010 21 46.162 0.447 0.379 6 0.106 2 29.014 0.281 64.09 0.54 132.4 2.1
M-1-2 0.010 18 49.285 0.508 0.421 6 0.026 6 30.977 0.319 69.00 1.28 133.6 3.1
M-1-3 0.020 31 22.406 0.214 0.161 9 0.005 3 14.083 0.135 31.28 0.35 133.2 2.4
M-2 0.010 04 49.358 0.486 0.469 3 0.000 9 31.022 0.306 68.40 1.03 132.2 2.7
M-3 0.010 09 50.294 0.510 2.514 5 0.238 5 31.611 0.321 70.27 0.82 133.3 2.4
M-4 0.350 22 0.601 0.004 6 0.017 3 0.003 8 3.781 0.002 9 0.841 6 0.018 1 133.4 3.3
M-6 0.010 06 91.486 1.333 0.532 8 0.039 6 57.501 0.838 127.2 0.80 132.6 2.5
M-8 0.010 19 27.002 0.255 0.600 0 0.058 7 16.971 0.160 37.92 0.27 134.0 2.1
), ArticleFig(id=1251249371686322619, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 2, caption=

Zircon LA-ICP-MS trace element data of Tanshuling molybdenum deposit(S1)

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点号 含量/10-6
Ti Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy
s1-1 4.30 776 3.89 0.18 33.1 0.07 1.56 2.48 0.78 12.7 4.07 59.0
s1-2 51.00 1 005 3.71 10.30 45.7 2.96 10.70 4.53 0.95 16.6 6.26 75.4
s1-3 7.49 1 199 5.17 0.03 36.5 0.03 1.56 2.65 1.17 18.8 6.71 99.2
s1-4 10.10 1 087 7.31 10.20 65.0 2.56 8.41 3.99 1.03 17.4 5.91 84.5
s1-5 1.67 862 4.47 0.01 34.4 0.01 0.27 1.60 0.62 12.0 4.42 61.9
s1-6 6.88 1 056 2.56 1.55 25.6 0.40 2.51 3.69 1.22 18.7 6.62 87.2
s1-7 6.59 1 367 6.43 5.57 40.4 1.09 5.78 5.16 1.12 20.8 7.96 105.0
s1-8 8.06 1 121 4.32 9.48 53.7 3.12 13.90 6.74 1.24 16.9 6.51 83.5
s1-9 2.89 838 3.55 0.60 32.2 0.16 1.54 2.16 0.66 13.2 4.67 62.0
s1-10 2.86 775 3.98 0.44 33.7 0.11 1.28 1.45 0.56 10.8 3.67 51.5
s1-11 4.78 1 374 9.94 0.47 44.5 0.27 1.87 2.67 1.04 20.4 8.35 102.0
s1-12 0.62 868 4.45 0.13 25.0 0.05 0.92 2.13 0.75 10.8 4.57 59.7
s1-13 6.94 901 3.97 8.11 43.8 2.53 11.70 4.65 0.99 15.3 4.98 62.5
s1-14 5.15 1 119 2.53 0.04 24.8 0.06 1.78 4.15 1.15 19.0 6.76 81.3
s1-15 4.14 1314 5.27 0.69 37.3 0.29 2.14 3.27 1.20 19.2 8.33 98.9
s1-16 2.99 1 324 3.84 4.40 38.0 1.13 6.21 5.67 1.59 25.3 8.87 99.5
s1-17 11.70 1 299 3.40 0.28 31.8 0.23 2.83 5.26 1.61 27.3 9.68 107.0
点号 含量/10-6 L/H δEu δCe
Ho Er Tm Yb Lu Hf Ta Pb ΣREE
s1-1 22.7 120 29.6 316 72.4 12 481 1.50 15.80 674 0.06 0.34 71.36
s1-2 30.8 152 37.1 379 81.0 11 904 1.78 10.90 854 0.10 0.30 1.98
s1-3 36.7 187 45.6 476 99.8 12 540 2.18 14.30 1 012 0.04 0.37 264.72
s1-4 32.5 173 42.6 447 97.8 13 018 2.26 18.80 992 0.10 0.32 3.01
s1-5 25.8 136 33.0 364 84.2 12 703 1.94 17.90 758 0.05 0.31 747.38
s1-6 33.7 166 39.6 394 84.0 11 424 1.06 7.53 864 0.04 0.36 7.70
s1-7 43.1 218 52.0 524 114.0 12 186 2.35 19.40 1 145 0.05 0.29 3.74
s1-8 35.3 179 42.8 440 92.9 12 808 1.96 12.20 984 0.10 0.34 2.38
s1-9 26.0 135 30.9 317 71.1 12 671 2.21 12.30 698 0.06 0.29 24.69
s1-10 22.2 121 30.8 332 77.3 12 771 1.72 13.20 687 0.06 0.31 36.17
s1-11 42.3 222 52.3 530 117.0 12 751 3.90 25.20 1 145 0.05 0.31 29.64
s1-12 25.4 137 34.6 360 78.0 13 121 1.95 11.50 740 0.04 0.39 74.99
s1-13 27.4 149 34.2 368 77.4 12 930 2.29 11.80 810 0.10 0.32 2.32
s1-14 33.5 176 39.9 398 86.8 11 985 1.66 8.54 873 0.04 0.33 99.32
s1-15 39.6 213 48.4 487 103.0 12 139 1.61 16.40 1062 0.04 0.36 20.18
s1-16 40.8 216 50.4 507 107.0 12 674 1.44 13.20 1 112 0.05 0.34 4.03
s1-17 40.8 201 41.8 416 86.8 12 865 1.23 12.60 972 0.05 0.33 28.34
), ArticleFig(id=1251249371858289098, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表2, caption=

檀树岭钼矿床锆石LA-ICP-MS微量元素数据(S1)

, figureFileSmall=null, figureFileBig=null, tableContent=
点号 含量/10-6
Ti Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy
s1-1 4.30 776 3.89 0.18 33.1 0.07 1.56 2.48 0.78 12.7 4.07 59.0
s1-2 51.00 1 005 3.71 10.30 45.7 2.96 10.70 4.53 0.95 16.6 6.26 75.4
s1-3 7.49 1 199 5.17 0.03 36.5 0.03 1.56 2.65 1.17 18.8 6.71 99.2
s1-4 10.10 1 087 7.31 10.20 65.0 2.56 8.41 3.99 1.03 17.4 5.91 84.5
s1-5 1.67 862 4.47 0.01 34.4 0.01 0.27 1.60 0.62 12.0 4.42 61.9
s1-6 6.88 1 056 2.56 1.55 25.6 0.40 2.51 3.69 1.22 18.7 6.62 87.2
s1-7 6.59 1 367 6.43 5.57 40.4 1.09 5.78 5.16 1.12 20.8 7.96 105.0
s1-8 8.06 1 121 4.32 9.48 53.7 3.12 13.90 6.74 1.24 16.9 6.51 83.5
s1-9 2.89 838 3.55 0.60 32.2 0.16 1.54 2.16 0.66 13.2 4.67 62.0
s1-10 2.86 775 3.98 0.44 33.7 0.11 1.28 1.45 0.56 10.8 3.67 51.5
s1-11 4.78 1 374 9.94 0.47 44.5 0.27 1.87 2.67 1.04 20.4 8.35 102.0
s1-12 0.62 868 4.45 0.13 25.0 0.05 0.92 2.13 0.75 10.8 4.57 59.7
s1-13 6.94 901 3.97 8.11 43.8 2.53 11.70 4.65 0.99 15.3 4.98 62.5
s1-14 5.15 1 119 2.53 0.04 24.8 0.06 1.78 4.15 1.15 19.0 6.76 81.3
s1-15 4.14 1314 5.27 0.69 37.3 0.29 2.14 3.27 1.20 19.2 8.33 98.9
s1-16 2.99 1 324 3.84 4.40 38.0 1.13 6.21 5.67 1.59 25.3 8.87 99.5
s1-17 11.70 1 299 3.40 0.28 31.8 0.23 2.83 5.26 1.61 27.3 9.68 107.0
点号 含量/10-6 L/H δEu δCe
Ho Er Tm Yb Lu Hf Ta Pb ΣREE
s1-1 22.7 120 29.6 316 72.4 12 481 1.50 15.80 674 0.06 0.34 71.36
s1-2 30.8 152 37.1 379 81.0 11 904 1.78 10.90 854 0.10 0.30 1.98
s1-3 36.7 187 45.6 476 99.8 12 540 2.18 14.30 1 012 0.04 0.37 264.72
s1-4 32.5 173 42.6 447 97.8 13 018 2.26 18.80 992 0.10 0.32 3.01
s1-5 25.8 136 33.0 364 84.2 12 703 1.94 17.90 758 0.05 0.31 747.38
s1-6 33.7 166 39.6 394 84.0 11 424 1.06 7.53 864 0.04 0.36 7.70
s1-7 43.1 218 52.0 524 114.0 12 186 2.35 19.40 1 145 0.05 0.29 3.74
s1-8 35.3 179 42.8 440 92.9 12 808 1.96 12.20 984 0.10 0.34 2.38
s1-9 26.0 135 30.9 317 71.1 12 671 2.21 12.30 698 0.06 0.29 24.69
s1-10 22.2 121 30.8 332 77.3 12 771 1.72 13.20 687 0.06 0.31 36.17
s1-11 42.3 222 52.3 530 117.0 12 751 3.90 25.20 1 145 0.05 0.31 29.64
s1-12 25.4 137 34.6 360 78.0 13 121 1.95 11.50 740 0.04 0.39 74.99
s1-13 27.4 149 34.2 368 77.4 12 930 2.29 11.80 810 0.10 0.32 2.32
s1-14 33.5 176 39.9 398 86.8 11 985 1.66 8.54 873 0.04 0.33 99.32
s1-15 39.6 213 48.4 487 103.0 12 139 1.61 16.40 1062 0.04 0.36 20.18
s1-16 40.8 216 50.4 507 107.0 12 674 1.44 13.20 1 112 0.05 0.34 4.03
s1-17 40.8 201 41.8 416 86.8 12 865 1.23 12.60 972 0.05 0.33 28.34
), ArticleFig(id=1251249372034449878, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 3, caption=

Zircon LA-ICP-MS trace element data of Tanshuling molybdenum deposit(S2)

