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[1]郭 涛,胡作维*,李 云,等.四川北川地区中泥盆统养马坝组碎屑锆石U-Pb年代学特征及其构造意义[J].地球科学与环境学报,2021,43(05):868-886.[doi:10.19814/j.jese.2021.01013]
 GUO Tao,HU Zuo-wei*,LI Yun,et al.Detrital Zircon U-Pb Dating of Middle Devonian Yangmaba Formation in Beichuan Area of Sichuan, China and Its Tectonic Significance[J].Journal of Earth Sciences and Environment,2021,43(05):868-886.[doi:10.19814/j.jese.2021.01013]
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四川北川地区中泥盆统养马坝组碎屑锆石U-Pb年代学特征及其构造意义(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第43卷
期数:
2021年第05期
页码:
868-886
栏目:
基础地质与矿产地质
出版日期:
2021-09-15

文章信息/Info

Title:
Detrital Zircon U-Pb Dating of Middle Devonian Yangmaba Formation in Beichuan Area of Sichuan, China and Its Tectonic Significance
文章编号:
1672-6561(2021)05-0868-19
作者:
郭 涛12胡作维12*李 云12史 格12詹旗胜12李韶昱12管晋红12
(1. 成都理工大学 沉积地质研究院,四川 成都 610059; 2. 成都理工大学 油气藏地质及开发工程国家重点实验室,四川 成都 610059)
Author(s):
GUO Tao12 HU Zuo-wei12* LI Yun12 SHI Ge12 ZHAN Qi-sheng12 LI Shao-yu12 GUAN Jin-hong12
(1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China)
关键词:
物源 碎屑锆石U-Pb年龄 中泥盆统 沉积再旋回 古地理 冈瓦纳大陆 扬子板块 四川
Keywords:
provenance detrital zircon U-Pb age Middle Devonian sedimentary recycle paleogeography Gondwana continent Yangtze block Sichuan
分类号:
P597
DOI:
10.19814/j.jese.2021.01013
文献标志码:
A
摘要:
扬子板块与冈瓦纳大陆在中泥盆世是否存在亲缘性一直有较大的分歧,两者的古地理位置关系对扬子板块的构造演化具有重要意义。扬子板块西北缘四川北川地区中泥盆统养马坝组的碎屑锆石U-Pb定年结果表明:碎屑锆石年龄谱主要集中在1 000~900、850~720、650~500 Ma等3个区间,与冈瓦纳大陆以及下伏地层志留系碎屑锆石年龄谱进行比较,发现它们具有相似的碎屑锆石特征,均显示出典型的冈瓦纳特征。结合古地磁数据、养马坝组沉积环境演化特征、岩相古地理特征、大地构造演化特征以及前人研究成果等信息,综合分析了研究区养马坝组陆源碎屑的可能来源,认为其碎屑物质可能来自于下伏地层志留系沉积岩的沉积再旋回,中泥盆世扬子板块与冈瓦纳大陆不具有亲缘性。
Abstract:
Whether Yangtze block and Gondwana continent are related to each other during Middle Devonian, the paleo-geographical relationship between the two is of great significance to the tectonic evolution of Yangtze block. Based on the detrital zircon U-Pb chronology of Middle Devonian Yangmaba Formation in Beichuan area of Sichuan on the northwestern margin of Yangtze block, the results show that the age spectrum of detrital zircon is mainly concentrated in three intervals of 1 000-900, 850-720 and 650-500 Ma. Compared with Gondwana continent and the underlying Silurian detrital zircon age spectrum, it is found that they have similar detrital zircon characteristics, all showing typical Gondwana characteristics. Combined with the paleomagnetic data, the evolution characteristics of sedimentary environment of Yangmaba Formation, the evolution characteristics of lithofacies and paleogeography, the characteristics of tectonic evolution, and the results of previous studies, the possible sources of terrigenous clastics in Yangmaba Formation are comprehensively analyzed. The detrital material in Yangmaba Formation may come from the sedimentary recycle of the underlying Silurian sedimentary rocks, and Yangtze block is not related to Gondwana continent during Middle Devonian.

参考文献/References:

[1] YANG C,LI X H,LI Z X,et al.Provenance Evolution of Age-calibrated Strata Reveals When and How South China Block Collided with Gondwana[J].Geophysical Research Letters,2020,47(19):1-9.
