Article(id=1307087668471419404, tenantId=1146029695717560320, journalId=1306274195778404443, issueId=1307087507837964779, articleNumber=null, orderNo=null, doi=10.12401/j.nwg.2025164, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1764864000000, receivedDateStr=2025-12-05, revisedDate=1769097600000, revisedDateStr=2026-01-23, acceptedDate=1769616000000, acceptedDateStr=2026-01-29, onlineDate=1789563584677, onlineDateStr=2026-09-16, pubDate=1781884800000, pubDateStr=2026-06-20, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1789563584677, onlineIssueDateStr=2026-09-16, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1789563584677, creator=13701087609, updateTime=1789563584677, 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=314, endPage=327, ext={EN=ArticleExt(id=1307087668634997261, articleId=1307087668471419404, tenantId=1146029695717560320, journalId=1306274195778404443, language=EN, title=Petrogenesis and Geological Significance of the Taihua Group TTG Gneisses in the Xiong'ershan Area, Southern Margin of the North China Craton, columnId=null, journalTitle=Northwestern Geology, columnName=null, runingTitle=null, highlight=null, articleAbstract=

The North China Craton underwent a prolonged and complex geological evolution during the Archean to Paleoproterozoic, with the magmatic and metamorphic processes remain as the research questions. This study focuses on the TTG (tonalite-trondhjemite-granodiorite) gneisses of the Taihua Group in the Xiong’ershan area along the southern margin of the North China Craton. The integrated field investigations, petrographic analysis under the microscope, geochemistry, zircon U-Pb dating and Hf isotopic studies are conducted to elucidate the Paleoproterozoic magmatic mechanisms and the tectonic evolution of this region. Zircon U-Pb dating constrains the magmatic crystallization age of the Taihua Group TTG gneisses in the Xiong’ershan area to approximately 2300 Ma, while the metamorphic ages range from 1984 Ma to 1940 Ma. The Taihua Group TTG gneisses exhibit a wide compositional range, with SiO2 (59.35%~70.78%), Al2O3 (12.41%~17.93%), and relatively high CaO (1.40%~5.52%) and MgO (0.95%~2.56%) contents. It is enriched in light rare earth elements (LREE) and depleted in heavy rare earth elements (HREE), displaying strong fractionation between LREE and HREE. In composition, it resembles high-Al TTG gneisses. The samples are enriched in large-ion lithophile elements (LILEs) such as Rb, Ba, and Sr, but depleted in high-field-strength elements (HFSEs) like Nb, Ta, and Ti, which are similar to the features of island arc granites. Additionally, magmatic zircons display relatively high (176Hf/177Hf)ᵢ ratios (0.281282~0.281332), εHf(t) values (−2.98 ~ +0.20), and two-stage model ages (2844~2994 Ma), indicating that the magmatic source originated from the partial melting of Mesoarchean ancient crust. These findings suggest that the TTG gneisses in the Xiong’ershan area formed during the Paleoproterozoic subduction process between the eastern and western blocks of the North China Craton. The metamorphic age of 1984~1940 Ma records the collisional process along the Trans-North China Orogeny. This further constrains the timing of collision between the eastern and western continental blocks.

, authors=Wenting YAN1, Li TANG1, *, Qianmu YANG2, Liang WANG3, Longlong CHEN1, authorsList=Wenting YAN, Li TANG, Qianmu YANG, Liang WANG, Longlong CHEN, authorCompany=null, correspAuthors=Li TANG, 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=1307087671852028446, articleId=1307087668471419404, tenantId=1146029695717560320, journalId=1306274195778404443, language=CN, title=华北克拉通南缘熊耳山地区太华群TTG片麻岩成因及地质意义, columnId=1307047819974570720, journalTitle=西北地质, columnName=非主题, runingTitle=null, highlight=null, articleAbstract=

华北克拉通经历太古宙—古元古代漫长且复杂的地质演化历史,形成该稳定克拉通的岩浆作用和变质作用过程一直是学者们关注的焦点。笔者以华北克拉通南缘熊耳山地区太华群TTG(英云闪长岩–奥长花岗岩–花岗闪长岩)片麻岩为研究对象,基于详细的野外地质调查、室内镜下研究、岩石地球化学、锆石U-Pb定年和Hf同位素分析,揭示区内古元古代岩浆作用机制及其构造指示意义。熊耳山地区太华群TTG片麻岩的岩浆结晶年龄为2300 Ma,而变质年龄为1984~1940 Ma。太华群TTG片麻岩SiO2含量为59.35%~70.78%,Al2O3含量为12.41%~17.93%,CaO含量为1.40%~5.52%,MgO含量为0.95%~2.56%,富集轻稀土元素亏损重稀土元素,并表现出轻、重稀土元素强烈分异的特点,成分上类似于高铝型TTG 片麻岩。样品富集Rb、Ba、Sr等大离子亲石元素,亏损Nb、Ta、Ti等高场强元素,与岛弧花岗岩的特征相似。此外,岩浆锆石具有相对较高的 (176Hf/177Hf)i值(0.281282~0.281332),εHf(t)值(−2.98~0.20)和二阶段模式年龄(2844~2994 Ma),指示其岩浆源区为中太古代古老地壳的熔融。综合研究认为,熊耳山地区的TTG片麻岩形成于华北克拉通东、西部陆块之间的古元古代俯冲过程,其1984~1940 Ma的变质年龄记录沿中部造山带的碰撞拼合过程,进一步约束了东、西部陆块的碰撞时限。

, authors=严文婷1, 唐利1, *, 杨谦牧2, 王亮3, 陈龙龙1, authorsList=严文婷, 唐利, 杨谦牧, 王亮, 陈龙龙, authorCompany=null, correspAuthors=唐利, authorNote=

严文婷(2004−),女,本科生,资源勘查工程(固体矿产)专业。E−mail:

, correspAuthorsNote=
唐利(1990−),男,副教授,博士生导师,主要从事钼–金–稀土等关键金属矿床成因和成矿规律的研究和教学工作。E−mail:。
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严文婷(2004−),女,本科生,资源勘查工程(固体矿产)专业。E−mail:

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严文婷(2004−),女,本科生,资源勘查工程(固体矿产)专业。E−mail:

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articleId=1307087668471419404, language=CN, orderNo=2, keyword=TTG片麻岩), Keyword(id=1307087674364416585, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, orderNo=3, keyword=太华群), Keyword(id=1307087674456691274, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, orderNo=4, keyword=岩石成因), Keyword(id=1307087676109247051, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, orderNo=5, keyword=华北克拉通)], refs=[Reference(id=1307087678109930082, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2024, volume=57, issue=2, pageStart=67, pageEnd=89, url=null, language=null, rfNumber=1, rfOrder=0, authorNames=null, journalName=西北地质, refType=null, unstructuredReference=陈龙龙, 唐利, 沈彦谋, 等. 秦岭造山带栾川Mo-W矿集区和柞水–山阳Cu-Mo矿集区斑岩型矿床成矿差异性对比[J]. 西北地质, 2024, 57(2): 67−89., 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Mineralium Deposita, 2021, 56: 1133−1150., articleTitle=Magmatic-hydrothermal evolution of an unusual Mo-rich carbonatite: a case study using LA-ICP-MS fluid inclusion microanalysis and He–Ar isotopes from the Huangshui’an deposit, Qinling, China, refAbstract=null), Reference(id=1307087686011998878, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2024, volume=59, issue=2, pageStart=366, pageEnd=380, url=null, language=null, rfNumber=37, rfOrder=60, authorNames=null, journalName=Geological Journal, refType=null, unstructuredReference=Wang H H, Tang L, Santosh M, et al. Metamorphic evolution of garnet amphibolites from the Fuping Complex: Implications for the Paleoproterozoic subduction–collision history of the Trans‐North China Orogen[J]. Geological Journal, 2024, 59(2): 366−380., articleTitle=Metamorphic evolution of garnet amphibolites from the Fuping Complex: Implications for the Paleoproterozoic subduction–collision history of the Trans‐North China Orogen, refAbstract=null), Reference(id=1307087686095884959, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2025, volume=16, issue=2, pageStart=101990, pageEnd=null, url=null, language=null, rfNumber=38, rfOrder=61, authorNames=null, journalName=Geoscience Frontiers, refType=null, unstructuredReference=Zeng T, Tang L, Santosh M, et al. Neoarchean-Paleoproterozoic metallogenesis associated with plate tectonics in early Earth: Insights from the North China Craton[J]. Geoscience Frontiers, 2025, 16(2): 101990., articleTitle=Neoarchean-Paleoproterozoic metallogenesis associated with plate tectonics in early Earth: Insights from the North China Craton, refAbstract=null), Reference(id=1307087686162993824, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2011, volume=20, issue=null, pageStart=6, pageEnd=25, url=null, language=null, rfNumber=39, rfOrder=62, authorNames=null, journalName=Gondwana Research, refType=null, unstructuredReference=Zhai M G, Santosh M. The early Precambrian odyssey of the North China Craton: A synoptic overview[J]. Gondwana Research, 2011, 20: 6−25., articleTitle=The early Precambrian odyssey of the North China Craton: A synoptic overview, refAbstract=null), Reference(id=1307087686230102689, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2012, volume=222−223, issue=null, pageStart=55, pageEnd=76, url=null, language=null, rfNumber=40, rfOrder=63, authorNames=null, journalName=Precambrian Research, refType=null, unstructuredReference=Zhao G C, Cawood P A, Li S, et al. Amalgamation of the North China Craton: Key issues and discussion[J]. Precambrian Research, 2012, 222−223: 55−76., articleTitle=Amalgamation of the North China Craton: Key issues and discussion, refAbstract=null), Reference(id=1307087686301405858, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2005, volume=136, issue=3−4, pageStart=177, pageEnd=202, url=null, language=null, rfNumber=41, rfOrder=64, authorNames=null, journalName=Precambrian Research, refType=null, unstructuredReference=Zhao G C, Sun M, Wilde S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited[J]. Precambrian Research, 2005, 136(3−4): 177−202., articleTitle=Late Archean to Paleoproterozoic evolution of the North China Craton: key issues revisited, refAbstract=null), Reference(id=1307087686389486243, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2008, volume=160, issue=3, pageStart=213, pageEnd=226, url=null, language=null, rfNumber=42, rfOrder=65, authorNames=null, journalName=Precambrian Research, refType=null, unstructuredReference=Zhao G C, Wilde S A, Sun M, et al. SHRIMP U-Pb zircon ages of granitoid rocks in the Lüliang Complex: Implications for the accretion and evolution of the Trans-North China Orogen[J]. Precambrian Research, 2008, 160(3): 213−226., articleTitle=SHRIMP U-Pb zircon ages of granitoid rocks in the Lüliang Complex: Implications for the accretion and evolution of the Trans-North China Orogen, refAbstract=null), Reference(id=1307087686444012196, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, doi=null, pmid=null, pmcid=null, year=2013, volume=23, issue=4, pageStart=1207, pageEnd=1240, url=null, language=null, rfNumber=43, rfOrder=66, authorNames=null, journalName=Gondwana Research, refType=null, unstructuredReference=Zhao G, Zhai M. Lithotectonic elements of Precambrian basement in the North China Craton: Review and tectonic implications[J]. 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Qz. 石英;Pl. 斜长石;Hb. 角闪石

, figureFileSmall=NligiYmhzrHadIvFJU6myw==, figureFileBig=j5EBAZzqwKiap5UaBNrOqA==, tableContent=null), ArticleFig(id=1307087676662895184, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=EN, label=Fig.3, caption=(a) TAS classification diagram and, (b) SiO2-K2O discrimination diagram of the Taihua Group TTG gneiss in the Xiong'ershan area, figureFileSmall=EzPJvO4y7QuAWmypbE+1Eg==, figureFileBig=/2C8C/i4IFUSr/Lf6Rwlgw==, tableContent=null), ArticleFig(id=1307087676721615441, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=图3, caption=熊耳山地区太华群TTG片麻岩的TAS岩石分类图解(a;底图据Middlemost, 1994)、SiO2-K2O岩石系列判别图解(b;底图据Peccerillo et al., 1976), figureFileSmall=EzPJvO4y7QuAWmypbE+1Eg==, figureFileBig=/2C8C/i4IFUSr/Lf6Rwlgw==, tableContent=null), ArticleFig(id=1307087676797112914, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=EN, label=Fig.4, caption=(a) Chondrite normalized REE and (b) primitive mantle-normalized trace elements diagrams of the Taihua Group TTG gneisses, figureFileSmall=pJ8/BBo7wBJnVNEX6+5ihg==, figureFileBig=bWGrP/0ot9JCwyDMlZBoPA==, tableContent=null), ArticleFig(id=1307087676868416083, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=图4, caption=太华群 TTG 片麻岩球粒陨石标准化稀土元素配分曲线(a)及原始地幔标准化微量元素蛛网图(b)

球粒陨石和原始地幔均一化值来自Sun et al.(1989)

, figureFileSmall=pJ8/BBo7wBJnVNEX6+5ihg==, figureFileBig=bWGrP/0ot9JCwyDMlZBoPA==, tableContent=null), ArticleFig(id=1307087676948107860, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=EN, label=Fig.5, caption=(a, b) Zircon CL images and (c, d) zircon concordia diagrams of the Taihua Group TTG gneisses in the Xiong'ershan area, figureFileSmall=6K1M+F69h9SN3IrtSC4hXA==, figureFileBig=4zPCHO0hxDnBfeNDISAV7g==, tableContent=null), ArticleFig(id=1307087677040382549, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=图5, caption=熊耳山地区太华群TTG片麻岩锆石CL图像(a、b)和锆石谐和图(c、d), figureFileSmall=6K1M+F69h9SN3IrtSC4hXA==, figureFileBig=4zPCHO0hxDnBfeNDISAV7g==, tableContent=null), ArticleFig(id=1307087677111685718, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=EN, label=Fig.6, caption=Zircon Lu-Hf isotopic characteristics of TTG gneisses in the Xiong'ershan area, southern margin of the North China Craton, figureFileSmall=4kXPkquhXUZka7Qoc9L69g==, figureFileBig=EiPpILsUBFDN1aWoob0f+g==, tableContent=null), ArticleFig(id=1307087677174600279, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=图6, caption=华北克拉通南缘熊耳山地区TTG片麻岩的锆石Lu-Hf同位素特征, figureFileSmall=4kXPkquhXUZka7Qoc9L69g==, figureFileBig=EiPpILsUBFDN1aWoob0f+g==, tableContent=null), ArticleFig(id=1307087677237514840, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=EN, label=Fig.7, caption=(a) Discrimination diagrams of (La/Yb)N-(Yb)N and (b) Sr/Y-Y for TTG gneisses in the Xiong'ershan area, figureFileSmall=u/mdA2KwixMeHIumwKl0ew==, figureFileBig=OGC5wZIX8ZdARRcryfhnGA==, tableContent=null), ArticleFig(id=1307087677313012313, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=图7, caption=熊耳山地区 TTG 片麻岩(La/Yb)N-(Yb)N(a)和Sr/Y-Y 判别图解(b;底图据万建军,2016)

a. 源区为太古代镁铁质组分且残留相为榴辉岩;b. 源区为太古代镁铁质组分且残留相为10%石榴角闪岩;c. 源区为太平洋中脊玄武岩且残留相为榴辉岩;d. 源区为太平洋中脊玄武岩且残留相为10%石榴角闪岩:e. 榴辉岩的部分熔融;f. 石榴斜长角闪岩的部分熔融;g. 斜长角闪岩的部分熔融

