Article(id=1307087562691076469, tenantId=1146029695717560320, journalId=1306274195778404443, issueId=1307087507837964779, articleNumber=null, orderNo=null, doi=10.12401/j.nwg.2025097, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1733068800000, receivedDateStr=2024-12-02, revisedDate=1748880000000, revisedDateStr=2025-06-03, acceptedDate=1749139200000, acceptedDateStr=2025-06-06, onlineDate=1789563559457, onlineDateStr=2026-09-16, pubDate=1781884800000, pubDateStr=2026-06-20, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1789563559457, onlineIssueDateStr=2026-09-16, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1789563559457, creator=13701087609, updateTime=1789563559457, updator=13701087609, issue=Issue{id=1307087507837964779, tenantId=1146029695717560320, journalId=1306274195778404443, year='2026', volume='59', issue='3', pageStart='1', pageEnd='376', issueExtLink='null', onlineDate='null', pubDate='1781884800000', pubDateStr='2026-06-20', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1789563546379, creator='13701087609', updateTime=1789616219263, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1307308434005709553, tenantId=1146029695717560320, journalId=1306274195778404443, issueId=1307087507837964779, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1307308434005709554, tenantId=1146029695717560320, journalId=1306274195778404443, issueId=1307087507837964779, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=121, endPage=142, ext={EN=ArticleExt(id=1307087562863042934, articleId=1307087562691076469, tenantId=1146029695717560320, journalId=1306274195778404443, language=EN, title=Geochronology, Geochemistry and Geological Significance of the Early Paleozoic Waizuishan Pluton in the Southern Beishan Orogenic Belt, columnId=null, journalTitle=Northwestern Geology, columnName=null, runingTitle=null, highlight=null, articleAbstract=

The Beishan Orogenic Belt, situated in the central segment of the southern margin of the Central Asian Orogenic Belt (CAOB), has undergone prolonged, multi-stage subduction and accretion. It represents a key region for reconstructing the tectonic evolution of the southern CAOB margin and the closure of the Paleo-Asian Ocean. The Early Paleozoic was a significant crustal evolution period for the Beishan Orogenic Belt, characterized by frequent magmatic activity. Previous studies primarily focused on the central-western part of the belt, reporting a magmatic flare-up at 450−420 Ma. This study presents systematic geochronological and geochemical investigations of the Waizuishan pluton, located on the southeastern edge of the Shuangyingshan-Huaniushan tectonic unit within the Beishan Orogenic Belt. The Waizuishan pluton mainly comprises quartz diorite (and granodiorite. Zircon U-Pb dating yielded crystallization ages of (427.1±3.4) Ma and (418.6±2.8) Ma. The rocks belong to the metaluminous series (A/CNK＜1), exhibiting calc-alkaline and magnesian affinities. They possess low total rare earth element (ΣREE) contents, are enriched in light rare earth elements (LREEs), and show weak negative Eu anomalies (δEu=0.72−0.86). Geochemically, they are enriched in large-ion lithophile elements (LILEs: e.g., Rb, Th, U, K, Pb) and depleted in high-field-strength elements (HFSEs: e.g., Nb, Ta, P, Zr, Ti). Zircon εHf(t) values range from −2.0 to 0.6, corresponding to Hf crustal model ages (T_DMC) of 1.53−1.36 Ga. The geochemical signatures indicate that the Waizuishan pluton is an I-type granite formed within a subduction-related continental margin igneous arc. It was derived predominantly from the remelting of Mesoproterozoic crustal material with minor contributions from mantle-derived components. Nearly contemporaneous magmatism occurred within all four tectonic units of the Beishan Orogenic Belt. Zircon Hf model ages from Paleozoic igneous rocks (500−350 Ma) exhibit prominent peaks at 1.5−1.4 Ga and 0.8−1.0 Ga, correlating with Mesoproterozoic (～1.4 Ga) and Neoproterozoic (～0.9 Ga) tectonothermal events. This suggests that the various tectonic units of the Beishan Orogenic Belt likely share a common source region. Comparisons with the Yili Block and Central Tianshan Block indicate that these three terranes show stronger affinities with the Baltica and Laurentia cratons, whereas they lack affinity with the Tarim Craton, as represented by the Dunhuang Block.

, authors=Meiling DONG¹, Chao TENG^{1, *}, Xinjie YANG¹, Biren WANG², Jun CAO¹, Xiqing CHEN¹, Jie SHAO¹, Xiaofei ZHANG³, Shucai LI¹, authorsList=Meiling DONG, Chao TENG, Xinjie YANG, Biren WANG, Jun CAO, Xiqing CHEN, Jie SHAO, Xiaofei ZHANG, Shucai LI, authorCompany=null, correspAuthors=Chao TENG, authorNote=null, correspAuthorsNote=null, copyrightStatement=Copyright © 2026 Northwestern Geology. All rights reserved., 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, fund=null), CN=ArticleExt(id=1307087566851826059, articleId=1307087562691076469, tenantId=1146029695717560320, journalId=1306274195778404443, language=CN, title=北山造山带南部早古生代歪咀山岩体的年代学、地球化学特征及地质意义, columnId=1307087508710380014, journalTitle=西北地质, columnName=中亚成矿域关键矿产研究进展, runingTitle=null, highlight=null, articleAbstract=

北山造山带位于中亚造山带南缘中段，经历了长期多阶段的俯冲、拼贴，是记录中亚造山带南缘构造演化与古亚洲洋闭合的重要区域。早古生代是北山造山带重要的地壳演化时期，岩浆活动频繁，前人的报道多集中在北山造山带的中西部，岩浆活动峰值为450～420 Ma。笔者以北山造山带双鹰山–花牛山构造单元东南缘的歪咀山岩体为研究对象，开展系统的年代学及地球化学研究。歪咀山岩体主要由石英闪长岩和花岗闪长岩组成，锆石U-Pb年龄为（427.1±3.4）Ma和(418.6±2.8) Ma。岩石属于准铝质系列（A/CNK＜1），显示钙碱性和镁质特征。岩石稀土元素总量较低，富集轻稀土元素，具有较弱的负Eu异常（δEu = 0.72～0.86），富集Rb、Th、U、K、Pb等大离子亲石元素（LILEs），亏损Nb、Ta、P、Zr、Ti等高场强元素（HFSEs）。锆石ε_Hf(t)值为−2.0～0.6，对应的Hf同位素地壳模式年龄为1.53～1.36 Ga。地球化学特征显示歪咀山岩体属于I型花岗岩，为形成于俯冲构造环境下的大陆边缘火成岩弧，主要来源于中元古代地壳物质的重熔，并有少量幔源物质的贡献。北山造山带4个构造单元存在几乎同期的岩浆活动，古生代岩浆岩（500～350 Ma）锆石Hf模式年龄具有1.5～1.4 Ga和0.8～1.0 Ga的峰值，与中元古代～1.4 Ga和新元古代～0.9 Ga两期构造热事件记录相对应，说明北山造山带各构造单元可能具有统一的来源。通过北山造山带与伊犁地块、中天山地块的对比，推断三者可能与波罗的克拉通和劳伦克拉通更具亲缘性，而与以敦煌地块为代表的塔里木克拉通不具亲缘性。

, authors=董美玲¹, 滕超^{1, *}, 杨欣杰¹, 王必任², 曹军¹, 陈喜庆¹, 邵杰¹, 张晓飞³, 李树才¹, authorsList=董美玲, 滕超, 杨欣杰, 王必任, 曹军, 陈喜庆, 邵杰, 张晓飞, 李树才, authorCompany=null, correspAuthors=滕超, authorNote=, correspAuthorsNote=, copyrightStatement=版权所有©《西北地质》编辑部 2026, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=NjXQf69iQMplPixcOs0HjA==, magXml=F0Q2OvcrkrFVo+8tw7rlUw==, pdfUrl=null, pdf=30W+msuctkmP+TSZCxh8Vw==, pdfFileSize=12480781, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=7QuZZn4o9aujCl7DmAmShw==, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=u07DvsVSAh580wbPA2VjKw==, mapNumber=null, fund=null)}, authors=[Author(id=1307087567694881174, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, orderNo=0, firstName=null, middleName=null, lastName=null, nameCn=null, orcid=null, stid=null, country=null, authorPic=null, dead=0, email=dml_happy@126.com, emailSecond=null, emailThird=null, correspondingAuthor=0, authorType=1, ext={EN=AuthorExt(id=1307087567770378648, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, authorId=1307087567694881174, language=EN, stringName=Meiling DONG, firstName=Meiling, middleName=null, lastName=DONG, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=¹Cores and Samples Center of Natural Resources, China Geological Survey, Sanhe 065201, Hebei, China, bio=null, bioImg=null, bioContent=null, aboutCorrespAuthor=null), CN=AuthorExt(id=1307087567845876121, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, authorId=1307087567694881174, language=CN, stringName=董美玲, firstName=null, middleName=null, lastName=null, prefix=null, suffix=null, authorComment=null, nameInitials=null, affiliation=null, department=null, xref=¹, address=¹中国地质调查局自然资源实物地质资料中心，河北 三河　065201, bio={"content":"