[2] QIU L,YAN D P,TANG S L,et al.Insights into Post-orogenic Extension and Opening of the Palaeo-Tethys Ocean Recorded by an Early Devonian Core Complex in South China[J].Journal of Geodynamics,2020,135:1-14.
[3] LUO L,ZENG L,WANG K,et al.Provenance Investigation for the Cambrian-Ordovician Strata from the Northern Margin of the Western Yangtze Block:Implications for Locating the South China Block in Gondwana[J].Geological Magazine,2019,157(4):1-22.
[4] LUO L,ZENG L,WANG K,et al.Detrital Zircon Provenance Investigation from the Neoproterozoic Successions of the South China Block:Paleogeogra-phic Implications[J].Journal of Geodynamics,2019,124:25-37.
[5] CHEN Q,SUN M,LONG X,et al.Provenance Study for the Paleozoic Sedimentary Rocks from the West Yangtze Block:Constraint on Possible Link of South China to the Gondwana Supercontinent Reconstruction[J].Precambrian Research,2018,309:271-289.
[6] 冼汉标.华南新元古代马底驿组和中泥盆世云台观组古地磁结果及其大地构造意义[D].北京:中国地质大学,2020.
XIAN Han-biao.Paleomagnetic Results from Neoproterozoic Madiyi Formation and Middle Devonian Yuntaiguan Formation in South China and Their Tectonic Implications[D].Beijing:China University of Geosciences,2020.
[7] CAWOOD P A,WANG Y,XU Y,et al.Locating South China in Rodinia and Gondwana:A Fragment of Greater India Lithosphere?[J].Geology,2013,41(8):903-906.
[8] LIKHANOV I I,NOZHKIN A D,REVERDATTO V V,et al.Grenville Tectonic Events and Evolution of the Yenisei Ridge at the Western Margin of the Siberian Craton[J].Geotectonics,2014,48(5):371-389.
[9] WANG Y J,WEI M F,ZHANG G W,et al.Phanerozoic Tectonics of the South China Block:Key Observations and Controversies[J].Gondwana Research,2013,23(4):1273-1305.
[10] 张国伟,郭安林,王岳军,等.中国华南大陆构造与问题[J].中国科学:地球科学,2013,43(10):1553-1582.
ZHANG Guo-wei,GUO An-lin,WANG Yue-jun,et al.Tectonics of South China Continent and Its Implications[J].Science China:Earth Sciences,2013,43(10):1553-1582.
[11] DUAN L,MENG Q R,WU G L,et al.Detrital Zircon Evidence for the Linkage of the South China Block with Gondwanaland in Early Palaeozoic Time[J].Geological Magazine,2013,149(6):1124-1131.
[12] DUAN L,MENG Q R,ZHANG C L,et al.Tracing the Position of the South China Block in Gondwana:U-Pb Ages and Hf Isotopes of Devonian Detrital Zircons[J].Gondwana Research,2011,19(1):141-149.
[13] 段 亮.南秦岭与扬子地体西北缘志留—泥盆系碎屑锆石物源分析及构造意义[D].西安:西北大学,2010.
DUAN Liang.Detrital Zircon Provenance of the Silurian and Devonian in South Qingling,and the Northwestern Margin of Yangtze Terrane and Its Tectonic Implications[D].Xi'an:Northwest University,2010.
[14] CHEN Q,SUN M,LONG X P,et al.U-Pb Ages and Hf Isotopic Record of Zircons from the Late Neopro-terozoic and Silurian-Devonian Sedimentary Rocks of the Western Yangtze Block:Implications for Its Tectonic Evolution and Continental Affinity[J].Gondwana Research,2016,31:184-199.
[15] 李学森.扬子地块四川江油地区上泥盆统—下石炭统古地磁研究[D].西安:西北大学,2001.
LI Xue-sen.Paleomagnetic Study of the Upper Devonian and the Lower Carboniferous Carbonates near Jiangyou,Sichuan,South China Block[D].Xi'an:Northwest University,2001.
[16] ZHANG S H.South China's Gondwana Connection in the Paleozoic:Paleomagnetic Evidence[J].Progress in Natural Science,2004,14(1):85-90.
[17] XIAN H B,ZHANG S H,LI H,et al.How Did South China Connect to and Separate from Gondwana?New Paleomagnetic Constraints from the Middle Devonian Red Beds in South China[J].Geophysical Research Letters,2019,46(13):7371-7378.
