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

卷:

第44卷

期数:

2022年第04期

页码:

641-657

栏目:

基础地质与矿产地质

出版日期:

2022-07-15

文章信息/Info

Title:

Geochemistry of Clastic Rocks from Lower Devonian Lianhuashan Formation in Dayaoshan Area of Guangxi, China: Implications for Provenance and Tectonic Setting

文章编号:

1672-6561(2022)04-0641-17

作者:

刘彦兵¹; 刘春发^1*; 屈海浪¹; 翁仲才²; 徐立为¹; 王化奇¹; 蒋正锋²; 黄 冲²; 吴炎潞²

(1. 北京金有地质勘查有限责任公司,北京 100011; 2. 贵港市金地矿业有限责任公司,广西 贵港 537100)

Author(s):

LIU Yan-bing¹;  LIU Chun-fa^1*;  QU Hai-lang¹;  WENG Zhong-cai²;  XU Li-wei¹;  WANG Hua-qi¹;  JIANG Zheng-feng²;  HUANG Chong²;  WU Yan-lu²

(1. Beijing Jinyou Geological Exploration Co. Ltd., Beijing 100011, China; 2. Guigang Jindi Mining Co. Ltd., Guigang 537100, Guangxi, China)

关键词:

元素地球化学;  沉积环境;  物源;  构造背景;  莲花山组;  早泥盆世;  华南板块

Keywords:

elemental geochemistry;  sedimentary environment;  provenance;  tectonic setting;  Lianhuashan Formation;  Early Denonion;  South China block

分类号:

P595

DOI:

10.19814/j.jese.2021.12052

文献标志码:

A

摘要:

受加里东期郁南运动和广西运动影响,华南板块西南部大瑶山地区下泥盆统莲花山组不整合于寒武系之上。对下泥盆统莲花山组砂岩开展岩石学和地球化学研究,探讨其物质来源和构造环境。砂岩碎屑组分以石英和长英质沉积岩岩屑为主,分选和磨圆中等,指示近源沉积。SiO₂含量(质量分数,下同)(74.19%～95.35%,平均值为85.72%)较高,Al₂O₃含量(1.23%～14.73%,平均值为6.48%)和TiO₂含量(0.09%～1.05%,平均值为0.38%)较低,Al₂O₃/SiO₂值(0.01～0.20)极低。砂岩亏损大离子亲石元素,富集高场强元素,稀土元素总含量为(12.48～281.10)×10^-6,轻、重稀土元素分异明显((La/Yb)_N值为3.70～29.40),呈现弱Eu负异常(0.66～1.14,平均值为0.88)。SiO₂/Al₂O₃值(5.04～77.28,平均值为22.30)较高,表明成分成熟度高。成分变异指数(0.61～2.13,平均值为1.21)变化较大,指示源岩包含再循环的古老沉积物与第一次循环物质; 化学蚀变指数为82.13～91.68,反映了强烈化学风化作用。综合地球化学、碎屑锆石U-Pb年代学、岩相古地理和大地构造演化研究成果认为,大瑶山地区下泥盆统莲花山组沉积于被动大陆边缘环境,物源为北侧大瑶山—大明山隆起带和南侧云开地区的隆升剥蚀物质,源岩以寒武系黄洞口组为主,包含少量云开地区新元古代沉积岩和广西运动形成的花岗岩类(470～435 Ma)。

Abstract:

The Lower Devonian Lianhuashan Formation is unconformly unlained by Cambrian strata due to Early Paleozoic Yunan orogeny and Kwangsian orogeny in Dayaoshan area of Guangxi. The new petrology and whole-rock geochemical data of Lower Devonian Lianhuashan Formation in Dayaoshan area were presented in order to constrain their provenance and sedimentary tectonic setting. The sandstones are composed of the predominated moderately sorted and rounded quartz and sedimentary lithic fragments, indicating a close detrital provenance. These samples have obviously high SiO₂ contents(74.19%-95.35% with an average of 85.72%), low Al₂O₃ contents(1.23%-14.73% with an average of 6.48%), TiO₂ contents(0.09%-1.05% with an average of 0.38%)and Al₂O₃/SiO₂(0.01-0.20). The sandstones have low REE contents((12.48-281.10)×10^-6)and are characterized by depletion in LILE, enrichments in HFSE and LREE((La/Yb)_N is 3.70-29.40)coupled with slightly negnative Eu anomaly(0.66-1.14 with an average of 0.88). The high SiO₂/Al₂O₃(5.04-77.28 with an average of 22.30)implies the high grade of maturity. The wide ranges of ICV(0.61-2.13 with an average of 1.21)and high CIA(82.13-91.68)indicate that the source rocks contain recycled ancient sediments and first-cycle materials, which have experienced high degree of chemical weathering and alteration in the heat and humid climate environment of tropical or subtropical zone. Integrated with geochemistry, clastic zircon U-Pb geochronology, paleogeography and tectonic evolution, it is suggested that Lower Devonian Lianhuashan Formation is deposited in passive margin, and its provenance may be Dayaoshan-Damingshan area in the north, and Yunkai area in the south. The source rocks of Lower Devonian Lianhuashan Formation mainly comprise Cambrian Huangdongkou Formation, and minor Neoproterozoic sedimentary rocks of Cathaysia block and the granitoids formed in Kwangsian orogeny(470-435 Ma).

参考文献/References:

[1] WANG Y J,FAN W M,ZHAO G C,et al.Zircon U-Pb Geochronology of Gneissic Rocks in the Yunkai Massif and Its Implications on the Caledonian Event in the South China Block[J].Gondwana Research,2007,12(4):404-416.
[2] 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.
[3] 翟明国.中国主要古陆与联合大陆的形成——综述与展望[J].中国科学:地球科学,2013,43(10):1583-1606.
ZHAI Ming-guo.The Main Old Lands in China and Assembly of Chinese Unified Continent[J].Science China:Earth Sciences,2013,43(10):1583-1606.
[4] 舒良树.华南构造演化的基本特征[J].地质通报,2012,31(7):1035-1053.
SHU Liang-shu.An Analysis of Principal Features of Tectonic Evolution in South China Block[J].Geologi-cal Bulletin of China,2012,31(7):1035-1053.
[5] LI Z X,LI X H,ZHOU H W,et al.Grenvillian Continental Collision in South China:New SHRIMP U-Pb Zircon Results and Implications for the Configuration of Rodinia[J].Geology,2002,30(2):163-166.
[6] TING V K.The Orogenic Movements in China[J].Bulletin of the Geological Society of China,1929,8(1):151-170.
[7] 杜远生,徐亚军.华南加里东运动初探[J].地质科技情报,2012,31(5):43-49.
DU Yuan-sheng,XU Ya-jun.A Preliminary Study on Caledonian Event in South China[J].Geological Science and Technology Information,2012,31(5):43-49.
[8] 徐亚军,杜远生.从板缘碰撞到陆内造山:华南东南缘早古生代造山作用演化[J].地球科学,2018,43(2):333-353.
XU Ya-jun,DU Yuan-sheng.From Periphery Collision to Intraplate Orogeny:Early Paleozoic Orogenesis in Southeastern Part of South China[J].Earth Science,2018,43(2):333-353.
[9] 王 怿,戎嘉余,唐 鹏,等.华南古生代中期地层界面的特征与大地构造意义[J].中国科学:地球科学,2021,51(2):218-240.
WANG Yi,RONG Jia-yu,TANG Peng,et al.Characteristics of Major Hiatus in Middle Paleozoic Rocks of South China and Their Significance of Geotectonics[J].Science China:Earth Sciences,2021,51(2):218-240.
[10] 柏道远,周 亮,王先辉,等.湘东南南华系—寒武系砂岩地球化学特征及对华南新元古代—早古生代构造背景的制约[J].地质学报,2007,81(6):755-771.
BAI Dao-yuan,ZHOU Liang,WANG Xian-hui,et al.Geochemistry of Nanhuan-Cambrian Sandstones in Southeastern Hunan,and Its Constraints on Neopro-terozoic-Early Paleozoic Tectonic Setting of South China[J].Acta Geologica Sinica,2007,81(6):755-771.
[11] 王鹏鸣,于津海,孙 涛,等.湘东新元古代沉积岩的地球化学和碎屑锆石年代学特征及其构造意义[J].岩石学报,2012,28(12):3841-3857.
WANG Peng-ming,YU Jin-hai,SUN Tao,et al.Geochemistry and Detrital Zircon Geochronology of Neoproterozoic Sedimentary Rocks in Eastern Hunan Pro-vince and Their Tectonic Significance[J].Acta Petrologica Sinica,2012,28(12):3841-3857.
[12] 田 洋,金 巍,王 晶,等.江南造山带中段冷家溪群沉积物源及构造背景:以岳阳地区黄浒洞组为例[J].地球科学,2021,46(4):1328-1348.
TIAN Yang,JIN Wei,WANG Jing,et al.Provenance and Tectonic Setting of Lengjiaxi Group in the Central Jiangnan Orogen:A Case Study of Huanghudong Formation,Yueyang Area[J].Earth Science,2021,46(4):1328-1348.
[13] 田 洋.江南造山带西段青白口系—寒武系火山—沉积建造及对华南构造演化的启示[D].武汉:中国地质大学,2021.
TIAN Yang.The Qingbaikouan-Cambrian Volcanic and Sedimentary Sequences in the Western Jiangnan Orogen and Its Implication for Tectonic Evolution of South China[D].Wuhan:China University of Geosciences,2021.
[14] 胡国辉,周艳艳,赵太平.河南嵩山地区元古宙五佛山群沉积岩的地球化学特征及其对物源区和构造环境的制约[J].岩石学报,2012,28(11):3692-3704.
HU Guo-hui,ZHOU Yan-yan,ZHAO Tai-ping.Geochemistry of Proterozoic Wufoshan Group Sedimentary Rocks in the Songshan Area,Henan Province:Implications for Provenance and Tectonic Setting[J].Acta Petrologica Sinica,2012,28(11):3692-3704.
[15] 田 洋,赵小明,王令占,等.鄂西南利川三叠纪须家河组地球化学特征及其对风化、物源与构造背景的指示[J].岩石学报,2015,31(1):261-272.