董美玲（1986−），女，博士，高级工程师，主要从事基础地质调查与研究。E−mail：dml_happy@126.com

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董美玲（1986−），女，博士，高级工程师，主要从事基础地质调查与研究。E−mail：dml_happy@126.com

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Precambrian Research, 2013, 235: 251−263., articleTitle=The generation and evolution of Archean continental crust in the Dunhuang block, northeastern Tarim craton, northwestern China, refAbstract=null)], funds=null, companyList=[AuthorCompany(id=1307087567325782412, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, xref=1, ext=[AuthorCompanyExt(id=1307087567334171021, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, companyId=1307087567325782412, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=¹Cores and Samples Center of Natural Resources, China Geological Survey, Sanhe 065201, Hebei, China), AuthorCompanyExt(id=1307087567342559630, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, companyId=1307087567325782412, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=¹中国地质调查局自然资源实物地质资料中心，河北 三河　065201)]), AuthorCompany(id=1307087567413862799, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, xref=2, ext=[AuthorCompanyExt(id=1307087567422251408, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, companyId=1307087567413862799, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=²School of Earth Sciences, Institute of Disaster Prevention, Sanhe 065201, Hebei, China), AuthorCompanyExt(id=1307087567430640017, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, companyId=1307087567413862799, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=²防灾科技学院地球科学学院，河北 三河　065201)]), AuthorCompany(id=1307087567485165970, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, xref=3, ext=[AuthorCompanyExt(id=1307087567493554579, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, companyId=1307087567485165970, language=EN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=³Development and Research Centre, China Geological Survey, Beijing 100037, China), AuthorCompanyExt(id=1307087567506137492, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, companyId=1307087567485165970, language=CN, country=null, province=null, city=null, postcode=null, companyName=null, departmentName=null, remark=³中国地质调查局发展研究中心，北京　100037)])], figs=[ArticleFig(id=1307087574795837901, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.1, caption=(a) Simplified tectonic map of the Central Asian Orogenic Belt and (b) simplified geological map of the Beishan Orogenic Belt, figureFileSmall=QQwTFk7XUnwiI19vfX8Zyg==, figureFileBig=7QuZZn4o9aujCl7DmAmShw==, tableContent=null), ArticleFig(id=1307087574892306894, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图1, caption=中亚造山带构造简图（a, 据孙海瑞等, 2020）和北山造山带地质简图（b, 据Niu et al., 2018和He et al., 2018修改）

图中年龄数据来源见表1

, figureFileSmall=QQwTFk7XUnwiI19vfX8Zyg==, figureFileBig=7QuZZn4o9aujCl7DmAmShw==, tableContent=null), ArticleFig(id=1307087575320125903, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.2, caption=Simplified geological map of the Waizuishan Area, figureFileSmall=7So9lU5llPMCbTCuQA2YHg==, figureFileBig=peQcCyAI8YnEBvoimocFxw==, tableContent=null), ArticleFig(id=1307087575617921488, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图2, caption=歪咀山地区地质简图（据自然资源实物地质资料中心, 2019修改）, figureFileSmall=7So9lU5llPMCbTCuQA2YHg==, figureFileBig=peQcCyAI8YnEBvoimocFxw==, tableContent=null), ArticleFig(id=1307087575685030353, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.3, caption=Field outcrops and microscopic characteristics of the Waizuishan pluton, figureFileSmall=5e+h/C6vaETtqO6hhSrRsw==, figureFileBig=XvcvR7GLGHYpGS/vymmKzw==, tableContent=null), ArticleFig(id=1307087575752139218, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图3, caption=歪咀山岩体的野外露头及显微特征

a、b.歪咀山岩体野外露头和手标本；c、d.石英闪长岩和花岗闪长岩单偏光下薄片；e、f.石英闪长岩和花岗闪长岩正交光下薄片；g、h.石英闪长岩和花岗闪长岩正交光下显微特征；MME.暗色包体；Hbl.角闪石；Bit.黑云母；Pl.斜长石；Kf.钾长石；Q.石英

, figureFileSmall=5e+h/C6vaETtqO6hhSrRsw==, figureFileBig=XvcvR7GLGHYpGS/vymmKzw==, tableContent=null), ArticleFig(id=1307087576028963283, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.4, caption=Zircon cathodoluminescence images of quartz diorite and granodiorite from the Waizuishan pluton, figureFileSmall=FKIJlBXlPbP/MPTURsAhsA==, figureFileBig=pcJtpo+GkqobAXbHvZLm7w==, tableContent=null), ArticleFig(id=1307087576100266452, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图4, caption=歪咀山岩体石英闪长岩和花岗闪长岩的锆石阴极发光图像, figureFileSmall=FKIJlBXlPbP/MPTURsAhsA==, figureFileBig=pcJtpo+GkqobAXbHvZLm7w==, tableContent=null), ArticleFig(id=1307087576188346837, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.5, caption=LA-ICP-MS zircon U-Pb concordia diagram for quartz diorite and granodiorite from the Waizuishan pluton, figureFileSmall=WocX033kxprOZl+JCiT1iw==, figureFileBig=btDQr+vjnpOqPE+4PWYNuw==, tableContent=null), ArticleFig(id=1307087576465170902, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图5, caption=歪咀山岩体石英闪长岩和花岗闪长岩的LA-ICP-MS锆石U-Pb年龄谐和图, figureFileSmall=WocX033kxprOZl+JCiT1iw==, figureFileBig=btDQr+vjnpOqPE+4PWYNuw==, tableContent=null), ArticleFig(id=1307087576536474071, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.6, caption=Geochemical classification diagrams of the Waizuishan pluton, figureFileSmall=NZrJlDG4cD90OYUtL9xljQ==, figureFileBig=+1Wochgx0Ya7OLEQD4lULQ==, tableContent=null), ArticleFig(id=1307087576607777240, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图6, caption=歪咀山岩体的地球化学分类图解

a. （K₂O+Na₂O）-SiO₂图解 （Middlemost, 1994）；b. A/CNK-A/NK图解 （Maniar and Piccoli, 1989）；c. （K₂O+Na₂O-CaO）-SiO₂和 d. FeO*/（MgO+ FeO*）-SiO₂图解 （Frost et al., 2001）；双鹰山−花牛山构造单元志留世—泥盆世（438～366 Ma）花岗岩类数据来源见表1

, figureFileSmall=NZrJlDG4cD90OYUtL9xljQ==, figureFileBig=+1Wochgx0Ya7OLEQD4lULQ==, tableContent=null), ArticleFig(id=1307087576876212697, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.7, caption=Primitive mantle-normalized trace element patterns and chondrite-normalized REE patterns of the Waizuishan pluton, figureFileSmall=gaRA6xAUmHLroDWJ4zmcug==, figureFileBig=1T86W7zr5pt/sUhGl5qJ8w==, tableContent=null), ArticleFig(id=1307087578558128602, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图7, caption=歪咀山岩体的微量元素原始地幔标准化蛛网图及稀土元素球粒陨石标准化配分曲线图