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Major element (%) and trace element (10−6) analytical results of the Xiong'ershan TTG gneiss

, figureFileSmall=null, figureFileBig=null, tableContent=
样品编号20TH-0120TH-0220TH-0420TH-0520TH-0620TH-0720TH-08
SiO266.1961.7970.7863.9670.4668.9159.35
TiO20.390.500.550.440.420.430.59
Al2O315.9316.1813.3812.4113.2514.1017.93
Fe2O33.665.183.526.674.123.995.60
MnO0.050.070.060.140.040.050.11
MgO1.732.560.961.260.950.992.18
CaO4.484.532.832.871.403.165.53
Na2O3.993.894.072.092.523.684.25
K2O1.422.102.075.575.412.632.25
P2O50.090.080.140.110.090.100.15
LOI1.352.451.243.760.901.301.83
Total99.2899.3399.5899.2899.5699.3399.76
Li5.658.764.177.735.666.269.82
Co11.020.16.1420.13.736.7510.5
Ni17.627.93.6310.81.553.0917.2
Rb40.260.338.613714468.084.7
Sr499603256360146356784
Y5.889.8523.239.745.925.040.5
Zr68.698.8614409417283300
Nb3.825.2211.818.125.116.316.2
Ba780125417272245121412681211
La9.4813.016599.110369.063.9
Ce17.727.0290186200131121
Pr2.013.2829.820.822.614.213.6
Nd7.7912.894.771.576.550.549.5
Sm1.352.4311.311.512.78.328.58
Eu0.680.861.652.061.661.641.57
Gd1.152.107.068.939.926.507.24
Tb0.190.330.941.321.480.941.19
Dy1.041.744.577.318.605.017.17
Ho0.210.350.921.421.700.941.49
Er0.591.022.394.284.952.324.41
Tm0.0790.140.310.580.660.300.59
Yb0.590.962.073.924.371.834.00
Lu0.0900.150.310.570.640.270.59
Hf1.722.4915.710.511.17.457.59
Ta0.210.300.340.831.010.760.74
Pb10.916.415.474.621.018.321.5
Th0.510.6630.817.335.618.18.93
U0.400.311.332.863.972.011.71
), ArticleFig(id=1307087677619196509, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=表1, caption=

熊耳山TTG片麻岩主量(%)和微量元素(10−6)分析结果统计表

, figureFileSmall=null, figureFileBig=null, tableContent=
样品编号20TH-0120TH-0220TH-0420TH-0520TH-0620TH-0720TH-08
SiO266.1961.7970.7863.9670.4668.9159.35
TiO20.390.500.550.440.420.430.59
Al2O315.9316.1813.3812.4113.2514.1017.93
Fe2O33.665.183.526.674.123.995.60
MnO0.050.070.060.140.040.050.11
MgO1.732.560.961.260.950.992.18
CaO4.484.532.832.871.403.165.53
Na2O3.993.894.072.092.523.684.25
K2O1.422.102.075.575.412.632.25
P2O50.090.080.140.110.090.100.15
LOI1.352.451.243.760.901.301.83
Total99.2899.3399.5899.2899.5699.3399.76
Li5.658.764.177.735.666.269.82
Co11.020.16.1420.13.736.7510.5
Ni17.627.93.6310.81.553.0917.2
Rb40.260.338.613714468.084.7
Sr499603256360146356784
Y5.889.8523.239.745.925.040.5
Zr68.698.8614409417283300
Nb3.825.2211.818.125.116.316.2
Ba780125417272245121412681211
La9.4813.016599.110369.063.9
Ce17.727.0290186200131121
Pr2.013.2829.820.822.614.213.6
Nd7.7912.894.771.576.550.549.5
Sm1.352.4311.311.512.78.328.58
Eu0.680.861.652.061.661.641.57
Gd1.152.107.068.939.926.507.24
Tb0.190.330.941.321.480.941.19
Dy1.041.744.577.318.605.017.17
Ho0.210.350.921.421.700.941.49
Er0.591.022.394.284.952.324.41
Tm0.0790.140.310.580.660.300.59
Yb0.590.962.073.924.371.834.00
Lu0.0900.150.310.570.640.270.59
Hf1.722.4915.710.511.17.457.59
Ta0.210.300.340.831.010.760.74
Pb10.916.415.474.621.018.321.5
Th0.510.6630.817.335.618.18.93
U0.400.311.332.863.972.011.71
), ArticleFig(id=1307087677707276894, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=EN, label=Tab.2, caption=