[18] 白志强.泥盆纪华南板块古地理的位置及其漂移[J].北京大学学报(自然科学版),1998,34(6):101-106.
BAI Zhi-qiang.The Paleogeographical Position and Drifting of the Southern China Block in Devonian[J].Acta Scientiarum Naturalium Universitatis Pekinensis,1998,34(6):101-106.
[19] 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.Zircon Genetic Mi-neralogy and Its Constraints on the Interpretation of U-Pb Age[J].Chinese Science Bulletin,2004,49(16):1589-1604.
[20] GEHRELS G E,DICKINSON W R,ROSS G M,et al.Detrital Zircon Reference for Cambrian to Triassic Miogeoclinal Strata of Western North America[J].Geology,1995,23(9):831-834.
[21] CAWOOD P A,NEMCHIN A A.Provenance Record of a Rift Basin:U/Pb Ages of Detrital Zircons from the Perth Basin,Western Australia[J].Sedimentary Geology,2000,134(3/4):209-234.
[22] 杨江海.造山带碰撞-隆升过程的碎屑沉积响应:以北祁连志留系、右江二叠—三叠系和大别山南麓侏罗系为例[D].武汉:中国地质大学,2012.
YANG Jiang-hai.Detrital Record of Collision and Exhumation Processes of Orogen:Studies from the Silurian in North Qilian Belt,the Permian-Triassic in Youjiang Basin and the Jurassic at Huangshi South of Dabie Mountains[D].Wuhan:China University of Geosciences,2012.
[23] DAVIS S J,DICKINSON W R,GEHRELS G E,et al.The Paleogene California River:Evidence of Mojave-Uinta Paleodrainage from U-Pb Ages of Detrital Zircons[J].Geology,2010,38(10):931-934.
[24] BLUM M,PECHA M.Mid-Cretaceous to Paleocene North American Drainage Reorganization from Detrital Zircons[J].Geology,2014,42(7):607-610.
[25] SURPLESS K D,GRAHAM S A,COVAULT J A,et al.Does the Great Valley Group Contain Jurassic Strata?Reevaluation of the Age and Early Evolution of a Classic Forearc Basin[J].Geology,2006,34(1):21-24.
[26] POLLOCK J C,HIBBARD J P,SYLVESTER P J,et al.Early Ordovician Rifting of Avalonia and Birth of the Rheic Ocean:U-Pb Detrital Zircon Constraints from Newfoundland[J].Journal of the Geological Society,2009,166(3):501-515.
[27] LAWTON T F,HUNT G J,GEHRELS G E.Detrital Zircon Record of Thrust Belt Unroofing in Lower Cretaceous Synorogenic Conglomerates,Central Utah[J].Geology,2010,38(5):463-466.
[28] 徐绪东,李凤杰,闫大伟,等.龙门山区北川甘溪剖面泥盆系养马坝组铁质鲕粒成因及其古环境讨论[J].中国地质,2021,48(1):322-331.
XU Xu-dong,LI Feng-jie,YAN Da-wei,et al.Genesis and Paleoenvironment of the Iron Ooids from the Ganxi Prolife of the Devonian Yangmaba Formation in Beichuan County,Longmenshan Area[J].Geology in China,2021,48(1):322-331.
[29] 黄 敏,朱怀诚,刘 锋,等.四川龙门山地区早中泥盆世孢子化石研究[J].地质论评,2016,62(6):1533-1548.
HUANG Min,ZHU Huai-cheng,LIU Feng,et al.Lower and Middle Devonian Spore Assemblages from Longmen Mountains,Sichuan Province[J].Geological Review,2016,62(6):1533-1548.
[30] 李凤杰,李佐强,沈 凡,等.龙门山地区中泥盆统观雾山组沉积相及其演化分析[J].中国海上油气,2020,32(1):32-41.
LI Feng-jie,LI Zuo-qiang,SHEN Fan,et al.Sedimentary Facies and Evolution Analysis of the Middle Devonian Guanwushan Formation in the Longmenshan Area[J].China Offshore Oil and Gas,2020,32(1):32-41.
[31] 邓予炜,侯明才,陈安清,等.川西北观雾山组白云岩稀土元素特征及其对白云岩化流体性质的指示[J].成都理工大学学报(自然科学版),2018,45(3):282-291.
