«上一篇/Previous Article|本期目录/Table of Contents|下一篇/Next Article»

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第46卷

期数:

2024年第01期

页码:

114-126

栏目:

基础地质与矿床地质

出版日期:

2024-01-15

文章信息/Info

Title:

Review on Isotopic Dating Methods of Mantle Eclogite Xenoliths

文章编号:

1672-6561(2024)01-0114-13

作者:

蒋蕾茵¹; 孙 晶¹; 2*; 黄铖铮¹; 吴 琪³

(1. 中国石油大学(北京)地球科学学院,北京 102249; 2. 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249; 3. 自然资源部信息中心,北京 100812)

Author(s):

JIANG Lei-yin¹;  SUN Jing¹; 2*;  HUANG Cheng-zheng¹;  WU Qi³

(1. College of Geosciences, China University of Petroleum, Beijing 102249, China; 2. State Key Laboratory of Petroleum Resources and Engineering, China University of Petroleum, Beijing 102249, China; 3. Information Center of the Ministry of Natural Resources, Beijing 100812, China)

关键词:

板块构造;  地幔榴辉岩包体;  放射性同位素;  定年方法;  锆石U-Pb年龄;  Sm-Nd等时线年龄;  Lu-Hf等时线年龄;  硫化物Re-Os等时线年龄

Keywords:

plate tectonics;  mantel eclogite xenolith;  radioisotope;  dating method;  zircon U-Pb age;  Sm-Nd isochron age;  Lu-Hf isochron age;  sulfide Re-Os isochron age

分类号:

P597

DOI:

10.19814/j.jese.2023.09010

文献标志码:

A

摘要:

地幔榴辉岩包体是寄主岩浆从地球深部地幔携带到地表的俯冲洋壳碎片,作为一种高压变质岩,它可能记录着有关大洋地壳原岩、板块俯冲以及后期交代变质过程等重要信息,因此其年龄也显得格外重要。通过统计全球超过500个已发表的地幔榴辉岩包体的年龄结果,对比几种常用的地幔榴辉岩包体同位素定年方法,讨论了不同方法的优缺点及适用情况。结果表明:金红石U-Pb和全岩Rb-Sr、Sm-Nd、Lu-Hf全岩等时线法一般给出的是寄主岩浆的年龄或地幔交代的时间,而榴辉岩中的硫化物Re-Os等时线年龄,锆石U-Pb上交点年龄,Sm-Nd、Lu-Hf石榴子石-单斜辉石双矿物等时线年龄以及锆石Hf亏损地幔模式年龄对于其原岩年龄及板块俯冲时代有较为可观的应用前景; 地幔榴辉岩包体最古老年龄的峰值分布在3.1～2.8 Ga,与Kaapvaal和西伯利亚克拉通构造拼合的时间吻合,可能代表着全球地幔榴辉岩包体的最早形成时代,也预示着板块构造可能于中太古代开启。

Abstract:

Mantle eclogite xenoliths are subducted oceanic crust fragments carried by host magma from the deep mantle. As a high-pressure metamorphic rock, mantle eclogite xenoliths may record important information about ancient oceanic crust, plate subduction and later metasomatic metamorphism. Therefore, their ages are particularly important. More than 500 published age results of mantle eclogite xenoliths in the world were selected, and several commonly used isotopic dating methods of mantle eclogite xenoliths were compared, and the advantages and disadvantages of different methods and their applicability were discussed. The results show that the rutile U-Pb, and Rb-Sr, Sm-Nd and Lu-Hf whole-rock isochron methods generally date the age of host magma or the time of mantle metasomatism; the sulfide Re-Os isochron age, zircon U-Pb age and the garnet-clinopyroxene isochron ages of Sm-Nd and Lu-Hf, as well as zircon Hf depleted-mantle model age, have a considerable prospect for the ages of protoliths and tectonic subduction; moreover, the peak of the oldest ages for mantle eclogite xenoliths mostly ranges from 3.1 Ga to 2.8 Ga, which coincides with the age of tectonic amalgamation of Kaapvaal and Siberian cratons. Therefore, it may represent the earliest formation age of mantle eclogite xenoliths, and also indicate that plate tectonics may have started in Mesoarchean.