标准化数值据Sun et al., （1989）

, figureFileSmall=gaRA6xAUmHLroDWJ4zmcug==, figureFileBig=1T86W7zr5pt/sUhGl5qJ8w==, tableContent=null), ArticleFig(id=1307087578650403291, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.8, caption=Zircon Hf isotopic evolution diagram for the Paleozoic granitoids from individual terranes of the Beishan Orogenic Belt, figureFileSmall=X5f0z0ftpiKdD94G6V4jEw==, figureFileBig=GRzdWZEfyWJBe9bqfZBdCA==, tableContent=null), ArticleFig(id=1307087578990141916, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图8, caption=北山造山带各构造单元古生代（500～350 Ma）花岗岩类的锆石Hf同位素演化图解（数据来源见表1）, figureFileSmall=X5f0z0ftpiKdD94G6V4jEw==, figureFileBig=GRzdWZEfyWJBe9bqfZBdCA==, tableContent=null), ArticleFig(id=1307087579065639389, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.9, caption=(a) Rb-(Y+Nb) and (b) R1-R2 tectonic discriminant diagrams of the Waizuishan pluton, figureFileSmall=fh9McOyedCQDbA1YCKRWSg==, figureFileBig=6KQ5e1Nj3hPqWj0j2x8Syg==, tableContent=null), ArticleFig(id=1307087579396989406, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图9, caption=歪咀山岩体Rb-(Y+Nb) （a；据Pearce et al., 1984） 和R1-R2 （b；据Batchelor et al., 1985 ） 构造环境判别图解, figureFileSmall=fh9McOyedCQDbA1YCKRWSg==, figureFileBig=6KQ5e1Nj3hPqWj0j2x8Syg==, tableContent=null), ArticleFig(id=1307087579472486879, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Fig.10, caption=Zircon Hf model age frequency diagrams of zircon grains from the Paleozoic magmatic rocks in the Beishan Orogenic Belt and adjacent tectonic units, figureFileSmall=OMDVqY6RDv2aS+R5sizNqg==, figureFileBig=jLOP2b2xU92F+eE8FdWpig==, tableContent=null), ArticleFig(id=1307087579547984352, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=图10, caption=北山造山带以及相邻构造单元古生代（500～350 Ma）岩浆锆石Hf模式年龄统计, figureFileSmall=OMDVqY6RDv2aS+R5sizNqg==, figureFileBig=jLOP2b2xU92F+eE8FdWpig==, tableContent=null), ArticleFig(id=1307087579837391329, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Tab.1, caption=

Magmatic activities from Paleozoic occurred in the Beishan Orogenic Belt, Yili Block and Central Tianshan Block

, figureFileSmall=null, figureFileBig=null, tableContent=

构造单元	样品名	岩性	年龄（Ma）	参考文献
黑鹰山–旱山单元	BS041	片麻状花岗岩	423	刘雪敏等（2010）
	10SYQ07	眼球状片麻岩	499	Song et al. （2013）
	10SYQ08	糜棱岩化花岗岩	474	Song et al. （2013）
	10SYQ03	花岗片麻岩	471	Song et al. （2013）
	10SYQ05	糜棱岩化花岗岩	448	Song et al. （2013）
	X10-70-1-01	石板井糜棱岩化花岗岩	464	Yuan et al. （2018）
	X10-71-1-01	石板井糜棱岩化花岗岩	455	Yuan et al. （2018）
	X10-73-1-01	石板井闪长岩	450	Yuan et al. （2018）
	X10-69-1-10	石板井糜棱岩化花岗岩	445	Yuan et al. （2018）
	X10-77-1-01	石板井糜棱岩化花岗岩	439	Yuan et al. （2018）
	X10-72-1-03	石板井糜棱岩化花岗岩	433	Yuan et al. （2018）
	X10-77-2-01	石板井石英二长岩	428	Yuan et al. （2018）
	TW12	二长花岗岩	442	胡新茁等（2024）
	P7TW2	花岗闪长岩	443	胡新茁等 （2024）
马鬃山单元	BS07-136	公婆泉花岗岩	402	郑荣国等（2012）
	1122CL	白圪塔石英闪长岩	436	李小菲（2013）
	1129HTJ	白圪塔二长花岗岩	435	李小菲（2013）
	1131CG-6	白圪塔花岗闪长岩	431	李小菲（2013）
	1132WG	马鬃山石英闪长岩	367	李小菲（2013）
	X10-48-1	糜棱岩化花岗岩	446	Yuan et al. （2018）
	X10-49-1	糜棱岩化花岗岩	444	Yuan et al. （2018）
	X10-50-1	糜棱岩化花岗岩	443	Yuan et al. （2018）
	X10-54-1	糜棱岩化花岗岩	438	Yuan et al. （2018）
	X10-51-1	糜棱岩化花岗岩	434	Yuan et al. （2018）
	X10-52-1	糜棱岩化花岗岩	430	Yuan et al. （2018）
	BA11-87	石英闪长岩	435	Zheng et al. （2018）
	BA11-91	石英二长岩	421	Zheng et al. （2018）
	BA11-96	花岗岩	401	Zheng et al. （2018）
	BA11-118	花岗闪长岩	434	Zheng et al. （2018）
	BA11-130	花岗岩	402	Zheng et al. （2018）
双鹰山–花牛山单元	LY-2-55	辉铜山东二长花岗岩	397	赵泽辉等（2007）
	LY-12-17	辉铜山东花岗岩闪长岩	423	赵泽辉等 （2007）
	LY-2-27	辉铜山东钾长花岗岩	436	赵泽辉等 （2007）
	TW-2	红脊山二长花岗岩	437	张新虎等（2008）
	SF07	双峰山正长花岗岩	415	李舢等 （2009）
	B70823-8	辉铜山钾长花岗岩	397	李舢等 （2011）
	LYB19	辉铜山片麻状黑云母花岗岩	424	毛启贵等 （2010）
	08L05	柳园英安斑岩	374	Mao et al. （2012）
	10MZS04	黑云斜长片麻岩	374	Song et al. （2013）
	SJP-3R	拾金坡黑云母二长花岗岩	406	朱江（2013）
	HTS-1	辉铜山钾长花岗岩	424	朱江（2013）
	BST	白山堂流纹斑岩	375	朱江（2013）
	XJ11-140	明舒井闪长岩	437	李小菲等（2015）
	XJ11-143	明舒井花岗岩	436	李小菲等（2015）
	PM019RZ1	黄草滩闪长岩	402	王疆涛等（2016）
双鹰山–花牛山单元	D0276RZ1	黄草滩花岗闪长岩	394	王疆涛等（2016）
	XQD-TW	小泉东花岗闪长斑岩	396	王怀涛（2019）
	HN4-1	花牛山石英闪长岩	363	王怀涛（2019）
	TW6239-1	双峰山南黑云母二长花岗岩	368	吕鑫等（2022）
	TW6237-3	双峰山南黑云母花岗闪长岩	366	吕鑫等（2022）
	PM011-2	明舒井二长花岗岩	423	王红杰等 （2024）
	D0600-19	明舒井正长花岗岩	425	王红杰等 （2024）
	D3782-1	明舒井花岗闪长岩	438	王红杰等 （2024）
	PM115TW9	歪咀山石英闪长岩	427	本文
	TW8813	歪咀山花岗闪长岩	419	本文
石板山单元	X10-128-1-01	金塔钾长花岗岩	435	贺振宇等 （2014）
	X10-98-2-01	桥湾糜棱岩化花岗岩	433	贺振宇等 （2014）
伊犁地块	D1011	石英二长岩	446	Gou L L and Zhang L F（2016）
	D1021	石英二长岩	443	Gou L L and Zhang LF（2016）
	w8034	糜棱岩化二长岩	453	Gou L L and Zhang L F（2016）
	13ts15B	二长花岗岩	411	Zhong et al. （2017）
	TKSB14-1	花岗闪长岩	370	Huang et al. （2020）
	ZS21	二长花岗岩	362	Bao et al. （2018）
	ZS34	钾长花岗岩	360	Bao et al. （2018）
	ZS1-1	花岗闪长岩	485	徐学义等（2010）
	KK1-1	黑云二长花岗岩	426	徐学义等 （2010）
	KK3-1	黑云母花岗岩	407	徐学义等 （2010）
	TL1-2	二长花岗岩	366	徐学义等（2010）
	XXY1-1	花岗闪长岩	430	徐学义等 （2010）
中天山地块	782	钾长花岗岩	434	Ma et al. （2014）
	784	花岗闪长岩	451	Ma et al. （2014）
	638	片麻状花岗闪长岩	475	Ma et al. （2014）
	BDB-12	花岗闪长岩	432	黄河等 （2015）
	BLT02	花岗闪长岩	473	Shi et al. （2014）
	XSS1	黑云母花岗岩	458	Shi et al. （2014）
	XSS2	花岗岩	404	Shi et al. （2014）
	791	钾长花岗岩	366	Ma et al. （2014）
	TKST-11	黑云母花岗岩	362	黄河等 （2015）
	TS1342	二长花岗岩	362	Yin et al. （2016）
	12ts30-1	糜棱岩化钾长花岗岩	417	Zhong et al. （2015）
	XXX01	花岗岩	393	Shi et al. （2014）
	YSG12	花岗岩	399	Shi et al. （2014）