, figureFileSmall=null, figureFileBig=null, tableContent=
点号 含量/10-6
Ti Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy
s2-1 0.98 762 4.19 1.03 27.8 0.31 1.45 1.62 0.70 12.4 4.47 57.6
s2-5 16.00 879 2.97 17.3 0.36 7.48 18.00 4.54 76.0 16.20 121.0
s2-7 3.96 692 2.36 4.44 28.5 1.19 4.62 2.49 0.49 12.5 3.61 53.9
s2-8 12.40 978 2.31 3.07 34.0 1.19 6.54 3.23 1.08 20.5 5.81 79.1
s2-9 741 4.17 22.9 0.02 0.31 0.78 0.50 9.6 3.85 51.2
s2-11 1.85 1 401 9.06 0.01 32.0 0.08 0.31 3.84 1.23 21.4 8.04 111.0
s2-12 6.67 916 4.75 0.51 23.6 0.17 1.57 0.86 0.82 11.2 4.71 64.3
s2-15 2.79 1 400 15.10 0.33 36.6 0.12 1.77 3.71 0.85 23.3 7.84 101.0
s2-16 4.25 1 304 7.86 0.01 33.8 0.03 0.99 2.73 0.83 20.6 7.21 96.3
s2-18 8.84 1 610 3.71 0.93 33.5 0.39 3.47 4.50 1.14 30.1 10.40 125.0
s2-19 6.52 1 765 3.09 10.60 50.8 3.02 19.40 10.60 3.22 41.6 14.10 154.0
s2-20 0.59 713 2.62 21.7 0.01 0.81 1.39 0.50 10.2 3.70 51.3
s2-21 0.95 772 2.98 2.82 25.2 0.45 1.28 2.04 0.64 10.4 4.04 52.4
s2-22 2.99 832 4.58 5.81 38.2 1.45 6.13 2.19 0.77 10.9 4.84 61.1
s2-23 3.16 884 5.30 3.88 35.2 1.14 5.03 2.27 0.64 11.6 4.83 63.9
s2-24 11.30 1 093 5.52 1.31 32.7 0.21 2.26 2.36 0.95 13.6 5.22 69.1
s2-25 2.79 705 3.68 0.11 23.7 0.03 0.17 1.12 0.54 8.9 3.65 46.4
s2-26 4.21 799 4.05 2.35 37.6 0.43 3.19 2.88 0.53 11.9 4.53 59.7
点号 含量/10-6 L/H δEu δCe
Ho Er Tm Yb Lu Hf Ta Pb ΣREE
s2-1 23.4 125.0 29.3 325 66.7 13 202 2.27 10.10 677 0.05 0.34 11.79
s2-5 27.6 83.8 14.4 110 15.5 10 687 0.45 4.04 512 0.10 0.32
s2-7 20.9 105.0 27.9 304 64.0 12 988 1.31 8.33 634 0.07 0.22 2.95
s2-8 29.7 148.0 33.5 332 66.0 11 319 1.00 5.05 763 0.07 0.31 4.30
s2-9 21.9 115.0 29.8 337 73.8 13 126 1.73 10.20 667 0.04 0.33
s2-11 43.7 225.0 55.1 584 122.0 12 179 2.20 13.80 1 208 0.03 0.33 115.28
s2-12 28.2 143.0 37.2 411 86.5 12 296 1.58 8.50 814 0.04 0.47 19.36
s2-15 42.3 214.0 50.4 516 103.0 12 167 2.67 16.50 1 101 0.04 0.21 44.48
s2-16 41.2 211.0 51.2 543 115.0 12 259 2.58 12.80 1 125 0.04 0.24 301.83
s2-18 48.9 243.0 56.1 571 118.0 11 929 2.06 17.40 1 246 0.04 0.22 13.46
s2-19 57.4 276.0 58.2 565 114.0 11 399 1.23 10.70 1 378 0.08 0.41 2.15
s2-20 22.1 116.0 28.6 308 74.0 13 553 1.54 10.00 639 0.04 0.29
s2-21 23.0 126.0 31.1 342 78.8 13 395 1.29 12.30 700 0.05 0.34 4.90
s2-22 26.0 131.0 31.1 332 73.3 12 871 2.11 10.30 724 0.08 0.39 3.10
s2-23 27.1 148.0 35.0 363 84.1 12 393 1.90 10.30 786 0.07 0.31 4.00
s2-24 30.4 177.0 42.3 461 109.0 11 560 1.67 13.20 948 0.04 0.40 13.70
s2-25 21.3 118.0 29.1 325 79.5 12 918 1.77 9.80 657 0.04 0.37 98.28
s2-26 23.9 134.0 30.6 326 76.8 12 816 1.89 14.00 714 0.07 0.24 8.43
), ArticleFig(id=1251249373229826526, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表3, caption=

檀树岭钼矿床锆石LA-ICP-MS微量元素数据(S2)

, figureFileSmall=null, figureFileBig=null, tableContent=
点号 含量/10-6
Ti Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy
s2-1 0.98 762 4.19 1.03 27.8 0.31 1.45 1.62 0.70 12.4 4.47 57.6
s2-5 16.00 879 2.97 17.3 0.36 7.48 18.00 4.54 76.0 16.20 121.0
s2-7 3.96 692 2.36 4.44 28.5 1.19 4.62 2.49 0.49 12.5 3.61 53.9
s2-8 12.40 978 2.31 3.07 34.0 1.19 6.54 3.23 1.08 20.5 5.81 79.1
s2-9 741 4.17 22.9 0.02 0.31 0.78 0.50 9.6 3.85 51.2
s2-11 1.85 1 401 9.06 0.01 32.0 0.08 0.31 3.84 1.23 21.4 8.04 111.0
s2-12 6.67 916 4.75 0.51 23.6 0.17 1.57 0.86 0.82 11.2 4.71 64.3
s2-15 2.79 1 400 15.10 0.33 36.6 0.12 1.77 3.71 0.85 23.3 7.84 101.0
s2-16 4.25 1 304 7.86 0.01 33.8 0.03 0.99 2.73 0.83 20.6 7.21 96.3
s2-18 8.84 1 610 3.71 0.93 33.5 0.39 3.47 4.50 1.14 30.1 10.40 125.0
s2-19 6.52 1 765 3.09 10.60 50.8 3.02 19.40 10.60 3.22 41.6 14.10 154.0
s2-20 0.59 713 2.62 21.7 0.01 0.81 1.39 0.50 10.2 3.70 51.3
s2-21 0.95 772 2.98 2.82 25.2 0.45 1.28 2.04 0.64 10.4 4.04 52.4
s2-22 2.99 832 4.58 5.81 38.2 1.45 6.13 2.19 0.77 10.9 4.84 61.1
s2-23 3.16 884 5.30 3.88 35.2 1.14 5.03 2.27 0.64 11.6 4.83 63.9
s2-24 11.30 1 093 5.52 1.31 32.7 0.21 2.26 2.36 0.95 13.6 5.22 69.1
s2-25 2.79 705 3.68 0.11 23.7 0.03 0.17 1.12 0.54 8.9 3.65 46.4
s2-26 4.21 799 4.05 2.35 37.6 0.43 3.19 2.88 0.53 11.9 4.53 59.7
点号 含量/10-6 L/H δEu δCe
Ho Er Tm Yb Lu Hf Ta Pb ΣREE
s2-1 23.4 125.0 29.3 325 66.7 13 202 2.27 10.10 677 0.05 0.34 11.79
s2-5 27.6 83.8 14.4 110 15.5 10 687 0.45 4.04 512 0.10 0.32
s2-7 20.9 105.0 27.9 304 64.0 12 988 1.31 8.33 634 0.07 0.22 2.95
s2-8 29.7 148.0 33.5 332 66.0 11 319 1.00 5.05 763 0.07 0.31 4.30
s2-9 21.9 115.0 29.8 337 73.8 13 126 1.73 10.20 667 0.04 0.33
s2-11 43.7 225.0 55.1 584 122.0 12 179 2.20 13.80 1 208 0.03 0.33 115.28
s2-12 28.2 143.0 37.2 411 86.5 12 296 1.58 8.50 814 0.04 0.47 19.36
s2-15 42.3 214.0 50.4 516 103.0 12 167 2.67 16.50 1 101 0.04 0.21 44.48
s2-16 41.2 211.0 51.2 543 115.0 12 259 2.58 12.80 1 125 0.04 0.24 301.83
s2-18 48.9 243.0 56.1 571 118.0 11 929 2.06 17.40 1 246 0.04 0.22 13.46
s2-19 57.4 276.0 58.2 565 114.0 11 399 1.23 10.70 1 378 0.08 0.41 2.15
s2-20 22.1 116.0 28.6 308 74.0 13 553 1.54 10.00 639 0.04 0.29
s2-21 23.0 126.0 31.1 342 78.8 13 395 1.29 12.30 700 0.05 0.34 4.90
s2-22 26.0 131.0 31.1 332 73.3 12 871 2.11 10.30 724 0.08 0.39 3.10
s2-23 27.1 148.0 35.0 363 84.1 12 393 1.90 10.30 786 0.07 0.31 4.00
s2-24 30.4 177.0 42.3 461 109.0 11 560 1.67 13.20 948 0.04 0.40 13.70
s2-25 21.3 118.0 29.1 325 79.5 12 918 1.77 9.80 657 0.04 0.37 98.28
s2-26 23.9 134.0 30.6 326 76.8 12 816 1.89 14.00 714 0.07 0.24 8.43
), ArticleFig(id=1251249373351461348, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 4, caption=

Zircon LA-ICP-MS trace element data of Tanshuling molybdenum deposit(S4)