参考文献/References:

[1] BOIFACE N,SCHENK V,APPEL P.Paleoprotero-zoic Eclogites of MORB-type Chemistry and Three Proterozoic Orogenic Cycles in the Ubendian Belt(Tanzania):Evidence from Monazite and Zircon Geochronology,and Geochemistry[J].Precambrian Re-search,2012,192/193/194/195:16-33.
[2] FRANÇOIS C,DEBAILLE V,PAQUETTE J L,et al.The Earliest Evidence for Modern-style Plate Tecto-nics Recorded by HP-LT Metamorphism in the Paleoproterozoic of the Democratic Republic of the Congo[J].Scientific Reports,2018,8:15452.
[3] LOOSE D,SCHENK V.2.09 Ga Old Eclogites in the Eburnian-Transamazonian Orogen of Southern Cameroon:Significance for Palaeoproterozoic Plate Tecto-nics[J].Precambrian Research,2018,304:1-11.
[4] AULBACH S,SMART K A.Petrogenesis and Geodynamic Significance of Xenolithic Eclogites[J].Annual Review of Earth and Planetary Sciences,2023,51:521-549.
[5] MACGREGOR I D,MANTON W I.Roberts Victor Eclogites:Ancient Oceanic Crust[J].Journal of Geophysical Research:Solid Earth,1986,91(B14):14063-14079.
[6] HATTON C J,GURNEY J J.Roberts Victor Eclogites and Their Relation to the Mantle[M]∥NIXON P H.Mantle Xenoliths.New York:John Wiley & Sons,1987:453-463.
[7] MENZIES A H,CARLSON R W,SHIREY S B,et al.Re-Os Systematics of Diamond-bearing Eclogites from the Newlands Kimberlite[J].Lithos,2003,71(2/3/4):323-336.
[8] JACOB D E,BIZIMIS M,SALTERS V J M.Lu-Hf and Geochemical Systematics of Recycled Ancient Oceanic Crust:Evidence from Roberts Victor Eclogites[J].Contributions to Mineralogy and Petrology,2005,148(6):707-720.
[9] HILLS D V,HAGGERTY S E.Petrochemistry of Eclogites from the Koidu Kimberlite Complex,Sierra Le-one[J].Contributions to Mineralogy and Petrology,1989,103(4):397-422.
[10] BARTH M G,RUDNICK R L,HORN I,et al.Geochemistry of Xenolithic Eclogites from West Africa,Part I:A Link Between Low MgO Eclogites and Archean Crust Formation[J].Geochimica et Cosmochi-mica Acta,2001,65(9):1499-1527.
[11] BARTH M G,RUDNICK R L,HORN I,et al.Geochemistry of Xenolithic Eclogites from West Africa,Part 2:Origins of the High MgO Eclogites[J].Geo-chimica et Cosmochimica Acta,2002,66(24):4325-4345.
[12] HEAMAN L M,CREASER R A,COOKENBOO H O,et al.Multi-stage Modification of the Northern Slave Mantle Lithosphere:Evidence from Zircon- and Diamond-bearing Eclogite Xenoliths Entrained in Jericho Kimberlite,Canada[J].Journal of Petrology,2006,47(4):821-858.
[13] AULBACH S,PEARSON N J,O'REILLY S Y,et al.Origins of Xenolithic Eclogites and Pyroxenites from the Central Slave Craton,Canada[J].Journal of Petro-logy,2007,48(10):1843-1873.
[14] JERDE E A,TAYLOR L A,CROZAZ G,et al.Diamondiferous Eclogites from Yakutia,Siberia:Evidence for a Diversity of Protoliths[J].Contributions to Mi-neralogy and Petrology,1993,114(2):189-202.