), ArticleFig(id=1307087579929666018, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=表1, caption=

北山造山带、伊犁地块、中天山地块古生代岩浆岩（500～350 Ma）侵位年龄

, figureFileSmall=null, figureFileBig=null, tableContent=

构造单元	样品名	岩性	年龄（Ma）	参考文献
黑鹰山–旱山单元	BS041	片麻状花岗岩	423	刘雪敏等（2010）
	10SYQ07	眼球状片麻岩	499	Song et al. （2013）
	10SYQ08	糜棱岩化花岗岩	474	Song et al. （2013）
	10SYQ03	花岗片麻岩	471	Song et al. （2013）
	10SYQ05	糜棱岩化花岗岩	448	Song et al. （2013）
	X10-70-1-01	石板井糜棱岩化花岗岩	464	Yuan et al. （2018）
	X10-71-1-01	石板井糜棱岩化花岗岩	455	Yuan et al. （2018）
	X10-73-1-01	石板井闪长岩	450	Yuan et al. （2018）
	X10-69-1-10	石板井糜棱岩化花岗岩	445	Yuan et al. （2018）
	X10-77-1-01	石板井糜棱岩化花岗岩	439	Yuan et al. （2018）
	X10-72-1-03	石板井糜棱岩化花岗岩	433	Yuan et al. （2018）
	X10-77-2-01	石板井石英二长岩	428	Yuan et al. （2018）
	TW12	二长花岗岩	442	胡新茁等（2024）
	P7TW2	花岗闪长岩	443	胡新茁等 （2024）
马鬃山单元	BS07-136	公婆泉花岗岩	402	郑荣国等（2012）
	1122CL	白圪塔石英闪长岩	436	李小菲（2013）
	1129HTJ	白圪塔二长花岗岩	435	李小菲（2013）
	1131CG-6	白圪塔花岗闪长岩	431	李小菲（2013）
	1132WG	马鬃山石英闪长岩	367	李小菲（2013）
	X10-48-1	糜棱岩化花岗岩	446	Yuan et al. （2018）
	X10-49-1	糜棱岩化花岗岩	444	Yuan et al. （2018）
	X10-50-1	糜棱岩化花岗岩	443	Yuan et al. （2018）
	X10-54-1	糜棱岩化花岗岩	438	Yuan et al. （2018）
	X10-51-1	糜棱岩化花岗岩	434	Yuan et al. （2018）
	X10-52-1	糜棱岩化花岗岩	430	Yuan et al. （2018）
	BA11-87	石英闪长岩	435	Zheng et al. （2018）
	BA11-91	石英二长岩	421	Zheng et al. （2018）
	BA11-96	花岗岩	401	Zheng et al. （2018）
	BA11-118	花岗闪长岩	434	Zheng et al. （2018）
	BA11-130	花岗岩	402	Zheng et al. （2018）
双鹰山–花牛山单元	LY-2-55	辉铜山东二长花岗岩	397	赵泽辉等（2007）
	LY-12-17	辉铜山东花岗岩闪长岩	423	赵泽辉等 （2007）
	LY-2-27	辉铜山东钾长花岗岩	436	赵泽辉等 （2007）
	TW-2	红脊山二长花岗岩	437	张新虎等（2008）
	SF07	双峰山正长花岗岩	415	李舢等 （2009）
	B70823-8	辉铜山钾长花岗岩	397	李舢等 （2011）
	LYB19	辉铜山片麻状黑云母花岗岩	424	毛启贵等 （2010）
	08L05	柳园英安斑岩	374	Mao et al. （2012）
	10MZS04	黑云斜长片麻岩	374	Song et al. （2013）
	SJP-3R	拾金坡黑云母二长花岗岩	406	朱江（2013）
	HTS-1	辉铜山钾长花岗岩	424	朱江（2013）
	BST	白山堂流纹斑岩	375	朱江（2013）
	XJ11-140	明舒井闪长岩	437	李小菲等（2015）
	XJ11-143	明舒井花岗岩	436	李小菲等（2015）
	PM019RZ1	黄草滩闪长岩	402	王疆涛等（2016）
双鹰山–花牛山单元	D0276RZ1	黄草滩花岗闪长岩	394	王疆涛等（2016）
	XQD-TW	小泉东花岗闪长斑岩	396	王怀涛（2019）
	HN4-1	花牛山石英闪长岩	363	王怀涛（2019）
	TW6239-1	双峰山南黑云母二长花岗岩	368	吕鑫等（2022）
	TW6237-3	双峰山南黑云母花岗闪长岩	366	吕鑫等（2022）
	PM011-2	明舒井二长花岗岩	423	王红杰等 （2024）
	D0600-19	明舒井正长花岗岩	425	王红杰等 （2024）
	D3782-1	明舒井花岗闪长岩	438	王红杰等 （2024）
	PM115TW9	歪咀山石英闪长岩	427	本文
	TW8813	歪咀山花岗闪长岩	419	本文
石板山单元	X10-128-1-01	金塔钾长花岗岩	435	贺振宇等 （2014）
	X10-98-2-01	桥湾糜棱岩化花岗岩	433	贺振宇等 （2014）
伊犁地块	D1011	石英二长岩	446	Gou L L and Zhang L F（2016）
	D1021	石英二长岩	443	Gou L L and Zhang LF（2016）
	w8034	糜棱岩化二长岩	453	Gou L L and Zhang L F（2016）
	13ts15B	二长花岗岩	411	Zhong et al. （2017）
	TKSB14-1	花岗闪长岩	370	Huang et al. （2020）
	ZS21	二长花岗岩	362	Bao et al. （2018）
	ZS34	钾长花岗岩	360	Bao et al. （2018）
	ZS1-1	花岗闪长岩	485	徐学义等（2010）
	KK1-1	黑云二长花岗岩	426	徐学义等 （2010）
	KK3-1	黑云母花岗岩	407	徐学义等 （2010）
	TL1-2	二长花岗岩	366	徐学义等（2010）
	XXY1-1	花岗闪长岩	430	徐学义等 （2010）
中天山地块	782	钾长花岗岩	434	Ma et al. （2014）
	784	花岗闪长岩	451	Ma et al. （2014）
	638	片麻状花岗闪长岩	475	Ma et al. （2014）
	BDB-12	花岗闪长岩	432	黄河等 （2015）
	BLT02	花岗闪长岩	473	Shi et al. （2014）
	XSS1	黑云母花岗岩	458	Shi et al. （2014）
	XSS2	花岗岩	404	Shi et al. （2014）
	791	钾长花岗岩	366	Ma et al. （2014）
	TKST-11	黑云母花岗岩	362	黄河等 （2015）
	TS1342	二长花岗岩	362	Yin et al. （2016）
	12ts30-1	糜棱岩化钾长花岗岩	417	Zhong et al. （2015）
	XXX01	花岗岩	393	Shi et al. （2014）
	YSG12	花岗岩	399	Shi et al. （2014）

), ArticleFig(id=1307087580273598947, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Tab.2, caption=