U-Pb dating results of the Taihua Group TTG gneisses in the Xiong'ershan area

, figureFileSmall=null, figureFileBig=null, tableContent=
样品
编号
PbThUTh/U207Pb/206Pb207Pb/206Pb207Pb/235U207Pb/235U206Pb/238U206Pb/238U207Pb/206Pb207Pb/206Pb207Pb/235U207Pb/235U206Pb/238U206Pb/238U208Pb/232Th208Pb/232Th
总232238普通Pb比值1σ比值1σ比值1σrho年龄(Ma)1σ年龄(Ma)1σ年龄(Ma)1σ年龄(Ma)1σ
20TH-04-01728.046014320.320.14290.00268.34340.19070.42030.00620.6419226531.33226920.79226228.02218945.79
20TH-04-02252.145.86330.070.11870.00205.85240.10960.35530.00340.5108193930.71195416.30196016.20204944.12
20TH-04-03248.82444560.540.14880.00238.77430.14180.42540.00300.4371233226.85231514.81228513.65227132.08
20TH-04-04221.12833830.740.15060.00248.87880.14250.42560.00300.4386235427.16232614.73228613.61227531.25
20TH-04-05296.644.87560.060.12290.00215.81830.10850.34120.00280.4411199829.78194916.21189213.53216747.72
20TH-04-06686.072812840.570.14860.00278.57490.16830.41610.00410.5067233131.17229417.92224318.88206453.45
20TH-04-07108.01281980.650.14980.00258.55960.14120.41280.00290.4289234328.86229215.08222813.38224632.31
20TH-04-08198.01473570.410.14890.00289.28260.17180.44890.00360.4283234431.80236617.04239115.88238342.14
20TH-04-09230.81814260.420.14930.00269.08710.15760.43850.00340.4480233929.48234715.94234415.32232037.50
20TH-04-10214.51983890.510.14730.00258.95720.15290.43820.00320.4224231527.94233415.67234314.22234135.30
20TH-04-11189.839.44770.080.11980.00215.85050.10270.35270.00260.4199195430.87195415.29194712.44224961.34
20TH-04-12113.523.22730.090.11920.00226.06720.14570.36590.00460.5204194627.62198620.97201021.60199138.27
20TH-04-13108.11001940.520.14620.00288.95930.17730.44250.00380.4288230237.81233418.15236216.83240643.90
20TH-04-14158.91342930.460.14300.00258.68300.15280.43830.00350.4503226529.63230516.10234315.612076150.7
20TH-04-15246.71854670.400.14540.00238.58530.13900.42630.00290.4230229227.93229514.81228913.261927221.2
20TH-06-01246.02044640.440.14330.00258.57080.15060.43140.00310.4055233330.71229316.06231213.901609360.4
20TH-06-0292.766.81720.390.14530.00308.76820.17700.43580.00340.3888229135.19231418.46233215.411709500.7
20TH-06-03170.41653130.530.14430.00318.72150.18480.43580.00370.3982228036.73230919.37233216.561324503.0
20TH-06-04154.51652710.610.14500.00278.97370.16950.44640.00390.4671228832.41233517.33237917.601554429.6
20TH-06-05355.23496330.550.14590.00259.05030.15750.44700.00360.4571229829.32234315.99238215.891727346.7
20TH-06-06153.31142840.400.14620.00258.87830.15010.43750.00310.4208230229.64232615.51234014.021855257.0
20TH-06-07244.01654560.360.14560.00268.96200.16020.44310.00350.4476229530.56233416.41236515.892039176.1
20TH-06-08147.41262660.470.14790.00309.13400.18610.44480.00400.4389232239.82235218.71237217.79219997.17
20TH-06-09176.21623120.520.14920.00259.30740.15890.45000.00360.4669233728.24236915.74239516.00238136.43
20TH-06-10143.41232550.480.14780.00279.24890.16650.45150.00320.3963232125.78236316.57240214.36237037.06
20TH-06-11457.51928880.220.14680.00289.22540.17960.45360.00400.4583230933.49236117.90241117.99258153.07
20TH-06-12149.31302680.480.15050.00329.32820.20240.44730.00380.3961235236.73237119.97238317.18242441.75
20TH-06-13106.086.11970.440.15010.00349.19240.21360.44190.00390.3768234738.89235721.34235917.34261156.13
20TH-06-14203.01553750.410.14880.00319.14340.19070.44360.00360.3876233236.27235219.15236716.06239740.70
20TH-06-15141.01422520.560.15270.00309.30200.18770.43960.00340.3778237633.49236818.57234915.06250346.96
20TH-06-16202.01393820.360.14790.00279.02320.16740.44040.00340.4184232231.18234017.03235215.35230236.66
20TH-06-17206.51713930.430.14960.00268.85040.15640.42700.00320.4203234325.00232316.20229214.38230234.40
20TH-06-18230.81194870.240.13980.00268.40840.19420.43200.00520.5218222532.57227621.02231523.48223134.71
20TH-06-19109.41122010.560.14780.00268.81610.15380.43050.00280.3707232129.63231915.99230812.61228236.28
), ArticleFig(id=1307087677807940191, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=表2, caption=

熊耳山地区太华群TTG片麻岩U-Pb测年结果

, figureFileSmall=null, figureFileBig=null, tableContent=
样品
编号
PbThUTh/U207Pb/206Pb207Pb/206Pb207Pb/235U207Pb/235U206Pb/238U206Pb/238U207Pb/206Pb207Pb/206Pb207Pb/235U207Pb/235U206Pb/238U206Pb/238U208Pb/232Th208Pb/232Th
总232238普通Pb比值1σ比值1σ比值1σrho年龄(Ma)1σ年龄(Ma)1σ年龄(Ma)1σ年龄(Ma)1σ
20TH-04-01728.046014320.320.14290.00268.34340.19070.42030.00620.6419226531.33226920.79226228.02218945.79
20TH-04-02252.145.86330.070.11870.00205.85240.10960.35530.00340.5108193930.71195416.30196016.20204944.12
20TH-04-03248.82444560.540.14880.00238.77430.14180.42540.00300.4371233226.85231514.81228513.65227132.08
20TH-04-04221.12833830.740.15060.00248.87880.14250.42560.00300.4386235427.16232614.73228613.61227531.25
20TH-04-05296.644.87560.060.12290.00215.81830.10850.34120.00280.4411199829.78194916.21189213.53216747.72
20TH-04-06686.072812840.570.14860.00278.57490.16830.41610.00410.5067233131.17229417.92224318.88206453.45
20TH-04-07108.01281980.650.14980.00258.55960.14120.41280.00290.4289234328.86229215.08222813.38224632.31
20TH-04-08198.01473570.410.14890.00289.28260.17180.44890.00360.4283234431.80236617.04239115.88238342.14
20TH-04-09230.81814260.420.14930.00269.08710.15760.43850.00340.4480233929.48234715.94234415.32232037.50
20TH-04-10214.51983890.510.14730.00258.95720.15290.43820.00320.4224231527.94233415.67234314.22234135.30
20TH-04-11189.839.44770.080.11980.00215.85050.10270.35270.00260.4199195430.87195415.29194712.44224961.34
20TH-04-12113.523.22730.090.11920.00226.06720.14570.36590.00460.5204194627.62198620.97201021.60199138.27
20TH-04-13108.11001940.520.14620.00288.95930.17730.44250.00380.4288230237.81233418.15236216.83240643.90
20TH-04-14158.91342930.460.14300.00258.68300.15280.43830.00350.4503226529.63230516.10234315.612076150.7
20TH-04-15246.71854670.400.14540.00238.58530.13900.42630.00290.4230229227.93229514.81228913.261927221.2
20TH-06-01246.02044640.440.14330.00258.57080.15060.43140.00310.4055233330.71229316.06231213.901609360.4
20TH-06-0292.766.81720.390.14530.00308.76820.17700.43580.00340.3888229135.19231418.46233215.411709500.7
20TH-06-03170.41653130.530.14430.00318.72150.18480.43580.00370.3982228036.73230919.37233216.561324503.0
20TH-06-04154.51652710.610.14500.00278.97370.16950.44640.00390.4671228832.41233517.33237917.601554429.6
20TH-06-05355.23496330.550.14590.00259.05030.15750.44700.00360.4571229829.32234315.99238215.891727346.7
20TH-06-06153.31142840.400.14620.00258.87830.15010.43750.00310.4208230229.64232615.51234014.021855257.0
20TH-06-07244.01654560.360.14560.00268.96200.16020.44310.00350.4476229530.56233416.41236515.892039176.1
20TH-06-08147.41262660.470.14790.00309.13400.18610.44480.00400.4389232239.82235218.71237217.79219997.17
20TH-06-09176.21623120.520.14920.00259.30740.15890.45000.00360.4669233728.24236915.74239516.00238136.43
20TH-06-10143.41232550.480.14780.00279.24890.16650.45150.00320.3963232125.78236316.57240214.36237037.06
20TH-06-11457.51928880.220.14680.00289.22540.17960.45360.00400.4583230933.49236117.90241117.99258153.07
20TH-06-12149.31302680.480.15050.00329.32820.20240.44730.00380.3961235236.73237119.97238317.18242441.75
20TH-06-13106.086.11970.440.15010.00349.19240.21360.44190.00390.3768234738.89235721.34235917.34261156.13
20TH-06-14203.01553750.410.14880.00319.14340.19070.44360.00360.3876233236.27235219.15236716.06239740.70
20TH-06-15141.01422520.560.15270.00309.30200.18770.43960.00340.3778237633.49236818.57234915.06250346.96
20TH-06-16202.01393820.360.14790.00279.02320.16740.44040.00340.4184232231.18234017.03235215.35230236.66
20TH-06-17206.51713930.430.14960.00268.85040.15640.42700.00320.4203234325.00232316.20229214.38230234.40
20TH-06-18230.81194870.240.13980.00268.40840.19420.43200.00520.5218222532.57227621.02231523.48223134.71
20TH-06-19109.41122010.560.14780.00268.81610.15380.43050.00280.3707232129.63231915.99230812.61228236.28
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Zircon Hf isotope analysis results of TTG gneisses from the Taihua Group in the Xiong'ershan