DENG Yu-wei,HOU Ming-cai,CHEN An-qing,et al.REE Characteristics of Dolomites and Indication of Dolomitization Fluid in Guanwushan Formation,NW Sichuan Basin,China[J].Journal of Chengdu University of Technology(Science and Technology Edition),2018,45(3):282-291.
[32] 冯春强.川西北部地区泥盆系有利储集相带预测[D].成都:西南石油大学,2016.
FENG Chun-qiang.Prediction of Favorable Reservoir Belt of Devonian System in Northwestern Sichuan[D].Chengdu:Southwest Petroleum University,2016.
[33] MENG Q R,WANG E,HU J M.Mesozoic Sedimentary Evolution of the Northwest Sichuan Basin:Implication for Continued Clockwise Rotation of the South China Block[J].Geological Society of America Bulletin,2005,117(3):396-410.
[34] 郑荣才,文华国,王昌勇,等.龙门山泥盆系野外实习指南[M].北京:地质出版社,2016.
ZHENG Rong-cai,WEN Hua-guo,WANG Chang-yong,et al.Longmen Mountain Devonian Field Practice Guide[M].Beijing:Geological Publishing House,2016.
[35] JACKSON S E,PEARSON N J,GRIFFIN W L,et al.The Application of Laser Ablation-inductively Coupled Plasma-mass Spectrometry to In-situ U-Pb Zircon Geochronology[J].Chemical Geology,2004,211(1/2):47-69.
[36] 罗宏谓.川东南志留系小河坝组物源分析[D].成都:成都理工大学,2019.
LUO Hong-wei.Provenance of Xiaoheba Formation of Silurian in Southeast Sichuan[D].Chengdu:Chengdu University of Technology,2019.
[37] LIU Y S,HU Z C,GAO S,et al.In-situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS Without Applying an Internal Standard[J].Chemical Geology,2008,257(1/2):34-43.
[38] GRIFFIN W L,BELOUSOVA E A,SHEE S R,et al.Archean Crustal Evolution in the Northern Yilgarn Craton:U-Pb and Hf-isotope Evidence from Detrital Zircons[J].Precambrian Research,2004,131(3/4):231-282.
[39] ANDERSEN T.Correction of Common Lead in U-Pb Analyses That Do Not Report 204Pb[J].Chemical Geo-logy,2002,192(1/2):59-79.
[40] LUDWIG K R.User's Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center,2003.
[41] HOSKIN P W,BLACK L P.Metamorphic Zircon Formation by Solid-state Recrystallization of Protolith Igneous Zircon[J].Journal of Metamorphic Geology,2002,18(4):423-439.
[42] 雷玮琰,施光海,刘迎新.不同成因锆石的微量元素特征研究进展[J].地学前缘,2013,20(4):273-284.
LEI Wei-yan,SHI Guang-hai,LIU Ying-xin.Research Progress on Trace Element Characteristics of Zircons of Different Origins[J].Earth Science Frontiers,2013,20(4):273-284.
[43] 胡俊良,刘劲松,刘阿睢,等.北大别木子店岩体斑状黑云二长花岗岩的年龄与成因:锆石U-Pb定年、Hf同位素与稀土元素证据[J].矿物岩石地球化学通报,2018,37(4):750-759.
HU Jun-liang,LIU Jin-song,LIU A-sui,et al.Age and Petrogenesis of the Porphyritic Biotite Monzogra-nite in the Muzidian Complex in Northern Dabie Mountains:Evidences from Zircon U-Pb Dating,Hf Isotopes and REE Geochemistry[J].Bulletin of Mine-ralogy,Petrology and Geochemistry,2018,37(4):750-759.
[44] 佘振兵.中上扬子上元古界—中生界碎屑锆石年代学研究[D].武汉:中国地质大学,2007.
SHE Zhen-bing.Detrital Zircon Geochronology of the Upper Proterozoic-Mesozoic Clastic Rocks in the Mid-upper Yangtze Region[D].Wuhan:China University of Geosciences,2007.
[45] MUNOZ M,CHARRIER R,FANNING C M,et al.Zircon Trace Element and O-Hf Isotope Analyses of Mineralized Intrusions from EI Teniente Ore Deposit,Chilean Andes:Constraints on the Source and Magmatic Evolution of Porphyry Cu-Mo Related Magmas[J].Journal of Petrology,2012,53(6):1091-1122.