[15] JACOB D E,JAGOUTZ E,LOWRY D,et al.Diamondiferous Eclogites from Siberia:Remnants of Archean Oceanic Crust[J].Geochimica et Cosmochimica Acta,1994,58(23):5191-5207.
[16] PEARSON D G,SNYDER G A,SHIREY S B,et al.Re-Os,Sm-Nd,and Rb-Sr Isotope Evidence for Thick Archaean Lithospheric Mantle Beneath the Siberian Craton Modified by Multistage Metasomatism[J].Geochimica et Cosmochimica Acta,1995,59(5):959-977.
[17] SNYDER G A,TAYLOR L A,CROZAZ G,et al.The Origins of Yakutian Eclogite Xenoliths[J].Journal of Petrology,1997,38(1):85-113.
[18] JACOB D E,FOLEY S F.Evidence for Archean Ocean Crust with Low High Field Strength Element Signature from Diamondiferous Eclogite Xenoliths[J].Li-thos,1999,48(1/2/3/4):317-336.
[19] GAO X Y,ZHENG Y F,CHEN Y X.U-Pb Ages and Trace Elements in Metamorphic Zircon and Titanite from UHP Eclogite in the Dabie Orogen:Constraints on P-T-t Path[J].Journal of Metamorphic Geology,2011,29(7):721-740.
[20] ZHANG L F,WANG Y,ZHANG L J,et al.Ultrahigh Pressure Metamorphism and Tectonic Evolution of Southwestern Tianshan Orogenic Belt,China:A Comprehensive Review[J].Geological Society,London,Special Publications,2019,474:133-152.
[21] 张泽明,丁慧霞,董 昕,等.喜马拉雅造山带两种不同类型榴辉岩与印度大陆差异性俯冲[J].地球科学,2019,44(5):1602-1619.
ZHANG Ze-ming,DING Hui-xia,DONG Xin,et al.Two Contrasting Eclogite Types in the Himalayan Orogen and Differential Subduction of Indian Continent[J].Earth Science,2019,44(5):1602-1619.
[22] 龚庭楠,杜瑾雪,张立飞,等.新疆西南天山榴辉岩高压—超高压峰期变质作用时代:Lu-Hf同位素年代学证据[J].岩石学报,2023,39(3):689-700.
GONG Ting-nan,DU Jin-xue,ZHANG Li-fei,et al.Ages of Peak HP-UHP Metamorphism of Eclogites from Chinese Southwestern Tianshan:Evidence from Lu-Hf Geochronology[J].Acta Petrologica Sinica,2023,39(3):689-700.
[23] 刘晓春,胡 娟,陈龙耀,等.海南洋壳型高温榴辉岩:基本特征及待解问题[J].岩石学报,2021,37(1):143-161.
LIU Xiao-chun,HU Juan,CHEN Long-yao,et al.Oceanic-type High-temperature Eclogites from Hai-nan Island,South China:General Characteristics and Unsolved Problems[J].Acta Petrologica Sinica,2021,37(1):143-161.
[24] HELMSTAEDT H,SCHULZE D J.Southern African Kimberlites and Their Mantle Sample:Implications for Archean Tectonics and Lithospheric Evolution[M]∥ROSS J.Kimberlites and Related Rocks Vo-lume 1:Their Composition,Occurrence,Origin and Emplacement.New York:Blackwell,1989:358-368.
[25] JACOB D E.Nature and Origin of Eclogite Xenoliths from Kimberlites[J].Lithos,2004,77(1/2/3/4):295-316.
[26] GRÉAU Y,HUANG J X,GRIFFIN W L,et al.Type I Eclogites from Roberts Victor Kimberlites:Products of Extensive Mantle Metasomatism[J].Geochimica et Cosmochimica Acta,2011,75(22):6927-6954.
[27] HUANG J X,GRÉAU Y,GRIFN W L,et al.Multi-stage Origin of Roberts Victor Eclogites:Progressive Metasomatism and Its Isotopic Effects[J].Lithos,2012,142/143:161-181.