, figureFileSmall=null, figureFileBig=null, tableContent=
点号 含量/10-6
Ti Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy
s4-1 802 4.66 10.70 45.7 4.27 14.70 4.20 0.88 13.70 4.05 54.0
s4-2 876 5.31 0.05 32.9 0.02 1.15 1.77 0.53 13.50 4.37 61.2
s4-3 1.54 689 3.27 0.87 28.2 0.28 1.14 1.31 0.49 11.70 3.28 46.2
s4-4 4.03 1 139 6.19 0.01 39.1 0.03 0.45 1.50 1.37 18.90 6.66 80.4
s4-5 10.40 1 342 3.52 0.08 28.3 0.25 2.80 4.08 1.12 26.90 8.34 104.0
s4-6 6.41 922 4.53 0.02 29.2 0.05 0.26 3.29 0.77 16.20 5.83 73.7
s4-7 0.86 1 069 2.58 0.04 25.9 0.16 2.12 4.47 1.55 21.80 7.05 85.7
s4-9 3.18 868 3.40 3.08 28.2 0.98 4.08 2.42 0.99 12.60 4.47 63.9
s4-10 7.24 690 2.76 4.06 30.9 0.93 3.99 2.08 0.49 13.00 4.40 51.2
s4-12 5.19 1 277 5.12 1.42 37.9 0.54 3.67 3.22 1.07 17.60 7.31 90.4
s4-13 2.88 964 5.61 3.01 47.5 0.43 2.44 2.47 0.77 14.70 5.79 69.7
s4-14 5.56 1 160 6.92 0.35 47.2 0.14 1.30 3.06 0.74 18.40 6.67 81.4
s4-15 1.65 645 2.92 0.01 20.7 0.33 1.18 0.52 9.66 3.71 46.6
s4-16 5.72 963 5.01 5.43 46.2 1.32 5.58 3.10 0.93 16.20 5.88 69.8
s4-17 6.46 1 322 11.30 0.05 39.3 0.07 0.90 2.36 0.93 17.00 6.80 85.0
s4-18 217.00 944 3.64 3.11 32.0 1.40 4.07 3.95 1.19 19.30 5.84 74.9
s4-19 4.87 947 5.27 34.1 0.00 0.47 2.01 0.71 16.30 5.69 64.6
s4-20 5.64 902 5.67 0.67 36.6 0.22 1.44 1.82 0.63 14.10 4.70 56.1
点号 含量/10-6 L/H δEu δCe
Ho Er Tm Yb Lu Hf Ta Pb ΣREE
s4-1 23.9 133 33.6 369 84.4 13 786 1.99 13.00 796 0.11 0.32 1.64
s4-2 26.5 140 35.2 391 87.0 13 772 2.42 14.60 795 0.05 0.24 251.30
s4-3 21.1 119 27.7 314 73.5 14 227 1.89 13.50 648 0.05 0.26 13.74
s4-4 35.2 189 45.8 502 107.0 13 242 2.34 16.80 1 028 0.04 0.46 349.23
s4-5 44.8 222 50.9 511 108.0 11 495 1.48 9.90 1 113 0.03 0.24 30.50
s4-6 29.7 152 35.0 396 82.2 13 168 1.99 10.60 824 0.04 0.26 152.77
s4-7 32.6 179 40.1 416 91.1 13 565 1.28 10.50 907 0.04 0.39 44.62
s4-9 26.5 148 34.9 384 87.0 13 474 1.53 10.10 801 0.05 0.44 3.90
s4-10 21.8 108 27.4 278 59.3 12 844 1.18 8.40 606 0.08 0.22 3.71
s4-12 38.0 211 47.6 522 113.0 12 276 1.76 18.20 1 094 0.05 0.35 10.48
s4-13 29.2 155 36.0 378 87.2 13 113 1.94 21.80 832 0.07 0.30 8.94
s4-14 36.2 181 40.4 441 101.0 12 473 2.14 17.70 959 0.06 0.23 51.59
s4-15 20.4 108 26.0 276 60.1 12 788 1.53 9.10 573 0.04 0.33
s4-16 30.5 152 38.0 397 90.9 12 497 1.82 15.20 862 0.08 0.32 4.06
s4-17 39.2 212 52.0 555 121.0 13 588 3.23 21.50 1 131 0.04 0.33 132.83
s4-18 30.8 150 33.1 340 72.0 10 967 1.38 7.00 772 0.06 0.34 3.71
s4-19 29.1 150 35.8 386 85.1 12 482 2.71 15.50 809 0.05 0.26
s4-20 27.5 143 34.6 387 86.6 13 084 2.21 14.60 795 0.05 0.27 22.97
), ArticleFig(id=1251249373464707570, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表4, caption=

檀树岭钼矿床锆石LA-ICP-MS微量元素数据(S4)

, figureFileSmall=null, figureFileBig=null, tableContent=
点号 含量/10-6
Ti Y Nb La Ce Pr Nd Sm Eu Gd Tb Dy
s4-1 802 4.66 10.70 45.7 4.27 14.70 4.20 0.88 13.70 4.05 54.0
s4-2 876 5.31 0.05 32.9 0.02 1.15 1.77 0.53 13.50 4.37 61.2
s4-3 1.54 689 3.27 0.87 28.2 0.28 1.14 1.31 0.49 11.70 3.28 46.2
s4-4 4.03 1 139 6.19 0.01 39.1 0.03 0.45 1.50 1.37 18.90 6.66 80.4
s4-5 10.40 1 342 3.52 0.08 28.3 0.25 2.80 4.08 1.12 26.90 8.34 104.0
s4-6 6.41 922 4.53 0.02 29.2 0.05 0.26 3.29 0.77 16.20 5.83 73.7
s4-7 0.86 1 069 2.58 0.04 25.9 0.16 2.12 4.47 1.55 21.80 7.05 85.7
s4-9 3.18 868 3.40 3.08 28.2 0.98 4.08 2.42 0.99 12.60 4.47 63.9
s4-10 7.24 690 2.76 4.06 30.9 0.93 3.99 2.08 0.49 13.00 4.40 51.2
s4-12 5.19 1 277 5.12 1.42 37.9 0.54 3.67 3.22 1.07 17.60 7.31 90.4
s4-13 2.88 964 5.61 3.01 47.5 0.43 2.44 2.47 0.77 14.70 5.79 69.7
s4-14 5.56 1 160 6.92 0.35 47.2 0.14 1.30 3.06 0.74 18.40 6.67 81.4
s4-15 1.65 645 2.92 0.01 20.7 0.33 1.18 0.52 9.66 3.71 46.6
s4-16 5.72 963 5.01 5.43 46.2 1.32 5.58 3.10 0.93 16.20 5.88 69.8
s4-17 6.46 1 322 11.30 0.05 39.3 0.07 0.90 2.36 0.93 17.00 6.80 85.0
s4-18 217.00 944 3.64 3.11 32.0 1.40 4.07 3.95 1.19 19.30 5.84 74.9
s4-19 4.87 947 5.27 34.1 0.00 0.47 2.01 0.71 16.30 5.69 64.6
s4-20 5.64 902 5.67 0.67 36.6 0.22 1.44 1.82 0.63 14.10 4.70 56.1
点号 含量/10-6 L/H δEu δCe
Ho Er Tm Yb Lu Hf Ta Pb ΣREE
s4-1 23.9 133 33.6 369 84.4 13 786 1.99 13.00 796 0.11 0.32 1.64
s4-2 26.5 140 35.2 391 87.0 13 772 2.42 14.60 795 0.05 0.24 251.30
s4-3 21.1 119 27.7 314 73.5 14 227 1.89 13.50 648 0.05 0.26 13.74
s4-4 35.2 189 45.8 502 107.0 13 242 2.34 16.80 1 028 0.04 0.46 349.23
s4-5 44.8 222 50.9 511 108.0 11 495 1.48 9.90 1 113 0.03 0.24 30.50
s4-6 29.7 152 35.0 396 82.2 13 168 1.99 10.60 824 0.04 0.26 152.77
s4-7 32.6 179 40.1 416 91.1 13 565 1.28 10.50 907 0.04 0.39 44.62
s4-9 26.5 148 34.9 384 87.0 13 474 1.53 10.10 801 0.05 0.44 3.90
s4-10 21.8 108 27.4 278 59.3 12 844 1.18 8.40 606 0.08 0.22 3.71
s4-12 38.0 211 47.6 522 113.0 12 276 1.76 18.20 1 094 0.05 0.35 10.48
s4-13 29.2 155 36.0 378 87.2 13 113 1.94 21.80 832 0.07 0.30 8.94
s4-14 36.2 181 40.4 441 101.0 12 473 2.14 17.70 959 0.06 0.23 51.59
s4-15 20.4 108 26.0 276 60.1 12 788 1.53 9.10 573 0.04 0.33
s4-16 30.5 152 38.0 397 90.9 12 497 1.82 15.20 862 0.08 0.32 4.06
s4-17 39.2 212 52.0 555 121.0 13 588 3.23 21.50 1 131 0.04 0.33 132.83
s4-18 30.8 150 33.1 340 72.0 10 967 1.38 7.00 772 0.06 0.34 3.71
s4-19 29.1 150 35.8 386 85.1 12 482 2.71 15.50 809 0.05 0.26
s4-20 27.5 143 34.6 387 86.6 13 084 2.21 14.60 795 0.05 0.27 22.97
), ArticleFig(id=1251249373556982267, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 5, caption=

Zircon LA-ICP-MS dating data of Tanshuling molybdenum deposit(S1)

, figureFileSmall=null, figureFileBig=null, tableContent=
测点号 U/10-6 Th/10-6 207Pb/206Pb 207Pb/235U ${{\mathrm{ }}^{2}}^{06}$Pb/238U 207Pb/235U 206Pb/238U
比值 1σ/% 比值 1σ/% 比值 1σ/% 年龄/Ma 2σ 年龄/Ma 2σ
s1-1 773 5 082.7 0.049 51 5.82 0.141 6 5.1 0.022 13 1.6 139 15 141 4
s1-2 436 7 068.5 0.053 48 5.46 0.169 7 5.8 0.022 86 2.2 157 17 146 6
s1-3 698 2 784.1 0.046 83 5.41 0.138 9 5.3 0.021 62 1.6 131 13 139 5
s1-4 976 1 640.1 0.058 48 4.17 0.166 8 3.9 0.020 99 1.8 156 11 134 5
s1-5 889 870.5 0.044 87 3.64 0.136 8 4.0 0.021 98 1.3 130 10 140 4
s1-6 382 375.9 0.047 81 8.07 0.137 4 7.5 0.022 23 2.4 128 18 142 7
s1-7 1 065 781.1 0.049 33 4.01 0.139 6 4.1 0.021 06 1.9 134 11 134 5
s1-8 634 458.2 0.049 90 4.99 0.155 0 5.0 0.022 72 2.1 145 14 145 6
s1-9 669 583.5 0.047 93 5.83 0.146 2 5.7 0.022 50 2.1 137 15 143 6
s1-10 712 493.1 0.049 26 5.59 0.147 1 5.4 0.021 90 1.4 138 14 140 4
s1-11 1 354 991.4 0.047 67 3.80 0.143 4 4.0 0.021 82 1.5 137 11 139 4
s1-12 612 411.6 0.051 64 6.23 0.162 1 6.6 0.022 55 2.2 150 19 144 6
s1-13 682 316.0 0.051 69 6.02 0.160 1 6.2 0.022 57 2.5 149 17 144 7
s1-14 514 412.0 0.052 61 5.41 0.151 3 5.6 0.020 83 2.1 141 15 133 6
s1-15 866 908.5 0.047 18 5.44 0.149 6 5.7 0.022 43 1.7 140 15 143 5
s1-16 716 701.2 0.046 60 5. 15 0.147 2 5.2 0.023 18 2.3 138 13 148 7
s1-17 505 596.8 0.051 32 6.28 0.173 2 7.0 0.023 55 2.2 159 21 150 7
), ArticleFig(id=1251249373695394306, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表5, caption=