[46] POWELL C M,PISAREVSKY S A.Late Neoproterozoic Assembly of East Gondwana[J].Geology,2002,30(1):3-6.
[47] COCKS L R M,TORSVIK T H.Earth Geography from 500 to 400 Million Years Ago:A Faunal and Palaeomagnetic Review[J].Journal of the Geological Society,2002,159(6):631-644.
[48] LI Z X,LI X H,KINNY P D,et al.The Breakup of Rodinia:Did It Start with a Mantle Plume Beneath South China?[J].Earth and Planetary Science Letters,1999,173(3):171-181.
[49] 郭 佩,刘池洋,王建强,等.碎屑锆石年代学在沉积物源研究中的应用及存在问题[J].沉积学报,2017,35(1):46-56.
GUO Pei,LIU Chi-yang,WANG Jian-qiang,et al.Considerations on the Application of Detrital-zircon Geochronology to Sedimentary Provenance Analysis[J].Acta Sedimentologica Sinica,2017,35(1):46-56.
[50] 刘文均,郑荣才,李祥辉.龙门山泥盆纪沉积盆地的古地理和古构造重建[J].地质学报,1999,73(2):109-119.
LIU Wen-jun,ZHENG Rong-cai,LI Xiang-hui.Reconstruction of Palaeogeography and Palaeotectonics of a Devonian Sedimentary Basin in the Longmenshan Area,Sichuan[J].Acta Geologica Sinica,1999,73(2):109-119.
[51] 李佐强,李凤杰,赖雪莲,等.龙门山区中泥盆统养马坝组混积相与混积层序及其控制因素分析[J].科学技术与工程,2020,20(26):10580-10591.
LI Zuo-qiang,LI Feng-jie,LAI Xue-lian,et al.Analysis of Hybrid Facies,Hybrid Sequence and Its Controlling Factors of the Middle Devonian Yangmaba Formation in Longmenshan Area[J].Science Technology and Engineering,2020,20(26):10580-10591.
[52] 张 昊,李凤杰,沈 凡,等.四川盆地龙门山区甘溪石沟里泥盆系养马坝组风暴沉积特征及其地质意义[J].古地理学报,2019,21(3):441-450.
ZHANG Hao,LI Feng-jie,SHEN Fan,et al.Storm Deposits Characteristics and Its Geological Significance in the Devonian Yangmaba Formation from Shigouli Section,Longmenshan Area,Sichuan Basin[J].Journal of Palaeogeography,2019,21(3):441-450.
[53] 曾允孚,张锦泉,刘文均,等.中国南方泥盆纪岩相古地理与成矿作用[M].北京:地质出版社,1993.
ZENG Yun-fu,ZHANG Jin-quan,LIU Wen-jun,et al.Devonian Lithofacies and Paleogeography and Mineralization in Southern China[M].Beijing:Geological Publishing House,1993.
[54] GARZANTI E.Petrographic Classification of Sand and Sandstone[J].Earth Science Reviews,2019,192:545-563.
[55] DICKINSON W R,SUCZEK C A.Block Tectonics and Sandstone Compositions[J].AAPG Bulletin,1979,63(12):2164-2182.
[56] DICKINSON W R.Interpreting Provenance Relations from Detrital Modes of Sandstones[J].Provenance of Arenites,1985,148:333-362.
[57] 罗志立.四川盆地基底结构的新认识[J].成都理工学院学报,1998,25(2):85-92,94.
LUO Zhi-li.New Recognition of Basement in Sichuan Basin[J].Journal of Chengdu University of Technology,1998,25(2):85-92,94.
[58] 杨逢清,殷鸿福,杨恒书,等.松潘甘孜地块与秦岭褶皱带、扬子地台的关系及其发展史[J].地质学报,1994,68(3):208-218.
YANG Feng-qing,YIN Hong-fu,YANG Heng-shu,et al.The Songpan-Ganze Massif:Its Relationship with the Qinling Fold Belt and Yangtze Platform and Development[J].Acta Geologica Sinica,1994,68(3):208-218.
[59] 庞艳君,张本健,冯仁蔚,等.龙门山构造带北段泥盆系沉积环境演化[J].世界地质,2010,29(4):561-568.