[28] SHU Q,BREY G P,GERDES A,et al.Geochronolo-gical and Geochemical Constraints on the Formation and Evolution of the Mantle Underneath the Kaapvaal Craton:Lu-Hf and Sm-Nd Systematics of Subcalcic Garnets from Highly Depleted Peridotites[J].Geo-chimica et Cosmochimica Acta,2013,113(4):1-20.
[29] HUANG J X,GRIFN W L,GRÉAU Y,et al.Unmasking Xenolithic Eclogites:Progressive Metasomatism of a Key Roberts Victor Sample[J].Chemical Geology,2014,364:56-65.
[30] AULBACH S,HEAMAN L M,JACOB D E,et al.Ages and Sources of Mantle Eclogites:ID-TIMS and In-situ MC-ICPMS Pb-Sr Isotope Systematics of Clinopyroxene[J].Chemical Geology,2019,503:15-28.
[31] SCHULZE D J.Constraints on the Abundance of Eclogite in the Upper Mantle[J].Journal of Geophysical Research:Solid Earth,1989,94(B4):4205-4212.
[32] RICHARDSON S H,SHIREY S B,HARRIS J W,et al.Archean Subduction Recorded by Re-Os Isotopes in Eclogitic Sulfide Inclusions in Kimberley Diamonds[J].Earth and Planetary Science Letters,2001,191(3/4):257-266.
[33] AULBACH S,CREASER R A,PEARSON N J,et al.Sulfide and Whole Rock Re-Os Systematics of Eclogite and Pyroxenite Xenoliths from the Slave Craton,Canada[J].Earth and Planetary Science Letters,2009,283(1/2/3/4):48-58.
[34] GONZAGA R G,MENZIES M A,THIRLWALL M F,et al.Eclogites and Garnet Pyroxenites:Problems Resolving Provenance Using Lu-Hf,Sm-Nd and Rb-Sr Isotope Systems[J].Journal of Petrology,2010,51(1/2):513-535.
[35] BREY G P,SHU Q.The Birth,Growth and Ageing of the Kaapvaal Subcratonic Mantle[J].Mineralogy and Petrology,2018,112(1):23-41.
[36] SCHMIDBERGER S S,SIMONETTI A,HEAMAN L M,et al.Lu-Hf,In-situ Sr and Pb Isotope and Trace Element Systematics for Mantle Eclogites from the Diavik Diamond Mine:Evidence for Paleoproterozoic Subduction Beneath the Slave Craton,Canada[J].Earth and Planetary Science Letters,2007,254(1/2):55-68.
[37] SHCHUKINA E V,AGASHEV A M,ZEDGENIZOV D A.Origin of Zircon-bearing Mantle Eclogites Entrained in the V.Grib Kimberlite(Arkhangelsk Region,NW Russia):Evidence from Mineral Geochemistry and the U-Pb and Lu-Hf Isotope Compositions of Zircon[J].Mineralogy and Petrology,2018,112(1):85-100.
[38] RAGOZIN A L,ZEDGENIZOV D A,SHATSKII V S,et al.U-Pb Age of Rutile from the Eclogite Xenolith of the Udachnaya Kimberlite Pipe[J].Doklady Earth Sciences,2014,457(1):861-864.
[39] SUN J,MITCHELL R N,KOSTROVITSKY S I,et al.Siberia's Largest Pulse of Kimberlites:U-Pb Geochronology of Perovskite and Rutile from the Obnazhennaya Kimberlite and Its Xenoliths,Siberia Craton[J].International Geology Review,2022,64(12):1743-1754.
[40] SCHMIDBERGER S S,HEAMAN L M,SIMONETTI A,et al.Formation of Paleoproterozoic Eclogitic Mantle,Slave Province(Canada):Insights from In-situ Hf and U-Pb Isotopic Analyses of Mantle Zircons[J].Earth and Planetary Science Letters,2005,240(3/4):621-633.