檀树岭钼矿床锆石LA-ICP-MS定年数据(S1)

, figureFileSmall=null, figureFileBig=null, tableContent=
测点号 U/10-6 Th/10-6 207Pb/206Pb 207Pb/235U ${{\mathrm{ }}^{2}}^{06}$Pb/238U 207Pb/235U 206Pb/238U
比值 1σ/% 比值 1σ/% 比值 1σ/% 年龄/Ma 2σ 年龄/Ma 2σ
s1-1 773 5 082.7 0.049 51 5.82 0.141 6 5.1 0.022 13 1.6 139 15 141 4
s1-2 436 7 068.5 0.053 48 5.46 0.169 7 5.8 0.022 86 2.2 157 17 146 6
s1-3 698 2 784.1 0.046 83 5.41 0.138 9 5.3 0.021 62 1.6 131 13 139 5
s1-4 976 1 640.1 0.058 48 4.17 0.166 8 3.9 0.020 99 1.8 156 11 134 5
s1-5 889 870.5 0.044 87 3.64 0.136 8 4.0 0.021 98 1.3 130 10 140 4
s1-6 382 375.9 0.047 81 8.07 0.137 4 7.5 0.022 23 2.4 128 18 142 7
s1-7 1 065 781.1 0.049 33 4.01 0.139 6 4.1 0.021 06 1.9 134 11 134 5
s1-8 634 458.2 0.049 90 4.99 0.155 0 5.0 0.022 72 2.1 145 14 145 6
s1-9 669 583.5 0.047 93 5.83 0.146 2 5.7 0.022 50 2.1 137 15 143 6
s1-10 712 493.1 0.049 26 5.59 0.147 1 5.4 0.021 90 1.4 138 14 140 4
s1-11 1 354 991.4 0.047 67 3.80 0.143 4 4.0 0.021 82 1.5 137 11 139 4
s1-12 612 411.6 0.051 64 6.23 0.162 1 6.6 0.022 55 2.2 150 19 144 6
s1-13 682 316.0 0.051 69 6.02 0.160 1 6.2 0.022 57 2.5 149 17 144 7
s1-14 514 412.0 0.052 61 5.41 0.151 3 5.6 0.020 83 2.1 141 15 133 6
s1-15 866 908.5 0.047 18 5.44 0.149 6 5.7 0.022 43 1.7 140 15 143 5
s1-16 716 701.2 0.046 60 5. 15 0.147 2 5.2 0.023 18 2.3 138 13 148 7
s1-17 505 596.8 0.051 32 6.28 0.173 2 7.0 0.023 55 2.2 159 21 150 7
), ArticleFig(id=1251249373796057610, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 6, caption=

Zircon LA-ICP-MS dating data of Tanshuling molybdenum deposit(S2+S4)

, figureFileSmall=null, figureFileBig=null, tableContent=
测点号 U/10-6 Th/10-6 207Pb/206Pb 207Pb/235U ${{\mathrm{ }}^{2}}^{06}$Pb/238U 207Pb/235U 206Pb/238U
比值 1σ/% 比值 1σ/% 比值 1σ/% 年龄/Ma 2σ 年龄/Ma 2σ
s2-1 297 148.9 0.050 74 6.06 0.147 9 6.0 0.021 63 2.0 141 16 138 6
s2-5 96 81.9 0.054 62 10.83 0.155 7 10.4 0.022 46 2.6 141 28 143 7
s2-7 236 120.3 0.046 24 6.14 0.142 3 5.7 0.023 00 1.8 137 16 147 5
s2-8 136 98.9 0.055 89 7.74 0.162 3 7.5 0.022 33 2.7 149 21 142 8
s2-9 317 140.4 0.051 98 5.62 0.160 5 5.4 0.022 20 1.8 149 15 142 5
s2-11 456 227.0 0.048 34 4.96 0.141 5 4.6 0.021 30 1.9 133 11 136 5
s2-12 262 127.6 0.048 80 6.94 0.156 8 7.2 0.022 90 2.3 145 20 146 6
s2-15 507 371.1 0.049 35 5.06 0.148 6 5.1 0.021 69 1.5 139 13 138 4
s2-16 442 267.5 0.051 50 5.42 0.153 6 5.0 0.021 34 2.0 146 14 136 5
s2-18 566 434.0 0.054 67 5.50 0.161 2 5.5 0.021 78 1.8 150 15 139 5
s2-19 331 253.8 0.043 46 7.60 0.139 0 7.9 0.023 12 1.9 129 19 147 6
s2-20 617 449.3 0.051 95 6.62 0.147 2 6.7 0.021 11 2.1 137 17 135 6
s2-21 676 393.3 0.044 65 5.81 0.142 6 6.1 0.022 65 2.3 134 15 144 7
s2-22 653 441.6 0.046 96 6.12 0.142 8 6.6 0.021 92 2.1 134 16 140 6
s2-23 691 502.9 0.046 85 5.73 0.138 4 6.0 0.021 42 2.3 130 15 137 6
s2-24 781 619.1 0.046 09 5.94 0.136 9 5.3 0.022 02 2.1 129 13 140 6
s2-25 633 425.9 0.052 25 6.47 0.152 9 6.6 0.021 55 2.1 142 17 137 6
s2-26 857 722.0 0.050 75 4.77 0.146 7 4.4 0.021 46 1.9 138 11 137 5
s4-1 584 1 190.1 0.055 43 6.65 0.160 2 6.7 0.021 02 1.8 148 18 134 5
s4-2 657 2 755.8 0.044 40 6.61 0.131 1 5.7 0.022 64 2.1 124 13 144 6
s4-3 597 4 889.6 0.045 44 5.60 0.135 4 5.6 0.021 89 2.1 128 14 140 6
s4-4 773 1 489.9 0.044 42 5.07 0.140 6 5.1 0.022 87 2.1 132 13 146 6
s4-5 505 750.0 0.042 95 8.62 0.137 7 9.1 0.023 09 2.2 128 22 147 6
s4-6 549 382.6 0.055 70 7.06 0.165 4 6.4 0.021 97 2.3 153 18 140 6
s4-7 566 436.7 0.055 59 7.31 0.172 1 6.9 0.022 54 2.3 158 20 144 6
s4-9 530 291.4 0.049 93 5.71 0.158 5 5.7 0.022 47 2.3 148 16 145 7
s4-10 453 288.9 0.046 43 9.48 0.144 4 9.0 0.022 36 2.4 133 23 143 7
s4-12 1 180 1 063.9 0.042 99 6.43 0.131 2 6.3 0.021 66 1.5 124 15 138 4
s4-13 1 176 1 104.1 0.045 55 6.24 0.138 3 6.2 0.021 58 1.7 130 15 138 5
s4-14 946 721.6 0.046 52 5.14 0.143 6 5.2 0.021 89 1.8 135 13 140 5
s4-15 458 324.2 0.049 29 7.37 0.152 5 7.4 0.022 36 2.4 141 20 143 7
s4-16 843 666.9 0.043 07 5.48 0.132 3 5.9 0.021 64 1.5 125 14 138 4
s4-17 1 151 733.6 0.051 40 4.68 0.153 0 4.6 0.021 57 1.6 143 12 138 4
s4-18 377 360.0 0.050 47 7.98 0.152 5 8.1 0.021 01 2.5 145 23 134 7
s4-19 830 646.4 0.048 20 5.35 0.142 5 5.1 0.021 91 2.1 134 13 140 6
s4-20 782 551.9 0.043 27 6.42 0.125 7 6.0 0.021 67 1.8 119 13 138 5
), ArticleFig(id=1251249373947052565, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表6, caption=

檀树岭钼矿床锆石LA-ICP-MS定年数据(S2+S4)