, figureFileSmall=null, figureFileBig=null, tableContent=
样品号176Hf/177Hf1σ176Lu/177Hf1σ176Yb/177Hf1σεHf(0)εHf(t)TDM1TDM2fLu/Hf
20TH-04-030.2813020.0000130.0009560.0000220.0333400.000802−52.0−1.127162934−0.99960
20TH-04-040.2813120.0000140.0011680.0000340.0400880.001159−51.6−1.127182934−0.99956
20TH-04-060.2812830.0000120.0004710.0000140.0156430.000469−52.7−1.027082929−0.99964
20TH-04-080.2812820.0000140.0005590.0000060.0190870.000206−52.7−1.227162940−0.99957
20TH-04-090.2813120.0000140.0009360.0000130.0326110.000537−51.6−0.727012911−0.99957
20TH-04-100.2813320.0000140.0008220.0000090.0266490.000317−50.90.226672857−0.99957
20TH-04-130.2812980.0000160.0007710.0000110.0253890.000404−52.1−0.927082924−0.99953
20TH-04-140.2813100.0000130.0002190.0000110.0069570.000278−51.70.426542845−0.99959
20TH-06-030.2813090.0000130.0008590.0000160.0273660.000604−51.7−1.627002910−0.99960
20TH-06-070.2812890.0000140.0006820.0000020.0216770.000072−52.4−2.027142935−0.99959
20TH-06-110.2812880.0000130.0006920.0000030.0226180.000137−52.5−2.127172940−0.99960
20TH-06-120.2812970.0000160.0014640.0000480.0457050.001526−52.2−3.027602994−0.99953
20TH-06-130.2812830.0000130.0007340.0000040.0234940.000136−52.7−2.327272955−0.99961
20TH-06-140.2812890.0000130.0008330.0000020.0264360.000112−52.5−2.327262952−0.99959
20TH-06-150.2812880.0000150.0006920.0000120.0212510.000394−52.5−2.127172940−0.99956
20TH-06-160.2812800.0000140.0008220.0000010.0255960.000089−52.8−2.627372970−0.99957
), ArticleFig(id=1307087677979906657, tenantId=1146029695717560320, journalId=1306274195778404443, articleId=1307087668471419404, language=CN, label=表3, caption=

熊耳山太华群 TTG 片麻岩的锆石 Hf 同位素分析结果

, figureFileSmall=null, figureFileBig=null, tableContent=
样品号176Hf/177Hf1σ176Lu/177Hf1σ176Yb/177Hf1σεHf(0)εHf(t)TDM1TDM2fLu/Hf
20TH-04-030.2813020.0000130.0009560.0000220.0333400.000802−52.0−1.127162934−0.99960
20TH-04-040.2813120.0000140.0011680.0000340.0400880.001159−51.6−1.127182934−0.99956
20TH-04-060.2812830.0000120.0004710.0000140.0156430.000469−52.7−1.027082929−0.99964
20TH-04-080.2812820.0000140.0005590.0000060.0190870.000206−52.7−1.227162940−0.99957
20TH-04-090.2813120.0000140.0009360.0000130.0326110.000537−51.6−0.727012911−0.99957
20TH-04-100.2813320.0000140.0008220.0000090.0266490.000317−50.90.226672857−0.99957
20TH-04-130.2812980.0000160.0007710.0000110.0253890.000404−52.1−0.927082924−0.99953
20TH-04-140.2813100.0000130.0002190.0000110.0069570.000278−51.70.426542845−0.99959
20TH-06-030.2813090.0000130.0008590.0000160.0273660.000604−51.7−1.627002910−0.99960
20TH-06-070.2812890.0000140.0006820.0000020.0216770.000072−52.4−2.027142935−0.99959
20TH-06-110.2812880.0000130.0006920.0000030.0226180.000137−52.5−2.127172940−0.99960
20TH-06-120.2812970.0000160.0014640.0000480.0457050.001526−52.2−3.027602994−0.99953
20TH-06-130.2812830.0000130.0007340.0000040.0234940.000136−52.7−2.327272955−0.99961
20TH-06-140.2812890.0000130.0008330.0000020.0264360.000112−52.5−2.327262952−0.99959
20TH-06-150.2812880.0000150.0006920.0000120.0212510.000394−52.5−2.127172940−0.99956
20TH-06-160.2812800.0000140.0008220.0000010.0255960.000089−52.8−2.627372970−0.99957
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严文婷 1 , 唐利 1, * , 杨谦牧 2 , 王亮 3 , 陈龙龙 1
西北地质 | 非主题 2026,59(3): 314-327
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西北地质 |非主题 2026 , 59 (3) : 314 -327
华北克拉通南缘熊耳山地区太华群TTG片麻岩成因及地质意义
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严文婷1 , 唐利1, * , 杨谦牧2, 王亮3, 陈龙龙1
作者信息
  • 1中国地质大学(北京) 地球科学与资源学院,北京 100083
  • 2中国地质大学(北京)能源学院,北京 100083
  • 3中国地质调查局金矿勘查技术创新中心/中国地质调查局西安矿产资源调查中心,陕西 西安 710100
通讯作者:
唐利(1990−),男,副教授,博士生导师,主要从事钼–金–稀土等关键金属矿床成因和成矿规律的研究和教学工作。E−mail:。
作者简介:

严文婷(2004−),女,本科生,资源勘查工程(固体矿产)专业。E−mail:

Petrogenesis and Geological Significance of the Taihua Group TTG Gneisses in the Xiong'ershan Area, Southern Margin of the North China Craton
Wenting YAN1 , Li TANG1, * , Qianmu YANG2, Liang WANG3, Longlong CHEN1
Affiliations
  • 1School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
  • 2School of Energy Institute, China University of Geosciences (Beijing), Beijing 100083, China
  • 3Technology Innovation Center for Gold Ore Exploration, Xi’an Mineral Resources Survey of China Geological Survey, Xi’an 710100, Shaanxi, China
出版时间: 2026-06-20 doi: 10.12401/j.nwg.2025164
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华北克拉通经历太古宙—古元古代漫长且复杂的地质演化历史,形成该稳定克拉通的岩浆作用和变质作用过程一直是学者们关注的焦点。笔者以华北克拉通南缘熊耳山地区太华群TTG(英云闪长岩–奥长花岗岩–花岗闪长岩)片麻岩为研究对象,基于详细的野外地质调查、室内镜下研究、岩石地球化学、锆石U-Pb定年和Hf同位素分析,揭示区内古元古代岩浆作用机制及其构造指示意义。熊耳山地区太华群TTG片麻岩的岩浆结晶年龄为2300 Ma,而变质年龄为1984~1940 Ma。太华群TTG片麻岩SiO2含量为59.35%~70.78%,Al2O3含量为12.41%~17.93%,CaO含量为1.40%~5.52%,MgO含量为0.95%~2.56%,富集轻稀土元素亏损重稀土元素,并表现出轻、重稀土元素强烈分异的特点,成分上类似于高铝型TTG 片麻岩。样品富集Rb、Ba、Sr等大离子亲石元素,亏损Nb、Ta、Ti等高场强元素,与岛弧花岗岩的特征相似。此外,岩浆锆石具有相对较高的 (176Hf/177Hf)i值(0.281282~0.281332),εHf(t)值(−2.98~0.20)和二阶段模式年龄(2844~2994 Ma),指示其岩浆源区为中太古代古老地壳的熔融。综合研究认为,熊耳山地区的TTG片麻岩形成于华北克拉通东、西部陆块之间的古元古代俯冲过程,其1984~1940 Ma的变质年龄记录沿中部造山带的碰撞拼合过程,进一步约束了东、西部陆块的碰撞时限。