[41] SMART K A,TAPPE S,SIMONETTI A,et al.Tectonic Significance and Redox State of Paleoproterozoic Eclogite and Pyroxenite Components in the Slave Cratonic Mantle Lithosphere,Voyageur Kimberlite,Arctic Canada[J].Chemical Geology,2017,455:98-119.
[42] LEE J K W,WILLIAMS I S,ELLIS D J.Pb,U and Th Diffusion in Natural Zircon[J].Nature,1997,390:159-162.
[43] PEARSON D G,WITTIG N.The Formation and Evolution of Cratonic Mantle Lithosphere:Evidence from Mantle Xenoliths[J].Treatise on Geochemistry(Se-cond Edition),2014,3:255-292.
[44] 吴元保,郑永飞.锆石成因矿物学研究及其对U-Pb年龄解释的制约[J].科学通报,2004,49(16):1589-1604.
WU Yuan-bao,ZHENG Yong-fei.Genetic Mineralogy of Zircons and Its Constraints to the Age of U-Pb Geochronology[J].Chinese Science Bulletin,2004,49(16):1589-1604.
[45] MELNIK A E,KOROLEV N M,SKUBLOV S G,et al.Zircon in Mantle Eclogite Xenoliths:A Review[J].Geological Magazine,2021,158(8):1371-1382.
[46] 陈道公,李彬贤,夏群科,等.变质岩中锆石U-Pb计时问题评述:兼论大别造山带锆石定年[J].岩石学报,2001,17(1):129-138.
CHEN Dao-gong,LI Bin-xian,XIA Qun-ke,et al.An Evaluation of Zircon U-Pb Dating for Metamorphic Rocks and Comments on Zircon Ages of Dabie Orogen[J].Acta Petrologica Sinica,2001,17(1):129-138.
[47] HEAMAN L M,CREASER R A,COOKENBOO H O.Extreme Enrichment of High Field Strength Elements in Jericho Eclogite Xenoliths:A Cryptic Record of Paleoproterozoic Subduction,Partial Melting,and Metasomatism Beneath the Slave Craton,Canada[J].Geology,2002,30(6):507-510.
[48] SCHMITZ M D,BOWRING S A.The Significance of U-Pb Zircon Dates in Lower Crustal Xenoliths from the Southwestern Margin of the Kaapvaal Craton:Southern Africa[J].Chemical Geology,2001,172(1/2):59-76.
[49] 吴福元,李献华,郑永飞,等.Lu-Hf同位素体系及其岩石学应用[J].岩石学报,2007,23(2):185-220.
WU Fu-yuan,LI Xian-hua,ZHENG Yong-fei,et al.Lu-Hf Isotopic Systematics and Their Applications in Petrology[J].Acta Petrologica Sinica,2007,23(2):185-220.
[50] KARAEVANGELOU M,KOPYLOVA M G,LUO Y,et al.Mineral Inclusions in Lace Diamonds and the Mantle Beneath the Kroonstad Kimberlite Cluster in South Africa[J].Contributions to Mineralogy and Petrology,2022,177(2):1-22.
[51] AULBACH S,HÖFER H E,GERDES A.High-Mg and Low-Mg Mantle Eclogites from Koidu(West African Craton)Linked by Neoproterozoic Ultramafic Melt Metasomatism of Subducted Archaean Plateau-like Oceanic Crust[J].Journal of Petrology,2019,60(4):723-754.
[52] SMART K A,THOMAS C,ANTONIO S,et al.A Record of Paleoproterozoic Subduction Preserved in the Northern Slave Cratonic Mantle:Sr-Pb-O Isotope and Trace-element Investigations of Eclogite Xenoliths from the Jericho and Muskox Kimberlites[J].Journal of Petrology,2014,55(3):549-583.
[53] 陈安平,张宏福.造山带榴辉岩的变质作用P-T-t轨迹研究进展[J].岩石学报,2023,39(1):170-186.
CHEN An-ping,ZHANG Hong-fu.Recent Progresses in Metamorphic P-T-t Path of Orogenic Eclogites[J].Acta Petrologica Sinica,2023,39(1):170-186.