, figureFileSmall=null, figureFileBig=null, tableContent=
测点号 U/10-6 Th/10-6 207Pb/206Pb 207Pb/235U ${{\mathrm{ }}^{2}}^{06}$Pb/238U 207Pb/235U 206Pb/238U
比值 1σ/% 比值 1σ/% 比值 1σ/% 年龄/Ma 2σ 年龄/Ma 2σ
s2-1 297 148.9 0.050 74 6.06 0.147 9 6.0 0.021 63 2.0 141 16 138 6
s2-5 96 81.9 0.054 62 10.83 0.155 7 10.4 0.022 46 2.6 141 28 143 7
s2-7 236 120.3 0.046 24 6.14 0.142 3 5.7 0.023 00 1.8 137 16 147 5
s2-8 136 98.9 0.055 89 7.74 0.162 3 7.5 0.022 33 2.7 149 21 142 8
s2-9 317 140.4 0.051 98 5.62 0.160 5 5.4 0.022 20 1.8 149 15 142 5
s2-11 456 227.0 0.048 34 4.96 0.141 5 4.6 0.021 30 1.9 133 11 136 5
s2-12 262 127.6 0.048 80 6.94 0.156 8 7.2 0.022 90 2.3 145 20 146 6
s2-15 507 371.1 0.049 35 5.06 0.148 6 5.1 0.021 69 1.5 139 13 138 4
s2-16 442 267.5 0.051 50 5.42 0.153 6 5.0 0.021 34 2.0 146 14 136 5
s2-18 566 434.0 0.054 67 5.50 0.161 2 5.5 0.021 78 1.8 150 15 139 5
s2-19 331 253.8 0.043 46 7.60 0.139 0 7.9 0.023 12 1.9 129 19 147 6
s2-20 617 449.3 0.051 95 6.62 0.147 2 6.7 0.021 11 2.1 137 17 135 6
s2-21 676 393.3 0.044 65 5.81 0.142 6 6.1 0.022 65 2.3 134 15 144 7
s2-22 653 441.6 0.046 96 6.12 0.142 8 6.6 0.021 92 2.1 134 16 140 6
s2-23 691 502.9 0.046 85 5.73 0.138 4 6.0 0.021 42 2.3 130 15 137 6
s2-24 781 619.1 0.046 09 5.94 0.136 9 5.3 0.022 02 2.1 129 13 140 6
s2-25 633 425.9 0.052 25 6.47 0.152 9 6.6 0.021 55 2.1 142 17 137 6
s2-26 857 722.0 0.050 75 4.77 0.146 7 4.4 0.021 46 1.9 138 11 137 5
s4-1 584 1 190.1 0.055 43 6.65 0.160 2 6.7 0.021 02 1.8 148 18 134 5
s4-2 657 2 755.8 0.044 40 6.61 0.131 1 5.7 0.022 64 2.1 124 13 144 6
s4-3 597 4 889.6 0.045 44 5.60 0.135 4 5.6 0.021 89 2.1 128 14 140 6
s4-4 773 1 489.9 0.044 42 5.07 0.140 6 5.1 0.022 87 2.1 132 13 146 6
s4-5 505 750.0 0.042 95 8.62 0.137 7 9.1 0.023 09 2.2 128 22 147 6
s4-6 549 382.6 0.055 70 7.06 0.165 4 6.4 0.021 97 2.3 153 18 140 6
s4-7 566 436.7 0.055 59 7.31 0.172 1 6.9 0.022 54 2.3 158 20 144 6
s4-9 530 291.4 0.049 93 5.71 0.158 5 5.7 0.022 47 2.3 148 16 145 7
s4-10 453 288.9 0.046 43 9.48 0.144 4 9.0 0.022 36 2.4 133 23 143 7
s4-12 1 180 1 063.9 0.042 99 6.43 0.131 2 6.3 0.021 66 1.5 124 15 138 4
s4-13 1 176 1 104.1 0.045 55 6.24 0.138 3 6.2 0.021 58 1.7 130 15 138 5
s4-14 946 721.6 0.046 52 5.14 0.143 6 5.2 0.021 89 1.8 135 13 140 5
s4-15 458 324.2 0.049 29 7.37 0.152 5 7.4 0.022 36 2.4 141 20 143 7
s4-16 843 666.9 0.043 07 5.48 0.132 3 5.9 0.021 64 1.5 125 14 138 4
s4-17 1 151 733.6 0.051 40 4.68 0.153 0 4.6 0.021 57 1.6 143 12 138 4
s4-18 377 360.0 0.050 47 7.98 0.152 5 8.1 0.021 01 2.5 145 23 134 7
s4-19 830 646.4 0.048 20 5.35 0.142 5 5.1 0.021 91 2.1 134 13 140 6
s4-20 782 551.9 0.043 27 6.42 0.125 7 6.0 0.021 67 1.8 119 13 138 5
), ArticleFig(id=1251249374081270298, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 7, caption=

Analytical results of main elements and trace elements in the Tanshuling granodiorite

, figureFileSmall=null, figureFileBig=null, tableContent=
样品编号 H1 H2 H3 H4 H5
主量元素/% Al2O3 14.9 14.4 15.8 16.0 15.9
CaO 2.69 1.56 2.01 2.80 2.75
Fe2O3 4.03 3.71 2.74 3.33 3.75
K2O 4.26 3.92 4.86 4.25 3.99
MgO 1.53 1.24 1.32 1.38 1.53
MnO 0.02 0.02 0.02 0.02 0.02
Na2O 2.90 3.81 3.27 3.53 3.43
P2O5 0.18 0.19 0.16 0.18 0.17
SiO2 64.50 66.30 66.80 65.00 65.10
TiO2 0.52 0.49 0.43 0.51 0.58
FeO 1.74 1.29 1.41 1.80 1.99
烧失量 1.98 2.47 1.79 1.29 1.12
总量 99.25 99.40 100.62 100.09 100.33
微量元素/10-6 Y 13.4 14.7 13.7 16.7 16.9
La 29.9 31.2 28.4 26.8 27.9
Ce 58.3 61.9 56.0 56.7 60.7
Pr 7.59 7.64 6.76 7.65 7.84
Nd 29.2 29.3 25.7 29.1 30.5
Sm 5.64 5.15 4.66 5.60 5.91
Eu 1.83 1.80 1.58 1.68 1.70
Gd 5.76 5.47 4.91 5.76 6.07
Tb 1.49 1.38 1.27 1.50 1.58
Dy 3.18 3.00 2.75 3.48 3.70
Ho 1.25 1.11 1.07 1.29 1.36
Er 2.83 3.17 3.00 3.65 3.80
Tm 0.49 0.45 0.42 0.50 0.54
Yb 2.84 2.85 2.79 3.39 3.46
Lu 0.51 0.42 0.44 0.48 0.52
V 62.7 61.7 62.4 71.5 74.1
Cu 213 2186 381 387 183
Pb 12.7 22.0 15.1 11.7 11.3
Zn 35.6 502 66.4 36.9 39.5
Ni 7.49 7.84 6.70 7.19 7.97
Co 9.33 10.8 5.87 7.20 7.45
W 18.5 44.4 20.3 17.5 26.1
Mo 86.4 79.2 27.0 44.6 12.5
Li 32.6 16.3 42.5 34.1 39.4
Sr 337 277 361 382 378
Rb 134 118 143 126 116
指标分析 A/NK 1.59 1.39 1.48 1.54 1.59
A/CNK 1.04 1.08 1.10 1.03 1.06
ΣREE/10-6 150 154 139 147 154
LREE/10-6 132 136 122 129 134
HREE/10-6 18.2 17.7 16.5 19.9 20.4
LREE/HREE 7.24 7.70 7.42 6.37 6.58
(La/Yb)N 7.15 7.44 6.91 5.37 5.48
δEu 0.96 1.04 0.96 0.90 0.86
δCe 0.91 0.95 0.95 0.95 0.98
), ArticleFig(id=1251249374232265250, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表7, caption=

檀树岭花岗闪长岩主量元素和微量元素分析结果

, figureFileSmall=null, figureFileBig=null, tableContent=
样品编号 H1 H2 H3 H4 H5
主量元素/% Al2O3 14.9 14.4 15.8 16.0 15.9
CaO 2.69 1.56 2.01 2.80 2.75
Fe2O3 4.03 3.71 2.74 3.33 3.75
K2O 4.26 3.92 4.86 4.25 3.99
MgO 1.53 1.24 1.32 1.38 1.53
MnO 0.02 0.02 0.02 0.02 0.02
Na2O 2.90 3.81 3.27 3.53 3.43
P2O5 0.18 0.19 0.16 0.18 0.17
SiO2 64.50 66.30 66.80 65.00 65.10
TiO2 0.52 0.49 0.43 0.51 0.58
FeO 1.74 1.29 1.41 1.80 1.99
烧失量 1.98 2.47 1.79 1.29 1.12
总量 99.25 99.40 100.62 100.09 100.33
微量元素/10-6 Y 13.4 14.7 13.7 16.7 16.9
La 29.9 31.2 28.4 26.8 27.9
Ce 58.3 61.9 56.0 56.7 60.7
Pr 7.59 7.64 6.76 7.65 7.84
Nd 29.2 29.3 25.7 29.1 30.5
Sm 5.64 5.15 4.66 5.60 5.91
Eu 1.83 1.80 1.58 1.68 1.70
Gd 5.76 5.47 4.91 5.76 6.07
Tb 1.49 1.38 1.27 1.50 1.58
Dy 3.18 3.00 2.75 3.48 3.70
Ho 1.25 1.11 1.07 1.29 1.36
Er 2.83 3.17 3.00 3.65 3.80
Tm 0.49 0.45 0.42 0.50 0.54
Yb 2.84 2.85 2.79 3.39 3.46
Lu 0.51 0.42 0.44 0.48 0.52
V 62.7 61.7 62.4 71.5 74.1
Cu 213 2186 381 387 183
Pb 12.7 22.0 15.1 11.7 11.3
Zn 35.6 502 66.4 36.9 39.5
Ni 7.49 7.84 6.70 7.19 7.97
Co 9.33 10.8 5.87 7.20 7.45
W 18.5 44.4 20.3 17.5 26.1
Mo 86.4 79.2 27.0 44.6 12.5
Li 32.6 16.3 42.5 34.1 39.4
Sr 337 277 361 382 378
Rb 134 118 143 126 116
指标分析 A/NK 1.59 1.39 1.48 1.54 1.59
A/CNK 1.04 1.08 1.10 1.03 1.06
ΣREE/10-6 150 154 139 147 154
LREE/10-6 132 136 122 129 134
HREE/10-6 18.2 17.7 16.5 19.9 20.4
LREE/HREE 7.24 7.70 7.42 6.37 6.58
(La/Yb)N 7.15 7.44 6.91 5.37 5.48
δEu 0.96 1.04 0.96 0.90 0.86
δCe 0.91 0.95 0.95 0.95 0.98
), ArticleFig(id=1251249374358094380, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 8, caption=

Sulfur isotope data of Tanshuling molybdenum deposit of granodiorites from Tanshuling

, figureFileSmall=null, figureFileBig=null, tableContent=
样品编号 检测方法 δ34SCDT/‰
M-1-2 直接燃烧法 5.8
M-2 直接燃烧法 5.0
M-3 直接燃烧法 6.0
M-6 直接燃烧法 5.9
M-8 直接燃烧法 6.3
), ArticleFig(id=1251249374479729204, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表8, caption=

檀树岭钼矿硫同位素测试结果

, figureFileSmall=null, figureFileBig=null, tableContent=
样品编号 检测方法 δ34SCDT/‰
M-1-2 直接燃烧法 5.8
M-2 直接燃烧法 5.0
M-3 直接燃烧法 6.0
M-6 直接燃烧法 5.9
M-8 直接燃烧法 6.3
), ArticleFig(id=1251249374622335551, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=EN, label=Table 9, caption=

Statistics on the diagenetic and metallogenic ages of deposits around the Tanshuling molybdenum deposit