LA-ICP-MS zircon U-Pb analytical data of the Waizuishan pluton

, figureFileSmall=null, figureFileBig=null, tableContent=

测点号	含量（10−6）			Th/U	同位素比值							年龄（Ma）
	Pb	Th	U		206Pb/238U	1σ	207Pb/235U	1σ	207Pb/206Pb	1σ		206Pb/238U	1σ	207Pb/235U	1σ	207Pb/206Pb	1σ
PM115TW9 花岗闪长岩 20个测点的加权平均年龄为427.1±3.4 Ma, MSWD=2.4
1	46	363	629	0.58	0.0704	0.0008	0.5477	0.0089	0.0564	0.0007		439	5	443	7	468	29
2	56	472	778	0.61	0.0693	0.0008	0.5365	0.0092	0.0561	0.0007		432	5	436	8	458	29
3	51	408	715	0.57	0.0687	0.0007	0.5404	0.0083	0.0571	0.0007		428	5	439	7	494	28
4	38	311	551	0.56	0.0673	0.0007	0.5336	0.0083	0.0575	0.0008		420	4	434	7	511	29
5	52	529	725	0.73	0.0671	0.0007	0.5285	0.0085	0.0571	0.0007		419	4	431	7	496	28
6	53	392	747	0.52	0.0691	0.0008	0.5409	0.0092	0.0568	0.0007		431	5	439	7	483	28
7	59	568	818	0.69	0.0680	0.0007	0.5130	0.0081	0.0547	0.0007		424	5	420	7	401	29
8	67	654	898	0.73	0.0689	0.0008	0.5471	0.0095	0.0576	0.0007		430	5	443	8	513	28
9	49	340	685	0.50	0.0693	0.0008	0.5257	0.0088	0.0551	0.0007		432	5	429	7	414	29
10	41	361	568	0.64	0.0685	0.0008	0.5374	0.0090	0.0569	0.0007		427	5	437	7	488	29
11	39	306	553	0.55	0.0682	0.0007	0.5235	0.0085	0.0557	0.0007		425	5	427	7	438	29
12	48	361	658	0.55	0.0698	0.0008	0.5413	0.0090	0.0562	0.0007		435	5	439	7	462	28
13	31	215	449	0.48	0.0678	0.0007	0.5059	0.0083	0.0542	0.0007		423	4	416	7	377	30
14	39	305	556	0.55	0.0683	0.0007	0.4984	0.0081	0.0530	0.0007		426	4	411	7	327	30
15	33	321	443	0.73	0.0703	0.0008	0.5201	0.0086	0.0537	0.0007		438	5	425	7	357	30
16	26	186	390	0.48	0.0658	0.0007	0.4941	0.0086	0.0545	0.0008		411	5	408	7	390	32
17	37	295	535	0.55	0.0685	0.0008	0.5281	0.0098	0.0559	0.0008		427	5	431	8	450	31
18	40	300	570	0.53	0.0695	0.0007	0.5222	0.0083	0.0545	0.0007		433	5	427	7	391	29
19	74	730	1062	0.69	0.0669	0.0007	0.5101	0.0081	0.0553	0.0007		417	5	419	7	424	28
20	43	404	595	0.68	0.0699	0.0007	0.5379	0.0086	0.0559	0.0007		435	4	437	7	446	29
TW8813 花岗闪长岩 20个测点的加权平均年龄为418.6±2.8Ma, MSWD=1.8
1	29	194	418	0.46	0.0690	0.0008	0.5117	0.0091	0.0538	0.0008		430	5	420	7	362	32
2	37	259	530	0.49	0.0681	0.0008	0.5188	0.0088	0.0552	0.0008		425	5	424	7	422	30
3	37	266	548	0.49	0.0677	0.0007	0.5002	0.0083	0.0536	0.0007		422	5	412	7	355	30
4	61	431	891	0.48	0.0681	0.0008	0.5085	0.0082	0.0542	0.0007		424	5	417	7	379	30
5	27	168	401	0.42	0.0687	0.0009	0.5174	0.0103	0.0547	0.0008		428	6	423	8	398	33
6	26	168	390	0.43	0.0675	0.0008	0.4895	0.0092	0.0526	0.0008		421	5	405	8	311	35
7	31	198	453	0.44	0.0681	0.0007	0.5195	0.0093	0.0553	0.0008		425	5	425	8	424	33
8	29	169	441	0.38	0.0676	0.0007	0.4967	0.0090	0.0533	0.0008		421	4	409	7	342	36
9	25	150	382	0.39	0.0675	0.0007	0.5080	0.0090	0.0545	0.0008		421	4	417	7	393	35
10	37	237	551	0.43	0.0675	0.0007	0.5015	0.0087	0.0539	0.0008		421	5	413	7	366	33
11	44	326	664	0.49	0.0664	0.0007	0.4864	0.0082	0.0531	0.0008		414	4	402	7	334	33
12	50	383	758	0.50	0.0653	0.0007	0.5166	0.0083	0.0574	0.0008		408	4	423	7	506	29
13	45	403	667	0.60	0.0660	0.0007	0.4901	0.0077	0.0539	0.0007		412	4	405	6	365	30
14	48	372	685	0.54	0.0674	0.0007	0.5245	0.0082	0.0564	0.0008		420	4	428	7	470	31
15	30	202	452	0.45	0.0663	0.0007	0.5082	0.0086	0.0556	0.0008		414	4	417	7	437	33
16	47	372	692	0.54	0.0664	0.0007	0.5198	0.0092	0.0568	0.0008		414	4	425	8	483	31
17	29	198	425	0.47	0.0667	0.0007	0.4998	0.0082	0.0544	0.0008		416	4	412	7	386	32
18	47	393	702	0.56	0.0655	0.0007	0.5246	0.0084	0.0581	0.0008		409	4	428	7	532	29
19	32	256	471	0.54	0.0664	0.0007	0.5019	0.0085	0.0548	0.0008		415	4	413	7	403	33
20	28	223	409	0.55	0.0678	0.0007	0.5559	0.0098	0.0594	0.0009		423	4	449	8	583	32

), ArticleFig(id=1307087580357485028, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=表2, caption=

歪咀山岩体的锆石LA-ICP-MS U-Pb分析结果

, figureFileSmall=null, figureFileBig=null, tableContent=

测点号	含量（10−6）			Th/U	同位素比值							年龄（Ma）
	Pb	Th	U		206Pb/238U	1σ	207Pb/235U	1σ	207Pb/206Pb	1σ		206Pb/238U	1σ	207Pb/235U	1σ	207Pb/206Pb	1σ
PM115TW9 花岗闪长岩 20个测点的加权平均年龄为427.1±3.4 Ma, MSWD=2.4
1	46	363	629	0.58	0.0704	0.0008	0.5477	0.0089	0.0564	0.0007		439	5	443	7	468	29
2	56	472	778	0.61	0.0693	0.0008	0.5365	0.0092	0.0561	0.0007		432	5	436	8	458	29
3	51	408	715	0.57	0.0687	0.0007	0.5404	0.0083	0.0571	0.0007		428	5	439	7	494	28
4	38	311	551	0.56	0.0673	0.0007	0.5336	0.0083	0.0575	0.0008		420	4	434	7	511	29
5	52	529	725	0.73	0.0671	0.0007	0.5285	0.0085	0.0571	0.0007		419	4	431	7	496	28
6	53	392	747	0.52	0.0691	0.0008	0.5409	0.0092	0.0568	0.0007		431	5	439	7	483	28
7	59	568	818	0.69	0.0680	0.0007	0.5130	0.0081	0.0547	0.0007		424	5	420	7	401	29
8	67	654	898	0.73	0.0689	0.0008	0.5471	0.0095	0.0576	0.0007		430	5	443	8	513	28
9	49	340	685	0.50	0.0693	0.0008	0.5257	0.0088	0.0551	0.0007		432	5	429	7	414	29
10	41	361	568	0.64	0.0685	0.0008	0.5374	0.0090	0.0569	0.0007		427	5	437	7	488	29
11	39	306	553	0.55	0.0682	0.0007	0.5235	0.0085	0.0557	0.0007		425	5	427	7	438	29
12	48	361	658	0.55	0.0698	0.0008	0.5413	0.0090	0.0562	0.0007		435	5	439	7	462	28
13	31	215	449	0.48	0.0678	0.0007	0.5059	0.0083	0.0542	0.0007		423	4	416	7	377	30
14	39	305	556	0.55	0.0683	0.0007	0.4984	0.0081	0.0530	0.0007		426	4	411	7	327	30
15	33	321	443	0.73	0.0703	0.0008	0.5201	0.0086	0.0537	0.0007		438	5	425	7	357	30
16	26	186	390	0.48	0.0658	0.0007	0.4941	0.0086	0.0545	0.0008		411	5	408	7	390	32
17	37	295	535	0.55	0.0685	0.0008	0.5281	0.0098	0.0559	0.0008		427	5	431	8	450	31
18	40	300	570	0.53	0.0695	0.0007	0.5222	0.0083	0.0545	0.0007		433	5	427	7	391	29
19	74	730	1062	0.69	0.0669	0.0007	0.5101	0.0081	0.0553	0.0007		417	5	419	7	424	28
20	43	404	595	0.68	0.0699	0.0007	0.5379	0.0086	0.0559	0.0007		435	4	437	7	446	29
TW8813 花岗闪长岩 20个测点的加权平均年龄为418.6±2.8Ma, MSWD=1.8
1	29	194	418	0.46	0.0690	0.0008	0.5117	0.0091	0.0538	0.0008		430	5	420	7	362	32
2	37	259	530	0.49	0.0681	0.0008	0.5188	0.0088	0.0552	0.0008		425	5	424	7	422	30
3	37	266	548	0.49	0.0677	0.0007	0.5002	0.0083	0.0536	0.0007		422	5	412	7	355	30
4	61	431	891	0.48	0.0681	0.0008	0.5085	0.0082	0.0542	0.0007		424	5	417	7	379	30
5	27	168	401	0.42	0.0687	0.0009	0.5174	0.0103	0.0547	0.0008		428	6	423	8	398	33
6	26	168	390	0.43	0.0675	0.0008	0.4895	0.0092	0.0526	0.0008		421	5	405	8	311	35
7	31	198	453	0.44	0.0681	0.0007	0.5195	0.0093	0.0553	0.0008		425	5	425	8	424	33
8	29	169	441	0.38	0.0676	0.0007	0.4967	0.0090	0.0533	0.0008		421	4	409	7	342	36
9	25	150	382	0.39	0.0675	0.0007	0.5080	0.0090	0.0545	0.0008		421	4	417	7	393	35
10	37	237	551	0.43	0.0675	0.0007	0.5015	0.0087	0.0539	0.0008		421	5	413	7	366	33
11	44	326	664	0.49	0.0664	0.0007	0.4864	0.0082	0.0531	0.0008		414	4	402	7	334	33
12	50	383	758	0.50	0.0653	0.0007	0.5166	0.0083	0.0574	0.0008		408	4	423	7	506	29
13	45	403	667	0.60	0.0660	0.0007	0.4901	0.0077	0.0539	0.0007		412	4	405	6	365	30
14	48	372	685	0.54	0.0674	0.0007	0.5245	0.0082	0.0564	0.0008		420	4	428	7	470	31
15	30	202	452	0.45	0.0663	0.0007	0.5082	0.0086	0.0556	0.0008		414	4	417	7	437	33
16	47	372	692	0.54	0.0664	0.0007	0.5198	0.0092	0.0568	0.0008		414	4	425	8	483	31
17	29	198	425	0.47	0.0667	0.0007	0.4998	0.0082	0.0544	0.0008		416	4	412	7	386	32
18	47	393	702	0.56	0.0655	0.0007	0.5246	0.0084	0.0581	0.0008		409	4	428	7	532	29
19	32	256	471	0.54	0.0664	0.0007	0.5019	0.0085	0.0548	0.0008		415	4	413	7	403	33
20	28	223	409	0.55	0.0678	0.0007	0.5559	0.0098	0.0594	0.0009		423	4	449	8	583	32