PANG Yan-jun,ZHANG Ben-jian,FENG Ren-wei,et al.Evolution of Devonian Depositional Environment in Northern Longmenshan Tectonic Belt[J].Global Geology,2010,29(4):561-568.
[60] DECELLES P G,GEHRELS G E,QUADE J,et al.Tectonic Implications of U-Pb Zircon Ages of the Himalayan Orogenic Belt in Nepal[J].Science,2000,288:497-499.
[61] GEHRELS G E,YIN A,WANG X F.Detrital-zircon Geochronology of the Northeastern Tibetan Plateau[J].Geological Society of America Bulletin,2003,115(7):881-896.
[62] MYROW P M,HUGHES N C,PAULSEN T S,et al.Integrated Tectonostratigraphic Analysis of the Himalaya and Implications for Its Tectonic Reconstruction[J].Earth and Planetary Science Letters,2003,212(3/4):433-441.
[63] 倪子尧.龙门山区甘溪中泥盆统养马坝组铁质鲕粒沉积成因分析[D].成都:成都理工大学,2020.
NI Zi-yao.Genetic Analysis of Iron Oolitic Deposition in the Middle Devonian Yangmaba Formation in Gan-xi Prolife,Beichuan County,Longmenshan Area[D].Chengdu:Chengdu University of Technology,2020.
[64] 赵一鸣,毕承思.宁乡式沉积铁矿床的时空分布和演化[J].矿床地质,2000,19(4):350-362.
ZHAO Yi-ming,BI Cheng-si.Time-space Distribution and Evolution of the Ningxiang Type Sedimentary Iron Deposits[J].Mineral Deposits,2000,19(4):350-362.

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[1]杜建军,张士安,肖伟峰,等.柴达木盆地北缘中—下侏罗统碎屑岩地球化学特征及其地质意义[J].地球科学与环境学报,2017,39(06):721.
 DU Jian-jun,ZHANG Shi-an,XIAO Wei-feng,et al.Geochemistry Characteristics of Middle-Lower Jurassic Clastic Rocks in the Northern Margin of Qaidam Basin and Their Geological Significance[J].Journal of Earth Sciences and Environment,2017,39(05):721.
[2]王铁晖,巩恩普,陈晓红,等.辽西义县盆地下白垩统义县组大康堡层纹泥地球化学特征及其古气候意义[J].地球科学与环境学报,2018,40(01):49.
 WANG Tie-hui,GONG En-pu,CHEN Xiao-hong,et al.Geochemical Characteristics and Their Paleoclimatic Significance of the Varve from Dakangpu Layer of Lower Cretaceous Yixian Formation in Yixian Basin of the Western Liaoning, China[J].Journal of Earth Sciences and Environment,2018,40(05):49.
[3]丁振举,文成雄,国阿千,等.西秦岭吴家山群地层时代及物源特征:来自碎屑锆石U-Pb年龄证据[J].地球科学与环境学报,2018,40(02):111.
 DING Zhen-ju,WEN Cheng-xiong,GUO A-qian,et al.Stratigraphic Ages and Provenance Characteristics of Wujiashan Group in West Qinling, China: Evidences from Detrital Zircon U-Pb Age[J].Journal of Earth Sciences and Environment,2018,40(05):111.
[4]陈有炘,裴先治*,王 盟,等.伊犁地块北缘别珍套山中泥盆统汗吉尕组物源特征及其地质意义[J].地球科学与环境学报,2021,43(03):469.[doi:10.19814/j.jese.2021.01029]
 CHEN You-xin,PEI Xian-zhi*,WANG Meng,et al.Provenance Characteristics and Geological Significance of the Middle Devonian Hanjiga Formation in Biezhentao Mountain, the Northern Margin of Yili Block, China[J].Journal of Earth Sciences and Environment,2021,43(05):469.[doi:10.19814/j.jese.2021.01029]

备注/Memo

备注/Memo:
收稿日期:2021-01-18; 修回日期:2021-04-20投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41772100); 国家科技重大专项项目(2016ZX05050)
作者简介:郭 涛(1995-),女,山西晋中人,理学硕士研究生,E-mail:526750403@qq.com。
*通讯作者:胡作维(1981-),男,广东佛山人,教授,理学博士,E-mail:huzuowei@foxmail.com。
更新日期/Last Update: 2021-09-30