, figureFileSmall=null, figureFileBig=null, tableContent=
地质情况 成岩年龄/Ma 成矿年龄/Ma 数据来源[40-41,48-58]
湛岭铼钼矿床 138.8±0.6 137.3±1.4 陈雪峰[48]
大坞尖钨钼矿床 148.5±2.1 144.4±1.5 李斌等[49]
东源钨钼矿床 146±1 146.4±2.3 王德恩等[50]
邓家坞钼矿床 772±11 141.4±0.88 李双等[51]
百丈岩钨钼矿床 130±1.5 136.3±2.6 秦燕等[52]
绩溪太子山钼矿 133.9±1.1 134.6±1.1 万建军等[53]
逍遥钨钼矿床 146.5±1.9 148.7±2.5 Su等[54]
桂林郑钨钼矿床 126.8±1.4 128.7±2.3 陈雪峰等[40]
高家塝钨矿床 144.9±1.2 146.1±4.8 肖鑫等[55]
竹溪岭钨钼矿床 143.3±1.9 142.7±2.1 黄马等[56]
西坞口钨钼矿床 141.7±1.0 陈雪峰等[41]
狮金山铜钼矿床 145.7±1.5 147.0±1.8 徐晓春等[57]
里东坑钼矿床 153.0±0.9 144.9±1.9 陈子微等[58]
), ArticleFig(id=1251249374748164678, tenantId=1146029695717560320, journalId=1146123166801305609, articleId=1149781954989613976, language=CN, label=表9, caption=

檀树岭钼矿床周边矿床成岩成矿年龄统计

, figureFileSmall=null, figureFileBig=null, tableContent=
地质情况 成岩年龄/Ma 成矿年龄/Ma 数据来源[40-41,48-58]
湛岭铼钼矿床 138.8±0.6 137.3±1.4 陈雪峰[48]
大坞尖钨钼矿床 148.5±2.1 144.4±1.5 李斌等[49]
东源钨钼矿床 146±1 146.4±2.3 王德恩等[50]
邓家坞钼矿床 772±11 141.4±0.88 李双等[51]
百丈岩钨钼矿床 130±1.5 136.3±2.6 秦燕等[52]
绩溪太子山钼矿 133.9±1.1 134.6±1.1 万建军等[53]
逍遥钨钼矿床 146.5±1.9 148.7±2.5 Su等[54]
桂林郑钨钼矿床 126.8±1.4 128.7±2.3 陈雪峰等[40]
高家塝钨矿床 144.9±1.2 146.1±4.8 肖鑫等[55]
竹溪岭钨钼矿床 143.3±1.9 142.7±2.1 黄马等[56]
西坞口钨钼矿床 141.7±1.0 陈雪峰等[41]
狮金山铜钼矿床 145.7±1.5 147.0±1.8 徐晓春等[57]
里东坑钼矿床 153.0±0.9 144.9±1.9 陈子微等[58]
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皖南泾县檀树岭钼矿床辉钼矿Re-Os和锆石U-Pb年代学及其地质意义
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穆玖清 1, 2, 3 , 王安东 1, 2, * , 汪方跃 4 , 王运 1, 2
科学技术与工程 | 论文·天文学、地球科学 2025,25(9): 3555-3572
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科学技术与工程 | 论文·天文学、地球科学 2025, 25(9): 3555-3572
皖南泾县檀树岭钼矿床辉钼矿Re-Os和锆石U-Pb年代学及其地质意义
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穆玖清1, 2, 3 , 王安东1, 2, * , 汪方跃4, 王运1, 2
作者信息
  • 1 东华理工大学核资源与环境省部共建国家重点实验室培育基地, 南昌 330013
  • 2 东华理工大学地球科学学院, 南昌 330013
  • 3 河北省地矿局第五地质大队, 唐山 063006
  • 4 合肥工业大学资源与环境工程学院, 合肥 230009
  • 穆玖清(1999—),男,汉族,河北唐山人,硕士研究生。研究方向:同位素地球化学。E-mail:

通讯作者:

* 王安东(1985—),男,汉族,安徽安庆人,博士,副教授。研究方向:同位素地球化学、地热学。E-mail:
Molybdenite Re-Os and Zircon U-Pb Chronology of Tanshuling Molybdenum Deposits from Jingxian County, Southern Anhui Province and Its Geological Significance
Jiu-qing MU1, 2, 3 , An-dong WANG1, 2, * , Fang-yue WANG4, Yun WANG1, 2
Affiliations
  • 1 State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
  • 2 School of Earth Sciences, East China University of Technology, Nanchang 330013, China
  • 3 The Fifth Geological Brigade of Hebei Bureau of Geology and Mineral Resources, Tangshan 063006, China
  • 4 School of Resource and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
出版时间: 2025-03-28 doi: 10.12404/j.issn.1671-1815.2403118
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檀树岭钼矿床处于江南隆起带内,位于江南断裂的南侧,其主体岩性为花岗闪长岩。为限定其成岩成矿时代和矿床成因,对其开展了锆石U-Pb年代学、辉钼矿Re-Os年代学和全岩主微量元素地球化学研究。结果表明:檀树岭花岗岩SiO2含量为64.5%~66.8%,Al2O3含量为14.4%~16.0%,K2O含量为3.92%~4.86%,Na2O含量为2.90%~3.91%,CaO含量为1.56%~2.8%,MgO含量为1.24%~1.53%,A/CNK为1.02~1.10,A/NK为1.37~1.59,主量元素特征显示其属于准铝质-弱过铝质高钾钙碱性-钾玄岩系列的I型花岗岩。稀土元素球粒陨石标准化曲线明显右倾,轻稀土相对富集,Eu负异常。檀树岭辉钼矿的Re-Os定年结果为(133.09±0.86) Ma,茂林岩体花岗闪长岩的U-Pb定年结果为(140.4±0.62) Ma、(139.9±0.66) Ma、(139.6±0.63) Ma,均属于早白垩世。综合年代学和地球化学结果可见檀树岭钼矿床主要岩浆活动属于太平洋构造体制,挤压与伸展的相互交替使该地区发生了大规模的岩浆与成矿作用。

江南隆起带  /  I型花岗岩  /  地球化学  /  Re-Os定年  /  U-Pb定年

The Tanshuling molybdenum deposit is located in the Jiangnan Uplift zone along south part of the Jiangnan Fault. Its main lithology type is granodiorite. With the aim to constrain their magma and ore-forming ages and deposit genesis, combined zircon U-Pb and molybdenite Re-Os geochronology together with whole-rock major and trace element geochemistry have been carried out. The result suggest that the content of SiO2 is 64.5%~66.8%, Al2O3 is 14.4%~16.0%, K2O is 3.92%~4.86%, Na2O is 2.90%~3.91%, CaO is 1.56%~2.8%, MgO is 1.24%~1.53%, A/CNK value of 1.02~1.10, and A/NK value of 1.37~1.59. The characteristics of major elements show that the granites belong to metaaluminium to weak peraluminous high potassium calc-alkaline pot-assium series with I-type granite nature. The chondrite-normalized REE patterns are evidently right-declined, with relatively LREE enrichment and slight Eu negative anomalies. The molybdenite Re-Os age of the Tanshuling molybdenite is (133.09±0.86) Ma, and the U-Pb dating of the Maolin granodiorite is (140.4±0.62) Ma, (139.9±0.66) Ma, (139.6±0.63) Ma, all belong to the Early Cretaceous. Integrated chronological and geochemical characteristics show that the main magmatic activity of the Tanshuling molybdenum deposit belong to the Pacific tectonic system, and the alternation of extrusion and extensional has led to large-scale magmatic and mineralization in this area.