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Whole-rock major (%) and trace (10⁻⁶) element data of the Waizuishan pluton

, figureFileSmall=null, figureFileBig=null, tableContent=

样号	Pm115YQ9	Pm115YQ16	Pm115YQ21	YQ8813	YQ8814	YQ8816
SiO2	60.83	59.13	67.30	60.69	61.48	58.48
TiO2	0.68	0.76	0.52	0.69	0.62	0.98
Al2O3	16.61	16.91	14.96	16.84	16.84	16.11
Fe2O3	2.02	2.24	1.64	1.89	2.19	2.25
FeO	3.41	3.43	2.08	3.35	2.77	4.58
MnO	0.089	0.086	0.063	0.091	0.091	0.12
MgO	2.98	3.20	2.00	3.27	2.79	4.13
CaO	5.40	5.78	3.60	5.44	5.25	5.33
Na2O	3.47	3.68	3.30	3.74	3.76	3.42
K2O	2.80	2.22	3.42	2.14	2.45	2.53
P2O5	0.19	0.20	0.13	0.19	0.18	0.26
H2O+	0.71	1.25	0.68	0.98	0.93	0.96
H2O−	0.15	0.16	0.19	0.26	0.21	0.22
灼失量	1.36	2.20	0.85	1.53	1.45	1.67
V	116.13	125.01	91.92	134.86	136.43	162.87
Cr	36.18	38.95	35.05	37.57	23.29	46.82
Co	17.02	19.42	11.55	17.33	15.39	23.50
Ni	24.53	27.11	19.41	24.66	18.14	32.34
Sc	13.70	14.75	8.72	10.16	10.92	12.71
Cs	6.25	3.15	3.50	4.56	4.24	3.94
Rb	93.87	82.61	102.68	96.05	109.97	106.86
Sr	498.40	557.85	391.48	522.70	522.63	531.49
Ba	565.97	476.51	476.80	507.86	485.75	515.39
Ga	20.50	21.87	17.68	20.38	21.34	22.92
Nb	9.31	7.28	9.94	8.29	9.91	14.87
Ta	0.94	0.41	0.94	0.54	0.90	1.24
Zr	185.44	130.99	112.05	155.64	143.06	195.22
Hf	5.95	4.26	3.52	4.12	4.00	5.96
Th	33.98	6.60	31.79	5.19	13.98	7.50
U	3.65	2.32	4.39	3.13	3.77	2.92
Pb	18.80	14.70	16.90	16.00	18.50	10.90
La	49.82	27.34	32.15	18.43	32.35	24.22
Ce	88.73	43.23	47.98	45.71	64.86	61.38
Pr	9.61	5.55	5.52	5.29	6.23	7.10
Nd	30.75	20.71	19.05	21.12	22.51	28.53
Sm	4.95	3.92	3.28	4.07	4.02	5.56
Eu	1.16	1.05	0.90	1.01	1.09	1.42
Gd	4.91	3.53	3.14	3.48	3.88	4.64
Tb	0.65	0.54	0.45	0.52	0.54	0.72
Dy	3.14	2.75	2.23	2.89	2.99	4.06
Ho	0.58	0.51	0.41	0.52	0.54	0.73
Er	1.62	1.36	1.18	1.51	1.61	2.21
Tm	0.26	0.22	0.20	0.24	0.26	0.34
Yb	1.60	1.38	1.35	1.49	1.57	2.20
Lu	0.22	0.18	0.19	0.22	0.25	0.35
Y	18.03	14.72	12.90	14.95	15.76	22.14
Na2O+K2O	6.36	6.04	6.78	5.98	6.31	6.06
K2O/Na2O	0.81	0.60	1.04	0.57	0.65	0.74
A/CNK	0.90	0.89	0.95	0.92	0.92	0.89
A/NK	1.90	2.00	1.64	1.99	1.90	1.93
FeO*	5.23	5.44	3.56	5.05	4.73	6.61
Mg#	36.35	37.07	36.02	39.29	37.04	38.43
LREE/HREE	14.26	9.73	11.91	8.79	11.26	8.40
δEu	0.72	0.86	0.86	0.82	0.84	0.86
（La/Yb）N	22.31	14.23	17.08	8.87	14.74	7.91
10000 Ga/Al	2.33	2.44	2.23	2.29	2.39	2.69
R1	2131	2089	2485	2185	2157	2044
R2	1068	1136	785	1093	1047	1111
Nb/La	0.19	0.27	0.31	0.45	0.31	0.61
Ta/Yb	0.59	0.30	0.69	0.36	0.57	0.56

), ArticleFig(id=1307087580734972390, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=表3, caption=