[54] 李秋立,杨亚楠,石永红,等.榴辉岩中金红石 U-Pb定年:对大陆碰撞造山带形成和演化的制约[J].科学通报,2013,58(23):2279-2284.
LI Qiu-li,YANG Ya-nan,SHI Yong-hong,et al.Eclogite Rutile U-Pb Dating:Constraint for Formation and Evolution of Continental Collisional Orogen[J].Chinese Science Bulletin,2013,58(23):2279-2284.
[55] PEARSON D G,WITTIG N.Formation of Archaean Continental Lithosphere and Its Diamonds:The Root of the Problem[J].Journal of the Geological Society,2008,165(5):895-914.
[56] AFANASYEV V P,AGASHEV A M,ORIHASHI Y,et al.Paleozoic U-Pb Age of Rutile Inclusions in Diamonds of the Ⅴ-Ⅶ Variety from Placers of the Northeast Siberian Platform[J].Doklady Earth Scien-ces,2009,428(7):1151-1155.
[57] KINNY P D,GRIFFIN B J,HEAMAN L M,et al.Shrimp U-Pb Ages of Perovskite from Yakutian Kimberlites[J].Russian Geology and Geophysics,1997,38:91-99.
[58] 李曙光,安诗超.变质岩同位素年代学:Rb-Sr和Sm-Nd体系[J].地学前缘,2014,21(3):246-255.
LI Shu-guang,AN Shi-chao.Isotope Geochronology of Metamorphic Rocks:Rb-Sr and Sm-Nd Systematics[J].Earth Science Frontiers,2014,21(3):246-255.
[59] SCHERER E E,CAMERON K L,BLICHERT-TOFT J.Lu-Hf Garnet Geochronology:Closure Temperature Relative to the Sm-Nd System and the Effects of Tra-ce Mineral Inclusions[J].Geochimica et Cosmochimica Acta,2000,64(19):3413-3432.
[60] PELTONEN P,KINNUNEN K A,HUHMA H.Petrology of Two Diamondiferous Eclogite Xenoliths from the Lahtojoki Kimberlite Pipe,Eastern Finland[J].Lithos,2002,63(3/4):151-164.
[61] SHCHUKINA E V,AGASHEV A M,SOLOSHENKO N G,et al.Origin of V.Grib Pipe Eclogites(Arkhangelsk Region,NW Russia):Geochemistry,Sm-Nd and Rb-Sr Isotopes and Relation to Regional Precambrian Tectonics[J].Mineralogy and Petrology,2019,113(5):593-612.
[62] JAGOUTZ E,DAWSON J B,HOERNES S,et al.Anorthositic Oceanic Crust in the Archean Earth[C]∥RYDER G,SCHUBERT G.15th Lunar and Planetary Science Conference.Houston:NASA,1984:395-396.
[63] SHU Q,BREY G P,GERDES A,et al.Mantle Eclogites and Garnet Pyroxenites:The Meaning of Two-point Isochrons,Sm-Nd and Lu-Hf Closure Temperatures and the Cooling of the Subcratonic Mantle[J].Earth and Planetary Science Letters,2014,389:143-154.
[64] 靳新娣,李文君,吴华英,等.同位素定年方法进展及ICP-MS精确定年测试关键技术[J].岩石学报,2010,26(5):1617-1624.
JIN Xin-di,LI Wen-jun,WU Hua-ying,et al.Development of Re-Os Isotopic Dating Analytical Technique and Determination Know:How on ICP-MS Precise Dating for Molybdenite[J].Acta Petrologica Sinica,2010,26(5):1617-1624.
[65] NIKITINA L P,BOGOMOLOV E S,KRYMSKY R S,et al.Nd-Sr-Os Systems of Eclogites in the Lithospheric Mantle of the Kasai Craton(Angola)[J].Russian Geology and Geophysics,2017,58(11):1305-1316.
[66] SHIREY S B,RICHARDSON S H.Start of the Wilson Cycle at 3 Ga Shown by Diamonds from Subcontinental Mantle[J].Science,2011,333:434-436.