熊耳山地区  /  TTG片麻岩  /  太华群  /  岩石成因  /  华北克拉通

The North China Craton underwent a prolonged and complex geological evolution during the Archean to Paleoproterozoic, with the magmatic and metamorphic processes remain as the research questions. This study focuses on the TTG (tonalite-trondhjemite-granodiorite) gneisses of the Taihua Group in the Xiong’ershan area along the southern margin of the North China Craton. The integrated field investigations, petrographic analysis under the microscope, geochemistry, zircon U-Pb dating and Hf isotopic studies are conducted to elucidate the Paleoproterozoic magmatic mechanisms and the tectonic evolution of this region. Zircon U-Pb dating constrains the magmatic crystallization age of the Taihua Group TTG gneisses in the Xiong’ershan area to approximately 2300 Ma, while the metamorphic ages range from 1984 Ma to 1940 Ma. The Taihua Group TTG gneisses exhibit a wide compositional range, with SiO2 (59.35%~70.78%), Al2O3 (12.41%~17.93%), and relatively high CaO (1.40%~5.52%) and MgO (0.95%~2.56%) contents. It is enriched in light rare earth elements (LREE) and depleted in heavy rare earth elements (HREE), displaying strong fractionation between LREE and HREE. In composition, it resembles high-Al TTG gneisses. The samples are enriched in large-ion lithophile elements (LILEs) such as Rb, Ba, and Sr, but depleted in high-field-strength elements (HFSEs) like Nb, Ta, and Ti, which are similar to the features of island arc granites. Additionally, magmatic zircons display relatively high (176Hf/177Hf)ᵢ ratios (0.281282~0.281332), εHf(t) values (−2.98 ~ +0.20), and two-stage model ages (2844~2994 Ma), indicating that the magmatic source originated from the partial melting of Mesoarchean ancient crust. These findings suggest that the TTG gneisses in the Xiong’ershan area formed during the Paleoproterozoic subduction process between the eastern and western blocks of the North China Craton. The metamorphic age of 1984~1940 Ma records the collisional process along the Trans-North China Orogeny. This further constrains the timing of collision between the eastern and western continental blocks.