Jiangnan Uplift belt  /  I-type granite  /  geochemistry  /  Re-Os dating  /  U-Pb dating
穆玖清, 王安东, 汪方跃, 王运. 皖南泾县檀树岭钼矿床辉钼矿Re-Os和锆石U-Pb年代学及其地质意义. 科学技术与工程, 2025 , 25 (9) : 3555 -3572 . DOI: 10.12404/j.issn.1671-1815.2403118
Jiu-qing MU, An-dong WANG, Fang-yue WANG, Yun WANG. Molybdenite Re-Os and Zircon U-Pb Chronology of Tanshuling Molybdenum Deposits from Jingxian County, Southern Anhui Province and Its Geological Significance[J]. Science Technology and Engineering, 2025 , 25 (9) : 3555 -3572 . DOI: 10.12404/j.issn.1671-1815.2403118
长江中下游成矿带和钦(赣)杭成矿带是中国东部两条重要的成矿带,是国内Cu-Fe-W-Mo等多金属矿产资源重要的产区[1-6]。夹持于两者东段之间的赣北—皖南地区,近20多年来,在该地区先后发现了诸多大型甚至超大型矿床,如大湖塘W-Cu矿、朱溪W-Cu矿、百丈岩W-Mo矿和东源Wo-M矿等,使得该地区成为中国又一重要的W-Mo多金属成矿带[7-8]。前人从岩浆岩、成岩成矿时代、成矿元素、矿床类型、全岩地球化学、全岩Sr-Nd-Pb和锆石Lu-Hf以及岩浆源区和成矿构造背景等方面将赣北—皖南地区成矿作用与长江中下游和钦杭成矿带成矿作用进行了对比[9-15],分别认为赣北—皖南成矿带类似于长江中下游成矿带或钦(赣)杭成矿带,或者代表了过渡型成矿带甚至是独立于两者之外的成矿带。因此,皖南地区金属成矿作用尤其是中生代钼-钨多金属成矿作用的成岩成矿时代、地球化学特征,以及矿床成因和成矿动力学背景还未形成共识。
钼作为一种全球稀缺性战略资源,同时也是中国的优势矿产资源,对其开展深入研究具有重要的理论和现实意义[16]。 现对产出于江南隆起带东段安徽南部泾县的檀树岭钼矿床开展系统的全岩主、微量元素和辉钼矿Re-Os年代学、S同位素以及含矿岩体的锆石U-Pb年代学研究,厘定它们的成岩成矿时代和成矿物质来源,并将其与研究区内其他矿床做进一步对比,探讨檀树岭钼矿床的成矿背景。
茂林岩体位于安徽泾县茂林镇,江南断裂带的南侧[图1(a)],属“沿江沉积区”和“皖南沉积区”的过渡地带;区域上褶皱单元为“太平复向斜”,沿次级背斜“茂林—龙门背斜”轴部侵入[17]。该岩体处于长江中下游南亚部南部,已不属于长江中下游成矿带,具有江南隆起过渡的成矿特色,而属于江南成矿带[5,7]。岩体总体出露面积约70 km2,以花岗闪长岩岩性为主,呈不规则椭圆状展布[图1(b)],并在岩体内部已发现湛岭钼矿和檀树岭钼矿,围岩南部为中志留统康山组及唐家坞组地层,北部为志留系、白垩系及新近系张家渡组地层,南东侧为泥盆系、石炭系、二叠系组成的向斜构造,属于铜山向斜的北东段[18];发育多条近平行展布的断裂,主要控制断裂有北东向断裂包括高坦断裂、江南断裂、赣东北—白际山断裂、江绍断裂,东西向断裂包括祁门—潜口断裂、周王断裂[3]
研究区处于茂林岩体中段相似穹窿位,面积约5.55 km2,距茂林镇4 km。矿段内钼矿体产于燕山期的花岗闪长斑岩内,地表矿化规模:长1 500 m,宽1 000 m;深部控制规模:长和延深均为600 m。钼矿化在时间和空间上与中酸性斑岩关系密切,矿化类型为非浸染状为主的细脉状V石英细脉和微裂隙控矿,属“渗透漏型”斑岩型钼矿床。
区内岩脉较发育,主要有石英正长斑岩、闪斜煌斑岩和石英闪长玢岩等;矿石类型为花岗斑岩型钼矿,主要金属矿物为辉钼矿、黄铁矿、少量磁铁矿,次生矿物为褐铁矿和白钨矿等,主要脉石矿物为石英、绢云母、钾长石、斜长石、绿泥石等。矿石品位:主要有益组分Mo含量一般为0.041%~0.144%,平均0.062%,略估算钼金属量为108 98 t,矿石钼品位变化较大,矿体平均品位变化不大,主要产于钾化蚀变带中,矿体局部伴生铜和硫品位较低[16]。研究样品均采自矿区露天采场内,样品总体新鲜。辉钼矿呈铅灰色,强金属光泽的细小鳞片状、叶片状,与石英关系密切,一般赋存于石英脉壁、裂隙壁及晶洞中,多以致密块状[图2(a)]和石英脉状[图2(b)]产出,岩体[图2(c)]大部分呈浅肉红色,具斑状结构。岩体镜下[图2(d)]观察主要由斜长石、石英、黑云母组成,含少量黄铁矿、磷灰石等,其中长石和黑云母颗粒较大,石英相对较小,组成似斑状结构,块状构造。斜长石约占60%,自形或半自形短柱状(0.2 mm×0.6 mm)~(0.7 mm×1.0 mm),多数颗粒表面较“脏”,一些颗粒几乎完全被绢云母等矿物取代,表明岩石遭受了强烈的后期风化蚀变;石英约含35%,呈它形粒状或不规则状充填于长石之间,有的形成“熔体假象”,粒径0.1~0.5 mm,内部常发育流体包裹体,部分颗粒表现出波状消光;黑云母约含5%,规则或不规则片状,颗粒大小范围较大,小的颗粒约为0.1 mm×0.2 mm,大的颗粒可达5 mm×10 mm,大颗粒的黑云母中通常含长石和石英包裹体,且自身有绿泥石化现象;黄铁矿呈浸染状分布或在石英细脉中发育,多数为不规则粒状,粒径0.1~0.2 mm。含矿石英脉镜下[图2(e)]观察岩石呈粒状变晶结构,几乎完全由石英组成,粒径在0.1~1 mm,石英颗粒直接接触,中间无胶结物,岩石中发育浸染状不透明矿物辉钼矿。
全岩主、微量元素测试分析在江西省地质局第十检测技术研究院完成,主量元素分析采用X荧光光谱仪Rigaku 100e(XRF)完成,测试的分析误差为1%~5%,分析程序见文献[21];微量元素采用Agilent 7900型电感耦合等离子体质谱仪(ICP-MS)进行测试,其中稀土元素的检测下限为0.05×10-6,部分元素检测下限为0.5×10-6,含量大于10×10-6的元素误差小于5%,含量小于10×10-6的元素误差小于10%,具体分析程序见文献[22]。
辉钼矿Re-Os同位素分析在国家地质实验测试中心铼-锇同位素年代学实验室完成。目前被普遍接受的187Os所求得的半衰期(4.23±0.13)×1010 a是美国劳伦兹实验室(Lawrance Livermore national lab)的1989年用ICP-MS测定由公斤级铼中产生的。将辉钼矿样品(主要以块状辉钼矿为主,部分为石英脉状辉钼矿)采用Carius管逆王水封闭溶液溶解,为避免因失耦现象而导致测年结果的误差,在溶解样品中应采用完整的颗粒并粉碎均匀,同位素测试仪器为电感耦合等离子体质谱仪TJA X-series ICP-MS,Re和Os分离化学前处理过程及质谱测试程序参见文献[23-26]。所测定的Re-Os同位素分析数据采用Ludwig程序软件进行处理[27],并计算同位素等时线年龄。Re、Os质量分数的不确定度为实验中产生的误差,置信水平95%。模式年龄的不确定度还包括衰变常数的不确定度(1.02%),置信水平为95%。模式年龄计算所采用的衰变常数为λ(187Re)=1.66×10-11 a-1
锆石单矿物分选在河北地质测绘院进行,将样品粉碎,经常规重选和电磁选后在双目镜下挑选出晶形、透明度较符合的锆石,在重庆宇劲科技有限公司锆石制靶,锆石CL图像与锆石激光剥蚀等离子体质谱(LA-ICP-MS)U-Pb同位素分析均在东华理工大学核资源与环境国家重点实验室完成。根据锆石CL结构特征,选择晶体特征良好、具有岩浆生长环带的锆石开展LA-ICP-MS U-Pb定年分析,分析采用PerkinElmer NexION 1000四极杆ICP-MS,激光剥蚀装置为ESI NWR 193 He准分子激光器。激光剥蚀能量密度为5.0 J/cm2,脉冲为5 Hz,剥蚀直径为30 μm。激光剥蚀过程中采用氦气作为剥蚀物质的载气。测试过程中,分别利用NIST 610玻璃和91500锆石(206Pb/238U年龄为1 063 Ma)作为元素和年龄外标,每间隔5个待测点插入两组91500锆石标样,间隔10个待测点插入两组NIST 610标样,并以29Si为元素内标。锆石U-Pb和微量元素数据利用Iolite软件处理[28]
硫同位素样品分析在东华理工大学核资源与环境国家重点实验室完成,把待测矿物碎块进行玛瑙球技术碎样,在镜下挑出单矿物,研磨至200目以下并保存,称取辉钼矿样品20~100 μg,在1 020 ℃下氧化为SO2,将用SO2进入Flash-EA与MAT-253质谱仪联机测试所得。数据结果采用以国际硫同位素CDT标准标定的国家硫同位素标准(硫化银)GBW-4414(δ34SCDT=-0.07‰)和GBW-4415(δ34SCDT=22.15‰)校正精度:δ34SCDT≤0.2‰,δ34SCDT的相对标准为V-CDT。
檀树岭钼矿8个辉钼矿样品的Re-Os同位素数据分析列于表1,样品的模式年龄在132.2~134.0 Ma。8个辉钼矿样品所拟合的直线具有良好的线性关系[图3(a)],所求得的Re-Os等时线年龄为(133.08±0.75) Ma,与模式年龄结果在误差范围内高度一致。初始187Os含量为(0.003±0.020) ng/g,表明初始187Os含量接近于0,该批数据符合辉钼矿Re-Os同位素定年的条件,此外该等时线的平均标准权重偏差(mean squared weighted deviation,MSWD)为0.45,表明所有样品的Re,Os同位素组成遵循放射性衰变定律,等时线年龄准确可靠。为更好地避免样品中Re-Os失耦现象导致的辉钼矿年龄偏差过大,所以采用辉钼矿Re-Os模式年龄的加权平均值来代表矿床的形成时代[29]。该8个样品模式年龄加权平均值[图3(b)]为(133.09±0.86) Ma,MSWD=0.26,与等时线年龄非常接近,因此可以代表檀树岭钼矿床确切的成矿年龄。
檀树岭钼矿床花岗闪长岩的锆石在透射光下多呈无色透明状,外形多为半自形-自形长柱状,晶形完好,颗粒相粒径长度150~200 μm,长宽比2∶1。锆石阴极发光图像中(图4)具有明显的岩浆生长环带,无核-幔结构,无后期变质壳,都表明这些锆石是岩浆形成后一次性结晶形成的,能代表岩浆冷却结晶的时代,说明是典型的岩浆成因锆石[30-31]。所测试样品的锆石具有稀土总量(ΣREE)较高、变化范围较大(482×10-6~1 377×10-6),全部锆石表现出重稀土元素(HREE)相对于轻稀土元素(LREE)强烈富集(L/H=LREE/HREE=0.03~0.31),并具有不同程度的δCe正异常(1.33~349.23)>1和δEu负异常(0.22~0.47)<1(表2~表4),表现出典型的岩浆锆石稀土元素分布特征(图5)。