[67] GRESS M U,KOORNNEEF J M,THOMASSOT E,et al.Sm-Nd Isochron Ages Coupled with C-N Isotope Data of Eclogitic Diamonds from Jwaneng,Bots-wana[J].Geochimica et Cosmochimica Acta,2021,293:1-17.
[68] 吕 串,高剑峰,漆 亮,等.硫化物Re-Os同位素定年分析方法及其在矿床年代学中的应用:研究现状及存在问题[J].地球科学,2023,48(12):4387-4403.
LYU Chuan,GAO Jian-feng,QI Liang,et al.Analytical Methods and Application of Sulfide Re-Os Isotope Dating of Mineral Deposits:Research Progress and Problems[J].Earth Science,2023,48(12):4387-4403.
[69] TAPPE S,SMART K,TORSVIK T,et al.Geodyna-mics of Kimberlites on a Cooling Earth:Clues to Plate Tectonic Evolution and Deep Volatile Cycles[J].Earth and Planetary Science Letters,2018,484:1-14.
[70] RICHARDSON S H,SHIREY S B,HARRIS J W.Episodic Diamond Genesis at Jwaneng,Botswana,and Implications for Kaapvaal Craton Evolution[J].Li-thos,2004,77(1/2/3/4):143-154.
[71] TIMMERMAN S,KOORNNEEF J M,CHINN I L,et al.Dated Eclogitic Diamond Growth Zones Reveal Variable Recycling of Crustal Carbon Through Time[J].Earth and Planetary Science Letters,2017,463:178-188.
[72] TAPPE S,SMART K,PEARSON D G,et al.Craton Formation in Late Archean Subduction Zones Revea-led by First Greenland Eclogites[J].Geology,2011,39(12):1103-1106.
[73] NIKITINA L P,KOROLEV N M,ZINCHENKO V N,et al.Eclogites from the Upper Mantle Beneath the Kasai Craton(Western Africa):Petrography,Whole-rock Geochemistry and U-Pb Zircon Age[J].Precambrian Research,2014,249:13-32.
[74] CONDIE K C.Episodic Continental Growth and Supercontinents:A Mantle Avalanche Connection?[J].Earth and Planetary Science Letters,1998,163(1/2/3/4):97-108.
[75] ZHAO G C,CAWOOD P A,WILDE S A,et al.Review of Global 2.1-1.8 Ga Orogens:Implications for a Pre-Rodinia Supercontinent[J].Earth-science Reviews,2002,59(1/2/3/4):125-162.
[76] AULBACH S,VILJOEN K S.Eclogite Xenoliths from the Lace Kimberlite,Kaapvaal Craton:From Convecting Mantle Source to Palaeo-ocean Floor and Back[J].Earth and Planetary Science Letters,2015,431:274-286.

相似文献/References:

[1]翟明国.大陆动力学的物质演化研究方向与思路[J].地球科学与环境学报,2015,37(04):1.
　ZHAI Ming-guo.New Research Interests and Concept of Material Evolution for Continental Dynamics[J].Journal of Earth Sciences and Environment,2015,37(01):1.
[2]杨高学.俯冲起始的机制、地质记录及其研究意义[J].地球科学与环境学报,2023,45(02):194.[doi:10.19814/j.jese.2022.09011]
　YANG Gao-xue.Mechanism, Geological Record and Significance of Subduction Initiation[J].Journal of Earth Sciences and Environment,2023,45(01):194.[doi:10.19814/j.jese.2022.09011]

备注/Memo

备注/Memo:

收稿日期:2023-09-04; 修回日期:2023-12-01投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(42072060); 自然资源部部门预算项目(121101000000180044)
作者简介:蒋蕾茵(1999-),女,浙江台州人,理学硕士研究生,E-mail:jiangleiyin@gmail.com。
*通信作者:孙 晶(1987-),女,黑龙江大庆人,副教授,理学博士,E-mail:sunjing@cup.edu.cn。

常用功能

更新日期/Last Update: 2024-01-25