Xiong'ershan area  /  TTG gneiss  /  Taihua Group  /  petrogenesis  /  North China Craton
严文婷, 唐利, 杨谦牧, 王亮, 陈龙龙. 华北克拉通南缘熊耳山地区太华群TTG片麻岩成因及地质意义. 西北地质, 2026 , 59 (3) : 314 -327 . DOI: 10.12401/j.nwg.2025164
Wenting YAN, Li TANG, Qianmu YANG, Liang WANG, Longlong CHEN. Petrogenesis and Geological Significance of the Taihua Group TTG Gneisses in the Xiong'ershan Area, Southern Margin of the North China Craton[J]. Northwestern Geology, 2026 , 59 (3) : 314 -327 . DOI: 10.12401/j.nwg.2025164
华北克拉通在古太古代就已经开始形成陆核(3.8 Ga),是中国最古老的地块(万渝生等, 2021; Liu et al., 2024),其经历了多期构造–岩浆–变质作用以及不同程度的混合岩化和深熔作用(翟明国, 2019; 万渝生等, 2022),具有漫长而复杂的演化历史(Zhai et al., 2011; Zeng et al., 2025)。目前,大部分研究将华北克拉通划分为东部陆块、西部陆块和中部造山带(图1a; Zhao et al., 2005, 2012, 2013),其中的中部造山带作为重要的前寒武纪碰撞造山带,是探讨华北克拉通早期寒武纪地质演化的一个关键区域(Zhao et al., 2008;Tang et al., 2023; 王晓青等, 2024)。前人关于该造山带新太古代至古元古代的构造演化历史还存在不同认识。一种观点认为,中部造山带自~2.55 Ga之后是一个漫长的安第斯型大陆弧或日本型岛弧(Zhao et al., 2012),东、西部陆块间的古大洋向东部陆块俯冲,形成了大陆边缘岩浆弧和弧后盆地,最终在古元古代(1.95~1.85 Ga)发生碰撞拼合形成中部造山带。另一种观点认为,华北克拉通由多个不同微陆块在新太古代末期聚合形成统一基底后,其中部地区在2.35~1.85 Ga先后经历了裂解、俯冲、增生和碰撞过程,最终形成中部造山带(Zhai et al., 2011; 翟明国, 2012; Tang et al., 2018)。
太华群是华北克拉通中部造山带南缘的典型早前寒武纪变质杂岩,总体呈NW–SE向展布,自西向东从陇山、骊山,经小秦岭地区华山、灵宝、崤山,到洛宁县熊耳山地区、鲁山县背孜–马楼地区和叶县辛店–舞阳县铁山庙地区(第五春荣等, 2010; 刘佛刚等, 2024)。太华群自下而上可划分为耐庄组、荡泽河组、铁山岭组、水底沟组和雪花沟组,其中前人又将耐庄组和荡泽河组划归为下太华群,后三组划归为上太华群(时毓等, 2014)。下太华群形成于新太古代早期(2.7~2.9 Ga),主要分布于鲁山地区,少量分布于熊耳山和小秦岭等地区;上太华群形成于新太古代晚期—古元古代早期,主要分布于熊耳山和小秦岭地区(时毓等, 2014; 刘金波等, 2024)。目前,前人研究认为鲁山地区下太华群的岩浆活动记录了华北克拉通南缘在新太古代早期新生地壳生长过程(韩长寿等, 2023; 张燕赞等, 2025)。相比而言,熊耳山地区古元古代岩浆作用形成的太华群TTG片麻岩研究较薄弱。
笔者以熊耳山太华群 TTG 片麻岩为研究对象,通过系统的岩石地球化学、锆石U-Pb年代学及Hf同位素研究,揭示熊耳山太华群 TTG 片麻岩的岩石成因、岩浆源区和构造背景,并为华北克拉通中部带的构造演化过程提供依据。
华北克拉通经历了两期克拉通化(Zhai et al., 2011; Tang et al., 2018)。第一期克拉通化及微陆块拼合发生在新太古代末期(~2.5 Ga),此时华北克拉通沿绿岩带被分为阴山陆块、鄂尔多斯陆块、龙岗陆块和狼林陆块(Zhao et al., 2012; Zeng et al., 2025)。龙岗陆块和狼林陆块在太古宙末期发生碰撞拼合形成完整的东部陆块,其间的胶吉辽造山带则形成于东部陆块古元古代(~2.1 Ga)的裂解–拼合作用。鄂尔多斯陆块在古元古代期间处于一个稳定被动型大陆边缘环境,阴山陆块南缘则处于活动型大陆边缘环境,二者在2.0~1.9 Ga发生碰撞拼合,形成统一的西部陆块及其内部的孔兹岩带(李三忠等, 2015)。第二期克拉通化发生在1.95~1.82 Ga期间,经历西部陆块和东部陆块的碰撞造山过程并最终形成统一的华北克拉通(Zhao et al., 2012; Tang et al., 2023)。
华北克拉通南缘新太古代—古元古代变质结晶基底之上不整合覆盖着巨厚的中—新元古代陆源碎屑岩–碳酸盐岩沉积盖层,具有典型的基底和沉积盖层的二元结构特征(刘富乐等, 2025; 孟轲荆等, 2025)。基底主要包括太华群,记录了华北克拉通南缘构造演化过程的岩浆作用和变质作用。下太华群的形成年龄记录了两期明显的地壳生长时间,一期以鲁山地区2.85~2.70 Ga TTG片麻岩和斜长角闪岩为代表(韩长寿等, 2023; 张燕赞等, 2025),一期以小秦岭~2.50 Ga各类花岗质岩石为代表(第五春荣等, 2018)。上太华群的主要岩性为TTG片麻岩、闪长质片麻岩、斜长角闪岩以及花岗岩,记录了华北克拉通南缘古元古代早期的岩浆活动,可能与西部地块和东部地块汇聚造山或与南部太古宙陆块和其他陆块汇聚-碰撞相关(第五春荣等, 2018)。此外,小秦岭熊耳山地区和鲁山地区的太华群均记录了~1.90 Ga的变质事件,暗示了华北克拉通中部带在该时期处于碰撞造山阶段,并于~1.85 Ga完成碰撞拼合(第五春荣等, 2018; 朱建江等, 2024)。熊耳群火山岩形成于古元古代(1.80~1.75 Ga),不整合覆盖于太华群之上,记录了华北克拉通基底结晶之后最大规模的火山活动,为一套中基性–中酸性火山岩,岩性主要为紫红色–灰黑色玄武安山岩、安山(玢)岩、英安岩、流纹(斑)岩(王俊等, 2025)。熊耳群火山–沉积岩形成于中元古代,此时华北克拉通南缘进入了稳定的盖层发育阶段(胡国辉等, 2013)。
本次研究的8件太华群TTG片麻岩样品采自华北克拉通南缘熊耳山地区(图1b),样品整体呈灰白色,中细粒结构,片麻状构造(图2a~图2c)。太华群TTG片麻岩样品的主要矿物组合为斜长石(50%~60%)、石英(20%~30%)和少量角闪石(图2d~图2f)。其中,斜长石、石英等粒状矿物与云母等片状矿物相间排列形成片麻状构造,副矿物有锆石、磷灰石等。全岩主量元素、微量元素、锆石LA-ICP-MS U-Pb定年以及Hf同位素分析均由武汉上谱分析科技有限责任公司完成。
全岩主微量元素测试仪器为波长色散X射线荧光光谱仪(ZSXPrimusⅡ),分析方法参照《硅酸盐岩石化学分析方法第28部分:16个主次成分量测定》(GB/T14506.28-2010)和《岩石矿物分析》,采用中国国家岩石标准(GBW07103、GBW07105、GBW07111)对测量样品的元素浓度进行校准,其检测结果与标准结果误差为1%~5%。样本的微量元素测定利用Agilent 7700e ICP-MS分析完成,用《硅酸盐岩石化学分析方法》中的测定方法作为评价标准,测定结果的精度为1%~5%。
锆石LA-ICP-MS U-Pb定年的GeolasPro激光剥蚀系统由COMPexPro 102 ArF 193 nm准分子激光器和MicroLas光学系统组成,ICP-MS型号为Agilent 7900,激光能量为80 mJ,频率为5 Hz,激光束斑直径为32 µm(Liu et al., 2008)。使用锆石91500和玻璃物质NIST610作为标准进行同位素和微量元素分馏校正。锆石Hf同位素分析利用LA-MC-ICP-MS完成,激光剥蚀系统为Geolas HD (Coherent,德国), MC-ICP-MS为Neptune Plus(Thermo Fisher Scientific,德国),用标样TEM(0.282683)进行外标校正,91500和GJ-1作为第二标样监控数据校正质量。
太华群TTG片麻岩样品的主微量元素分析结果(表1)显示,样品整体表现为富Na、高Al、贫K,富轻稀土、富Rb、Ba等大离子亲石元素,贫重稀土及Nb、Ta、Ti等高场强元素的特征。在 TAS 图中,大多数样品落在花岗闪长岩至闪长岩区域(图3、图4),显示钙碱性到高钾钙碱性系列的特征,与典型TTG组合的地球化学特征一致。
两件太华群TTG片麻岩样品(20TH-04、20TH-06)中的锆石粒径为100~150 µm,多呈自形–半自形的棱柱状(图5a)。阴极发光图像显示,大部分锆石颗粒具有振荡环带,具有岩浆成因特征(图5a)。部分锆石具有核–边结构,其中核部具有环带特征,边部在阴极发光图像中呈现亮白色且无环带结构,指示边部锆石为变质成因(图5a、图5b)。