歪咀山岩体的全岩主量元素（%）和微量元素（10⁻⁶）分析结果

, figureFileSmall=null, figureFileBig=null, tableContent=

样号	Pm115YQ9	Pm115YQ16	Pm115YQ21	YQ8813	YQ8814	YQ8816
SiO2	60.83	59.13	67.30	60.69	61.48	58.48
TiO2	0.68	0.76	0.52	0.69	0.62	0.98
Al2O3	16.61	16.91	14.96	16.84	16.84	16.11
Fe2O3	2.02	2.24	1.64	1.89	2.19	2.25
FeO	3.41	3.43	2.08	3.35	2.77	4.58
MnO	0.089	0.086	0.063	0.091	0.091	0.12
MgO	2.98	3.20	2.00	3.27	2.79	4.13
CaO	5.40	5.78	3.60	5.44	5.25	5.33
Na2O	3.47	3.68	3.30	3.74	3.76	3.42
K2O	2.80	2.22	3.42	2.14	2.45	2.53
P2O5	0.19	0.20	0.13	0.19	0.18	0.26
H2O+	0.71	1.25	0.68	0.98	0.93	0.96
H2O−	0.15	0.16	0.19	0.26	0.21	0.22
灼失量	1.36	2.20	0.85	1.53	1.45	1.67
V	116.13	125.01	91.92	134.86	136.43	162.87
Cr	36.18	38.95	35.05	37.57	23.29	46.82
Co	17.02	19.42	11.55	17.33	15.39	23.50
Ni	24.53	27.11	19.41	24.66	18.14	32.34
Sc	13.70	14.75	8.72	10.16	10.92	12.71
Cs	6.25	3.15	3.50	4.56	4.24	3.94
Rb	93.87	82.61	102.68	96.05	109.97	106.86
Sr	498.40	557.85	391.48	522.70	522.63	531.49
Ba	565.97	476.51	476.80	507.86	485.75	515.39
Ga	20.50	21.87	17.68	20.38	21.34	22.92
Nb	9.31	7.28	9.94	8.29	9.91	14.87
Ta	0.94	0.41	0.94	0.54	0.90	1.24
Zr	185.44	130.99	112.05	155.64	143.06	195.22
Hf	5.95	4.26	3.52	4.12	4.00	5.96
Th	33.98	6.60	31.79	5.19	13.98	7.50
U	3.65	2.32	4.39	3.13	3.77	2.92
Pb	18.80	14.70	16.90	16.00	18.50	10.90
La	49.82	27.34	32.15	18.43	32.35	24.22
Ce	88.73	43.23	47.98	45.71	64.86	61.38
Pr	9.61	5.55	5.52	5.29	6.23	7.10
Nd	30.75	20.71	19.05	21.12	22.51	28.53
Sm	4.95	3.92	3.28	4.07	4.02	5.56
Eu	1.16	1.05	0.90	1.01	1.09	1.42
Gd	4.91	3.53	3.14	3.48	3.88	4.64
Tb	0.65	0.54	0.45	0.52	0.54	0.72
Dy	3.14	2.75	2.23	2.89	2.99	4.06
Ho	0.58	0.51	0.41	0.52	0.54	0.73
Er	1.62	1.36	1.18	1.51	1.61	2.21
Tm	0.26	0.22	0.20	0.24	0.26	0.34
Yb	1.60	1.38	1.35	1.49	1.57	2.20
Lu	0.22	0.18	0.19	0.22	0.25	0.35
Y	18.03	14.72	12.90	14.95	15.76	22.14
Na2O+K2O	6.36	6.04	6.78	5.98	6.31	6.06
K2O/Na2O	0.81	0.60	1.04	0.57	0.65	0.74
A/CNK	0.90	0.89	0.95	0.92	0.92	0.89
A/NK	1.90	2.00	1.64	1.99	1.90	1.93
FeO*	5.23	5.44	3.56	5.05	4.73	6.61
Mg#	36.35	37.07	36.02	39.29	37.04	38.43
LREE/HREE	14.26	9.73	11.91	8.79	11.26	8.40
δEu	0.72	0.86	0.86	0.82	0.84	0.86
（La/Yb）N	22.31	14.23	17.08	8.87	14.74	7.91
10000 Ga/Al	2.33	2.44	2.23	2.29	2.39	2.69
R1	2131	2089	2485	2185	2157	2044
R2	1068	1136	785	1093	1047	1111
Nb/La	0.19	0.27	0.31	0.45	0.31	0.61
Ta/Yb	0.59	0.30	0.69	0.36	0.57	0.56

), ArticleFig(id=1307087580885967335, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=EN, label=Tab.4, caption=

Hf isotopic data for zircons of the Waizuishan pluton

, figureFileSmall=null, figureFileBig=null, tableContent=

测点号	年龄（Ma）	176Yb/177Hf	1σ	176Lu/177Hf	1σ	176Hf/177Hf	1σ	176Hf/177Hfi	eHf（0）	eHf（t）	TDM （Ma）	TDMC （Ma）	fLu/Hf
PM115TW9：20个测点加权平均年龄（427.1 ± 3.4） Ma, MSWD = 2.4
01	439	0.035765	0.000518	0.001013	0.000009	0.282508	0.000013	0.282500	−9.3	0.0	1053	1420	−0.97
02	432	0.015118	0.000227	0.000463	0.000003	0.282501	0.000012	0.282497	−9.6	−0.2	1047	1429	−0.99
03	428	0.028509	0.000368	0.000884	0.000008	0.282505	0.000014	0.282498	−9.4	−0.3	1053	1430	−0.97
04	420	0.020915	0.000094	0.000630	0.000003	0.282512	0.000012	0.282507	−9.2	−0.1	1037	1415	−0.98
05	419	0.040645	0.001288	0.001179	0.000030	0.282491	0.000015	0.282482	−9.9	−1.1	1081	1473	−0.96
06	431	0.023287	0.000187	0.000672	0.000004	0.282481	0.000013	0.282476	−10.3	−1.0	1080	1478	−0.98
07	424	0.034053	0.000263	0.000994	0.000006	0.282505	0.000012	0.282497	−9.4	−0.4	1056	1435	−0.97
08	430	0.021156	0.000692	0.000601	0.000016	0.282495	0.000013	0.282490	−9.8	−0.5	1059	1446	−0.98
09	432	0.025823	0.000150	0.000785	0.000003	0.282490	0.000013	0.282484	−10.0	−0.7	1071	1460	−0.98
10	427	0.021963	0.000189	0.000647	0.000005	0.282501	0.000012	0.282496	−9.6	−0.4	1053	1436	−0.98
11	425	0.017687	0.000157	0.000617	0.000006	0.282457	0.000013	0.282452	−11.1	−2.0	1113	1535	−0.98
12	435	0.030201	0.000385	0.000919	0.000019	0.282504	0.000013	0.282496	−9.5	−0.2	1056	1429	−0.97
13	423	0.019962	0.000117	0.000595	0.000006	0.282499	0.000012	0.282494	−9.7	−0.5	1054	1443	−0.98
14	426	0.020011	0.000492	0.000582	0.000009	0.282471	0.000013	0.282467	−10.6	−1.4	1092	1502	−0.98
15	438	0.039400	0.000233	0.001043	0.000012	0.282519	0.000013	0.282511	−8.9	0.4	1037	1395	−0.97
16	411	0.039359	0.000846	0.001174	0.000028	0.282489	0.000014	0.282480	−10.0	−1.3	1084	1482	−0.96
17	427	0.019749	0.000141	0.000579	0.000003	0.282505	0.000012	0.282501	−9.4	−0.2	1044	1425	−0.98
18	433	0.026524	0.000368	0.000761	0.000005	0.282485	0.000012	0.282478	−10.2	−0.9	1078	1471	−0.98
19	417	0.037198	0.000452	0.001055	0.000007	0.282514	0.000014	0.282506	−9.1	−0.2	1045	1419	−0.97
20	435	0.028414	0.000140	0.000843	0.000011	0.282510	0.000014	0.282503	−9.3	0.1	1045	1413	−0.97
TW8813：20个测点加权平均年龄418.6 ± 2.8 Ma, MSWD = 1.8
01	430	0.023624	0.000209	0.000721	0.000005	0.282520	0.000015	0.282514	−8.9	0.3	1028	1394	−0.98
02	425	0.019415	0.000072	0.000592	0.000005	0.282496	0.000013	0.282491	−9.8	−0.6	1058	1448	−0.98
03	422	0.014699	0.000190	0.000439	0.000003	0.282497	0.000013	0.282494	−9.7	−0.6	1052	1444	−0.99
04	424	0.027697	0.000648	0.000817	0.000011	0.282488	0.000012	0.282482	−10.0	−0.9	1075	1469	−0.98
05	428	0.030441	0.000339	0.000854	0.000003	0.282497	0.000012	0.282490	−9.7	−0.6	1064	1449	−0.97
06	421	0.016097	0.000118	0.000578	0.000010	0.282490	0.000012	0.282486	−10.0	−0.9	1065	1462	−0.98
07	425	0.021139	0.000326	0.000603	0.000007	0.282490	0.000012	0.282485	−10.0	−0.8	1067	1461	−0.98
08	421	0.022162	0.000131	0.000692	0.000004	0.282515	0.000012	0.282509	−9.1	0.0	1034	1409	−0.98
09	421	0.017558	0.000095	0.000514	0.000006	0.282502	0.000012	0.282498	−9.6	−0.4	1047	1435	−0.98
10	421	0.019321	0.000045	0.000575	0.000002	0.282504	0.000011	0.282500	−9.5	−0.4	1046	1431	−0.98
11	414	0.019847	0.000187	0.000567	0.000002	0.282507	0.000012	0.282502	−9.4	−0.4	1042	1430	−0.98
12	408	0.020279	0.000448	0.000598	0.000009	0.282488	0.000013	0.282484	−10.0	−1.2	1069	1476	−0.98
13	412	0.047310	0.000641	0.001343	0.000015	0.282505	0.000014	0.282495	−9.4	−0.7	1066	1448	−0.96
14	420	0.030907	0.000361	0.000876	0.000008	0.282489	0.000013	0.282482	−10.0	−1.0	1075	1471	−0.97
15	414	0.013487	0.000319	0.000403	0.000007	0.282535	0.000013	0.282532	−8.4	0.6	998	1362	−0.99
16	414	0.020755	0.000771	0.000640	0.000016	0.282463	0.000012	0.282458	−10.9	−2.0	1105	1528	−0.98
17	416	0.015991	0.000122	0.000476	0.000005	0.282490	0.000011	0.282487	−10.0	−0.9	1062	1463	−0.99
18	409	0.015802	0.000250	0.000486	0.000006	0.282515	0.000012	0.282511	−9.1	−0.2	1029	1413	−0.99
19	415	0.018577	0.000176	0.000601	0.000009	0.282493	0.000012	0.282489	−9.8	−0.9	1061	1459	−0.98
20	423	0.014677	0.000215	0.000460	0.000005	0.282524	0.000012	0.282520	−8.8	0.4	1016	1384	−0.99