锆石U和Th质量分数变化较大,锆石U、Th含量及Th/U比值可以作为不同成因类型锆石的判断依据,岩浆成因锆石的Th/U值大于0.4[30,33]。对3组新鲜花岗岩样品进行了锆石U-Pb同位素定年(表5表6图6),去除部分异常数据,并保留误差范围内分析得到的53个有效测试数据,绘制成等时线年龄图和谐和年龄图,基本皆分布于谐和曲线及其附近,S1样品中选取17颗锆石进行U-Pb同位素分析,其Th/U值为0.46~3.99,加权平均年龄为(140.4±0.62) Ma(MSWD=2.84);S2样品中选取18颗锆石进行U-Pb同位素分析,其Th/U值为0.44~0.85,加权平均年龄为(139.9±0.66) Ma(MSWD=1.95);S4样品中选取18颗锆石进行U-Pb同位素分析,其Th/U值为0.63~1.92,加权平均年龄为(139.6±0.63) Ma(MSWD=1.63),研究表明,REE-LREE和REE-δEu图解可用来进一步区分岩浆锆石和热液锆石[33],在REE-LREE图解[图7(a)]和REE-δEu图解中[图7(b)],样品全部落入岩浆锆石区域。因此样品锆石都属于典型的岩浆成因锆石,其年龄能够代表岩浆形成的年龄,表明该岩体形成于燕山晚期,代表其岩浆活动处于早白垩世。
根据檀树岭花岗闪长岩的地球化学元素分析结果中(表7),烧矢量(LOI)为1.12%~2.47%,表明样品并未经历强烈的蚀变。5件样品(H1~H5)的SiO2含量为64.50%~66.80%,平均值为65.54%;K2O含量为3.92%~4.86%,平均值为4.25%;Al2O3含量为14.40%~16.00%,平均值为15.40%;Fe2O3含量为2.74%~4.03%,平均值为3.51%;Na2O含量为2.90%~3.81%,平均值为3.39%;CaO含量为1.56%~2.8%,平均值为2.36%;MgO含量为1.24%~1.53%,平均值为1.40%;FeO含量为1.29%~1.99%,平均值为1.64%;TiO2含量为0.43%~0.58%,平均值为0.51%;P2O5含量为0.16%~0.19%,平均值为0.17%;MnO平均值为0.02%;碱铝比A/NK为1.37~1.59,平均值为1.52;铝过饱和度A/CNK为1.03~1.10,平均值为1.06。
根据檀树岭花岗闪长岩地球化学数据(表7)及稀土元素球粒陨石标准化图解[图8(a)]可知含有较低的稀土含量(ΣREE)139.5×10-6~154.9×10-6,轻稀土与重稀土比值(LREE/HREE)6.58~7.70,重稀土相对轻稀土亏损,模式斜率(La/Yb)N为5.48~7.44,说明轻重稀土分馏明显,表现出δEu的轻微负异常(0.86~1.04),在稀土元素球粒陨石标准化图解[图8(a)]呈右倾。微量元素原始地幔标准化图解[图8(b)]中,表现出富集Rb、K、Yb等元素,强烈的Sr、Ti、P元素亏损,Sr负异常表明受长石结晶的影响,而Ti的负异常可能是钛铁矿的分离结晶造成的,在微量元素原始地幔标准化图解[图8(b)]呈右倾。
5件檀树岭辉钼矿样品δ34SCDT的变化范围为5.0‰~6.3‰(表8),平均值为5.8‰,说明檀树岭钼矿床中的硫来源较为单一,通过硫同位素分析可初步判断成矿物质的来源并探讨矿床的成因。
研究得到的檀树岭岩体花岗闪长岩锆石U-Pb模式年龄为(140.43±0.62) Ma、(139.87±0.66) Ma、(139.61±0.63) Ma,代表岩体的形成时代;檀树岭辉钼矿Re-Os模式年龄为(133.09±0.86) Ma,代表矿床的形成时代,均属于早白垩世,为燕山期早期的岩浆活动与成矿作用的产物。檀树岭含矿岩浆结晶时间与矿化时间之间相差约7 Ma,其含矿热液活动时间较长,正是这一长时间的热液活动,使得钼高度富集。中国东部燕山期钼成岩年龄集中在145~135 Ma,成矿年龄集中在145~130 Ma,总体时差为0~15 Ma,杜保峰等[35]统计出钼的单体矿床成岩成矿时差集中在0~14 Ma,平均为4.1 Ma,其中斑岩型矿床(3.3 Ma)相比矽卡岩型(6.9 Ma)和石英脉型矿床(8.7 Ma)时差更短,也符合热液成矿中岩浆迁移的过程规律。7 Ma较一般斑岩型矿床成岩成矿时差(3.3 Ma)要长,但这个时间差仍符合一般矿床的演化特点,并未脱离钼矿成岩成矿时差的一般规律。如果时差小于14 Ma,可认为该岩体与成矿有直接联系;如果时差高出14 Ma,则认为该岩体与成矿无直接联系,可以理解为该岩体可能为矿床提供了成矿空间或者提供了少部分的物质来源。
综合前人同位素资料,142 Ma代表了江南隆起带上岩石年龄,指示了江南隆起带岩石圈拆沉的开始时间[36]。檀树岭钼矿的岩浆结晶年龄约140 Ma,成矿年龄约为133 Ma,其处在江南成矿带的成岩成矿年龄范围内,而长江中下游成矿带(安徽段)Cu-Mo-W矿带成岩成矿年龄为139~152 Ma,多数都在143 Ma以上[4,37-45],可初步判定檀树岭钼矿与江南成矿带成岩时间相吻合。经前人研究显示,檀树岭钼矿床周边的众多钼矿床成岩成矿年龄结果如表9所示,在此阶段,太平洋板块俯冲于亚欧大陆东南缘,该地处于俯冲带环境[46-47],表明皖南地区存在大规模的岩浆与成矿作用,并且成岩与成矿年龄相对集中[邓家坞钼矿床成岩年龄(772±11) Ma和天井山金矿成岩年龄(765.9±3.7) Ma除外],因此檀树岭钼矿床成岩成矿时代代表了皖南地区重要的岩浆与成矿作用,为皖南地区一带找矿提供了重要线索,进一步说明江南皖南地区燕山期成矿作用值得重视。
檀树岭花岗岩主量元素数据K2O-SiO2图解[图9(a)]中样品主体落在高钾钙碱性系列与钾玄岩系列分界线处;A/NK-A/CNK图解[图9(b)]中指示为准铝质-弱过铝质岩石;在花岗岩TAS分类图上[图9(c)],主要落于石英二长岩和花岗闪长岩二者分界线附近;SiO2-Y图解[图9(d)]中指示为I型花岗岩。可知檀树岭花岗岩属于准铝质-弱过铝质高钾钙碱性-钾玄岩系列的I型花岗岩。
Re4+的离子半径与Mo4+相近,Re以类质同象的形式替代Mo进入辉钼矿中,富集程度在辉钼矿中能达到最大,并且Re在地幔中的富集程度大于在地壳中的富集程度,因此辉钼矿中Re元素的含量可以指示相关矿床的成矿物质来源,从幔源(×10-4)到壳幔混源(×10-5)再到壳源(×10-6),辉钼矿中Re的质量分数呈数量级的降低[62],檀树岭辉钼矿样品中Re质量分数为0.6×10-6~91.4×10-6(表1),说明其成矿物质来源于地壳物质的部分熔融,并且含有地幔物质的参与。
5件檀树岭辉钼矿样品δ34SCDT的变化范围为5.0‰~6.3‰(表5),平均值为5.8‰,说明檀树岭钼矿床中的硫来源较为单一,通过硫同位素分析可初步判断成矿物质的来源。花岗质岩浆硫δ34SCDT在5‰~15‰,壳源岩浆δ34SCDT在-5‰~7‰;幔源岩浆δ34SCDT为0±3‰[63]。通过硫同位素数据及变化范围(图10),该5件辉钼矿样品处在花岗岩(-5%~11%)和花岗质岩浆岩硫(3%~15%)范围内,并与壳源岩浆(-4%~6%)有部分交集,可知成矿物质部分来源于有地壳部分参与的花岗质熔体,说明檀树岭钼矿床与该地区的花岗斑岩具有密切的成因关系。地幔岩浆对地壳物质的混染,钙碱性系列花岗岩或多或少与地幔有直接关系,其程度取决于部分熔融的时间和作用过程,具有特有的地球化学特征。岩体中的微量元素(表4),Sr、Ti元素的亏损可能是岩浆活动中受到了斜长石、钛铁矿或金红石的结晶分异和源区残留造成的,LREE型的低Sr高Yb的特征符合中生代的壳幔混合型[64];δEu-(La/Yb)N图解中(图11),样品落入壳幔混合的区域。都说明地幔物质与地壳发生了部分熔融[65]
图12所示,从燕山期岩体构造事件及其对应年龄来看,江南隆起带燕山期的主要岩浆活动正处于太平洋构造体制,太平洋板块运动挤压与伸展的相互交替使该地区发生了大规模的岩浆与成矿作用,处在了岩浆活动的高峰期,是早白垩时期由伸展(120 Ma)到挤压(130 Ma)再到伸展(140 Ma)背景的过渡阶段,具有沿江与皖南地区岩浆岩混合类型的过渡特征。燕山期的岩浆活动主要集中在125~140 Ma[66-67],江南隆起带(安徽段)在146~136 Ma构造背景由挤压向伸展背景过渡,产生大量逆掩断层和推覆构造;在135 Ma之后以伸展背景为主,并存在着少数的挤压背景[11,44,68-71],檀树岭钼矿床所代表的Ⅰ型花岗岩(140 Ma)即形成于挤压向伸展的过渡背景中。随着太平洋板块的向西俯冲的程度增加,沿陆内俯冲带发生了大量的岩浆活动,驱赶软流圈沿构造薄弱带上涌,地幔侵蚀减薄,致使地幔物质侵入至下地壳部位并发生部分熔融,所产生的壳幔混合岩浆沿着一系列断裂通道侵入,形成了花岗闪长岩、二长花岗岩为主的典型I型花岗岩。
(1)檀树岭辉钼矿Re-Os模式年龄为(133.1±0.86) Ma,代表矿床的形成时代;檀树岭岩体花岗闪长岩锆石U-Pb模式年龄为(140.4±0.62)Ma、(139.9±0.66)Ma、(139.6±0.63) Ma,代表岩体的形成时代,与江南成矿带成岩成矿时间吻合,为中国东部燕山早期岩石圈活化和早白垩世成岩成矿大爆发的一部分。研究结果为后续在江南成矿带,尤其是皖南和赣北地区寻找新的Mo-W金属矿产资源提供了新的启示。
(2)地球化学特征表明檀树岭花岗岩富集大离子亲石元素,轻重稀土分馏明显,重稀土相对轻稀土亏损,Eu负异常,属于准铝质-弱过铝质高钾钙碱性-钾玄岩系列的Ⅰ型花岗岩。通过辉钼矿样品中Re质量分数0.6×10-6~91.4×10-6和δEu-(La/Yb)N图解,说明其成矿物质来源可能具有壳幔混合源的特点。通过硫同位素示踪得知δ34S平均值为5.8‰,说明硫来源较为单一,其成矿物质来源于花岗质的岩浆岩。
(3)檀树岭钼矿床形成时正处于太平洋构造体制下的挤压向伸展背景转换的构造环境,并形成了典型的I型花岗岩。
  • 国家自然科学基金(41763005)
  • 国家重点研发计划(2018YFA0404104)
  • 放射性地质与勘探技术国防重点学科实验室项目(RGET2209)
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2025年第25卷第9期
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doi: 10.12404/j.issn.1671-1815.2403118
  • 接收时间:2024-04-26
  • 首发时间:2025-07-09
  • 出版时间:2025-03-28
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  • 收稿日期:2024-04-26
  • 修回日期:2024-12-19
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国家自然科学基金(41763005)
国家重点研发计划(2018YFA0404104)
放射性地质与勘探技术国防重点学科实验室项目(RGET2209)
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    1 东华理工大学核资源与环境省部共建国家重点实验室培育基地, 南昌 330013
    2 东华理工大学地球科学学院, 南昌 330013
    3 河北省地矿局第五地质大队, 唐山 063006
    4 合肥工业大学资源与环境工程学院, 合肥 230009

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* 王安东(1985—),男,汉族,安徽安庆人,博士,副教授。研究方向:同位素地球化学、地热学。E-mail:
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2种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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