样品20TH-04中11个点的206 Pb/238 U 和207 Pb/235 U年龄在误差范围内谐和度超过90%,加权平均207Pb/206Pb年龄为(2324±16)Ma(MSWD=1.4),Th/U值为0.32~0.74(表2),指示该年龄代表太华群TTG片麻岩样品的岩浆结晶年龄。此外,4个边部锆石的分析点具有更加年轻的207Pb/206Pb年龄,其加权平均年龄为(1962±22)Ma(MSWD=0.41),Th/U值为0.06~0.09,指示其代表TTG片麻岩的变质年龄(图5)。样品20TH-06的19个分析点具有较为一致的年龄,加权平均207Pb/206Pb年龄为(2307±34)Ma(MSWD=1.07),Th/U值为0.22~0.61,指示其代表岩浆结晶年龄。
样品20TH-04分析的8颗锆石均为岩浆锆石,具有相对较高的 (176Hf/177Hf)i值(0.281282~0.281332)及εHf(t)值(−1.2~0.4),其亏损地幔一阶段Hf模式年龄为2718~2654 Ma,二阶段模式年龄为2940~2845 Ma,总体变化范围均较小。样品20TH-06分析了8颗锆石的Lu-Hf同位素,均具有较高的 (176Hf/177Hf)i值(0.281280~0.281309)及全部为负的εHf(t)值(−3.0~−1.6),其二阶段模式年龄总体上略老(2994~2910 Ma)。
华北克拉通南缘熊耳山地区太华群TTG片麻岩中具有明显震荡环带的岩浆锆石和边部变质。锆石定年结果表明,区域花岗质岩浆作用的时限为2324~2307 Ma,其侵位后经历(1962±22)Ma变质作用事件。研究结果与华北克拉通中部带古元古代岩浆作用和变质作用年龄相一致(李三忠等, 2015; Tang et al., 2018; 卢成森等, 2025)。华北克拉通基底主要经历了~2.50 Ga和1.95~1.80 Ga的两次变质作用,~2.50 Ga的变质作用主要记录了沿绿岩带的微陆块碰撞拼合。此后,中部造山带经历古元古代裂解–俯冲–碰撞过程(Zeng et al., 2025),样品的岩浆结晶年龄记录了中部带的2324~2307 Ma岩浆事件。此外,文中的变质锆石边部的定年结果指示西部陆块和东部陆块的碰撞造山和变质作用发生于(1962±22)Ma,指示东、西部陆块开始碰撞的时限不晚于1.96 Ga。
样品具高SiO2(59.35%~70.78%)、Al2O3(12.41%~17.93%),高Na 贫 K(Na2O/K2O>1,Na2O=2.09%~4.25%,K2O=1.42%~5.57%)特征,稀土元素配分显示轻稀土元素富集((La/Yb)N =9.72%~57.20%)和重稀土元素亏损(Yb=0.852×10−6 ),并表现出轻、重稀土元素强烈分异的特点,具典型高铝TTG的特征。岛弧花岗岩在形成过程中,由于俯冲板片脱水作用而释放出富含大离子亲石元素和轻稀土元素的流体和熔体,高场强元素由于不易在岛弧岩浆中富集而呈现亏损的特点(王楠等, 2017; 王慧等, 2021)。样品的 Rb 元素含量较低(< 150×10−6),球粒陨石标准化图解显示出Ti、Nb、Ta负异常及Pb正异常(图4a),原始地幔标准化蛛网图显示样品富集大离子亲石元素(Rb、Ba、Th、U),亏损高场强元素(Nb、Ta、Ti),与俯冲板片含水熔体混入下地壳镁铁质岩石的特征一致(Kamber et al., 2000)。此外,Sr/Y-Y与(La/Yb)N-(Yb)N判别图显示样品主要落入岛弧岩浆岩及埃达克质TTG区域(图7);Nb-Y和Rb-(Y+Nb)图解显示样品落入后碰撞火山弧花岗岩区域(图8),指示熊耳山地区的古元古代太华群TTG片麻岩形成于华北克拉通中部带俯冲的构造背景。
大多数学者认为太古宙TTG质岩石是在下地壳贫 Mg、Cr、Ni 区域部分熔融形成,或由下地壳中富 Mg、Cr、Ni 的俯冲洋壳部分熔融形成(Nédélec et al., 2012)。Hf同位素可以为岩浆源区和壳幔相互作用提供关键证据,样品Hf模式年龄(2845~2994 Ma;表3)显著老于成岩年龄(2324±16 Ma),且εHf(t)多呈负值(−2.98~0.40),表明岩浆源区混入再循环古老地壳物质(图8,表3)。Nb/Ta值(17.48~34.37)也与受俯冲板片含水熔体影响的镁铁质岩石比值相似(Kamber et al., 2000;陈龙龙等,2024),反映研究区内TTG质岩石的岩浆源区很可能是来自俯冲洋壳部分熔融的产物(周艳艳等, 2009)。熊耳山太华群TTG片麻岩具有较高的La/Yb值(13.5~79.7;表1)。在(La/Yb)N-YbN和Sr/Y-Y图解中(图7),大部分样品落入典型的埃达克岩或高铝TTG的成分范围,小部分落入岛弧岩浆岩的成分范围中,指示其原岩可能为太古宙TTG片麻岩,其中还包含其他大陆地壳物质的参与。此外,(La/Yb)N-YbN和Sr/Y-Y图解(图7)表明,太华群母岩浆在熔融过程中存在金红石、石榴石或角闪石残留,导致Nb/Ta值与Zr/Sm值(分别为17.48×10−6~34.37×10−6、32.89×10−6~54.23×10−6)值变化较大,并具有低Y含量(5.88×10−6~45.90×10−6)与高Sr/Y值(3.17~84.87)。球粒陨石标准化稀土元素配分曲线显示出显著的Eu负异常(Eu/Eu*=0.30~0.45),指示太华群TTG片麻岩形成过程中伴随大量的斜长石结晶分异。
华北克拉通经历了多阶段构造演化过程。2.58~2.48 Ga,鄂尔多斯、迁怀与许昌等微陆块沿五台花岗岩–绿岩带及其赞皇分支发生碰撞拼合,与此同时其他主要微陆块也沿一系列~2.50 Ga的花岗岩–绿岩带汇聚,导致华北克拉通的初始克拉通化(Zhai et al., 2011; Tang et al., 2018)。2.50~2.45 Ga,发育以未变形基性岩墙群和花岗质岩墙为标志的后碰撞伸展作用,进而引发沿恒山及怀安–宣化杂岩带分布的洋盆扩张(葛松胜等, 2016)。~2.45~2.12 Ga,恒山、怀安–宣化及吕梁杂岩带普遍经历了俯冲作用,而阜平、五台与赞皇杂岩带则在同时期经历裂谷作用(Tang et al., 2018)。2.12~1.98 Ga,五台–阜平地区发生双向俯冲,导致在阜平、五台和吕梁杂岩带发生了广泛的弧岩浆活动,同一时期恒山和怀安–宣化–赞皇杂岩记录裂解过程。1.96~1.80 Ga,在东、西部陆块拼合作用的驱动下,先前分离的陆块最终发生聚合(Tang et al., 2018; Wang et al., 2024)。因此,华北克拉通中部带完整记录了一个始于新太古代克拉通化之后的威尔逊旋回,该旋回涉及新太古代克拉通化、古元古代多次裂谷、俯冲与碰撞过程,最终形成统一的华北克拉通并入Columbia超大陆(Tang et al., 2018)。
研究结果显示,华北克拉通南缘熊耳山地区的太华群TTG片麻岩的岩浆年龄为~2.30 Ga,形成于俯冲背景并具有岛弧特征,其Hf同位素数据显示岩浆源区混有古老地壳物质,记录了华北克拉通中部带南缘的太古宙陆块在~2.3 Ga与其他陆块俯冲碰撞过程并产生了广泛的弧岩浆作用。样品的变质年龄为~1.96 Ga,指示东、西部陆块碰撞拼合的时限不晚于1.96 Ga,东、西部陆块沿中部造山带主碰撞造山事件发生于1.96~1.90 Ga。
(1) 华北克拉通南缘熊耳山地区太华群TTG片麻岩的岩浆结晶年龄时限为2324~2307 Ma,变质年龄为(1962±22)Ma。
(2) 熊耳山地区太华群TTG片麻岩属高铝型TTG,具有俯冲背景下的岛弧岩浆岩特征,岩浆源区混入太古宙古老地壳物质并具有富钙贫铝的特征。
(3) 熊耳山地区太华群TTG片麻岩形成于古元古代东、西部陆块俯冲相关的弧岩浆作用,其变质年龄进一步约束东、西部陆块的碰撞时限应为1.96~1.90 Ga。

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2026年第59卷第3期
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doi: 10.12401/j.nwg.2025164
  • 接收时间:2025-12-05
  • 首发时间:2026-09-16
  • 出版时间:2026-06-20
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  • 收稿日期:2025-12-05
  • 修回日期:2026-01-23
  • 录用日期:2026-01-29
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    1中国地质大学(北京) 地球科学与资源学院,北京 100083
    2中国地质大学(北京)能源学院,北京 100083
    3中国地质调查局金矿勘查技术创新中心/中国地质调查局西安矿产资源调查中心,陕西 西安 710100

通讯作者:

唐利(1990−),男,副教授,博士生导师,主要从事钼–金–稀土等关键金属矿床成因和成矿规律的研究和教学工作。E−mail:。
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2种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
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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