), ArticleFig(id=1307087580974047720, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087562691076469, language=CN, label=表4, caption=

歪咀山岩体锆石Hf同位素组成

, figureFileSmall=null, figureFileBig=null, tableContent=

测点号	年龄（Ma）	176Yb/177Hf	1σ	176Lu/177Hf	1σ	176Hf/177Hf	1σ	176Hf/177Hfi	eHf（0）	eHf（t）	TDM （Ma）	TDMC （Ma）	fLu/Hf
PM115TW9：20个测点加权平均年龄（427.1 ± 3.4） Ma, MSWD = 2.4
01	439	0.035765	0.000518	0.001013	0.000009	0.282508	0.000013	0.282500	−9.3	0.0	1053	1420	−0.97
02	432	0.015118	0.000227	0.000463	0.000003	0.282501	0.000012	0.282497	−9.6	−0.2	1047	1429	−0.99
03	428	0.028509	0.000368	0.000884	0.000008	0.282505	0.000014	0.282498	−9.4	−0.3	1053	1430	−0.97
04	420	0.020915	0.000094	0.000630	0.000003	0.282512	0.000012	0.282507	−9.2	−0.1	1037	1415	−0.98
05	419	0.040645	0.001288	0.001179	0.000030	0.282491	0.000015	0.282482	−9.9	−1.1	1081	1473	−0.96
06	431	0.023287	0.000187	0.000672	0.000004	0.282481	0.000013	0.282476	−10.3	−1.0	1080	1478	−0.98
07	424	0.034053	0.000263	0.000994	0.000006	0.282505	0.000012	0.282497	−9.4	−0.4	1056	1435	−0.97
08	430	0.021156	0.000692	0.000601	0.000016	0.282495	0.000013	0.282490	−9.8	−0.5	1059	1446	−0.98
09	432	0.025823	0.000150	0.000785	0.000003	0.282490	0.000013	0.282484	−10.0	−0.7	1071	1460	−0.98
10	427	0.021963	0.000189	0.000647	0.000005	0.282501	0.000012	0.282496	−9.6	−0.4	1053	1436	−0.98
11	425	0.017687	0.000157	0.000617	0.000006	0.282457	0.000013	0.282452	−11.1	−2.0	1113	1535	−0.98
12	435	0.030201	0.000385	0.000919	0.000019	0.282504	0.000013	0.282496	−9.5	−0.2	1056	1429	−0.97
13	423	0.019962	0.000117	0.000595	0.000006	0.282499	0.000012	0.282494	−9.7	−0.5	1054	1443	−0.98
14	426	0.020011	0.000492	0.000582	0.000009	0.282471	0.000013	0.282467	−10.6	−1.4	1092	1502	−0.98
15	438	0.039400	0.000233	0.001043	0.000012	0.282519	0.000013	0.282511	−8.9	0.4	1037	1395	−0.97
16	411	0.039359	0.000846	0.001174	0.000028	0.282489	0.000014	0.282480	−10.0	−1.3	1084	1482	−0.96
17	427	0.019749	0.000141	0.000579	0.000003	0.282505	0.000012	0.282501	−9.4	−0.2	1044	1425	−0.98
18	433	0.026524	0.000368	0.000761	0.000005	0.282485	0.000012	0.282478	−10.2	−0.9	1078	1471	−0.98
19	417	0.037198	0.000452	0.001055	0.000007	0.282514	0.000014	0.282506	−9.1	−0.2	1045	1419	−0.97
20	435	0.028414	0.000140	0.000843	0.000011	0.282510	0.000014	0.282503	−9.3	0.1	1045	1413	−0.97
TW8813：20个测点加权平均年龄418.6 ± 2.8 Ma, MSWD = 1.8
01	430	0.023624	0.000209	0.000721	0.000005	0.282520	0.000015	0.282514	−8.9	0.3	1028	1394	−0.98
02	425	0.019415	0.000072	0.000592	0.000005	0.282496	0.000013	0.282491	−9.8	−0.6	1058	1448	−0.98
03	422	0.014699	0.000190	0.000439	0.000003	0.282497	0.000013	0.282494	−9.7	−0.6	1052	1444	−0.99
04	424	0.027697	0.000648	0.000817	0.000011	0.282488	0.000012	0.282482	−10.0	−0.9	1075	1469	−0.98
05	428	0.030441	0.000339	0.000854	0.000003	0.282497	0.000012	0.282490	−9.7	−0.6	1064	1449	−0.97
06	421	0.016097	0.000118	0.000578	0.000010	0.282490	0.000012	0.282486	−10.0	−0.9	1065	1462	−0.98
07	425	0.021139	0.000326	0.000603	0.000007	0.282490	0.000012	0.282485	−10.0	−0.8	1067	1461	−0.98
08	421	0.022162	0.000131	0.000692	0.000004	0.282515	0.000012	0.282509	−9.1	0.0	1034	1409	−0.98
09	421	0.017558	0.000095	0.000514	0.000006	0.282502	0.000012	0.282498	−9.6	−0.4	1047	1435	−0.98
10	421	0.019321	0.000045	0.000575	0.000002	0.282504	0.000011	0.282500	−9.5	−0.4	1046	1431	−0.98
11	414	0.019847	0.000187	0.000567	0.000002	0.282507	0.000012	0.282502	−9.4	−0.4	1042	1430	−0.98
12	408	0.020279	0.000448	0.000598	0.000009	0.282488	0.000013	0.282484	−10.0	−1.2	1069	1476	−0.98
13	412	0.047310	0.000641	0.001343	0.000015	0.282505	0.000014	0.282495	−9.4	−0.7	1066	1448	−0.96
14	420	0.030907	0.000361	0.000876	0.000008	0.282489	0.000013	0.282482	−10.0	−1.0	1075	1471	−0.97
15	414	0.013487	0.000319	0.000403	0.000007	0.282535	0.000013	0.282532	−8.4	0.6	998	1362	−0.99
16	414	0.020755	0.000771	0.000640	0.000016	0.282463	0.000012	0.282458	−10.9	−2.0	1105	1528	−0.98
17	416	0.015991	0.000122	0.000476	0.000005	0.282490	0.000011	0.282487	−10.0	−0.9	1062	1463	−0.99
18	409	0.015802	0.000250	0.000486	0.000006	0.282515	0.000012	0.282511	−9.1	−0.2	1029	1413	−0.99
19	415	0.018577	0.000176	0.000601	0.000009	0.282493	0.000012	0.282489	−9.8	−0.9	1061	1459	−0.98
20	423	0.014677	0.000215	0.000460	0.000005	0.282524	0.000012	0.282520	−8.8	0.4	1016	1384	−0.99

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