TIAN Yang,ZHAO Xiao-ming,WANG Ling-zhan,et al.Geochemistry of Clastic Rocks from the Triassic Xu-jiahe Formation,Lichuan Area,Southwestern Hubei:Implications for Weathering,Provenance and Tectonic Setting[J].Acta Petrologica Sinica,2015,31(1):261-272.
[16] 陈懋弘,梁金城,张桂林,等.加里东期扬子板块与华夏板块西南段分界线的岩相古地理制约[J].高校地质学报,2006,12(1):111-122.
CHEN Mao-hong,LIANG Jin-cheng,ZHANG Gui-lin,et al.Lithofacies Paleogeographic Constraints of Southwestern Boundary Between Yangtze and Ca-thaysian Plates in Caledonian[J].Geological Journal of China Universities,2006,12(1):111-122.
[17] 李 青,段瑞春,凌文黎,等.桂东早古生代地层碎屑锆石U-Pb同位素年代学及其对华夏陆块加里东期构造事件性质的约束[J].地球科学,2009,34(1):189-202.
LI Qing,DUAN Rui-chun,LING Wen-li,et al.Detrital Zircon U-Pb Geochronology of the Early Paleozoic Strata in Eastern Guangxi and Its Constraint on the Caledonian Tectonic Nature of the Cathaysian Continental Block[J].Earth Science,2009,34(1):189-202.
[18] 杜晓东,邹和平,苏章歆,等.广西大瑶山—大明山地区寒武纪砂岩-泥岩的地球化学特征及沉积-构造环境分析[J].中国地质,2013,40(4):1112-1128.
DU Xiao-dong,ZOU He-ping,SU Zhang-xin,et al.Geochemical Characteristics and Sedimentary-tectonic Setting of the Cambrian Sandstones and Mudstones in Dayaoshan-Damingshan Area,Guangxi[J].Geology in China,2013,40(4):1112-1128.
[19] 邹和平,杜晓东,劳妙姬,等.广西大明山地块寒武系碎屑锆石U-Pb年龄及其构造意义[J].地质学报,2014,88(10):1800-1819.
ZOU He-ping,DU Xiao-dong,LAO Miao-ji,et al.Detrital Zircon U-Pb Geochronology of Cambrian Sandstones in Damingshan,Central Guangxi and Its Tectonic Implications[J].Acta Geologica Sinica,2014,88(10):1800-1819.
[20] 乔 龙.右江盆地及其周缘地区构造演化及铝土矿成矿作用[D].北京:中国地质大学,2016.
QIAO Long.Tectonic Evolution and Bauxite Metallogenesis in the Youjiang Basin and Adjacent Area[D].Beijing:China University of Geosciences,2016.
[21] 冯洋洋,付 伟,冯佐海,等.广西西大明山隆起带寒武—泥盆系碎屑锆石年龄谱系及其地质意义[J].桂林理工大学学报,2021,41(1):15-26.
FENG Yang-yang,FU Wei,FENG Zuo-hai,et al.Cambrian-Devonian Detrital Zircon U-Pb Age Spectrums and Its Geological Significance for the Xida-mingshan Uplift Zone in Guangxi[J].Journal of Gui-lin University of Technology,2021,41(1):15-26.
[22] 张 雄,曾佐勋,刘 伟,等.湘南—桂东北地区寒武—奥陶纪沉积岩碎屑锆石U-Pb年代学特征及其地质意义[J].中国地质,2016,43(1):153-173.
ZHANG Xiong,ZENG Zuo-xun,LIU Wei,et al.Detrital Zircon Geochronology of Cambrian-Ordovician Sedimentary Rocks in Southern Hunan-Northeast Guangxi Area and Its Tectonic Implications[J].Geo-logy in China,2016,43(1):153-173.
[23] 广西壮族自治区地质矿产局.广西壮族自治区地质志[M].北京:地质出版社,1985.
Bureau of Geology and Mineral Resources of Guangxi Zhuang Autonomous Region Regional Geology of Guangxi Zhuang Autonomous Region[M].Beijing:Geological Publishing House,1985.
[24] 毛治超.广西桂中坳陷泥盆系沉积相与烃源岩地球化学特征研究[D].武汉:中国地质大学,2016.
MAO Zhi-chao.Sedimentary Facies and Geochemical Characteristics of Source Rocks of Devonian in Gui-zhong Depression,Guangxi[D].Wuhan:China University of Geosciences,2016.
[25] 广西壮族自治区地质调查院.贵县幅1:250 000区域地质调查报告[R].南宁:广西壮族自治区地质调查院,2013.
Geological Survey Institute of Guangxi Zhuang Antonomous Region.Regional Geology Survey Report of Guixian Sheet(1:250 000 )[R].Nanning:Geological Survey Institute of Guangxi Zhuang Antonomous Region,2013.
[26] 陈懋弘,李忠阳,李 青,等.初论广西大瑶山地区多期次花岗质岩浆活动与成矿系列[J].地学前缘,2015,22(2):41-53.
CHEN Mao-hong,LI Zhong-yang,LI Qing,et al.A Preliminary Study of Multi-stage Granitoids and Related Metallogenic Series in Dayaoshan Area of Guangxi,China[J].Earth Science Frontiers,2015,22(2):41-53.
[27] 郭春丽,刘泽坤.华南地区加里东期花岗岩:成岩和成矿作用的地质与地球化学特征[J].地球科学与环境学报,2021,43(6):927-961.
GUO Chun-li,LIU Ze-kun.Caledonian Granites in South China:The Geological and Geochemical Characteristics on Their Petrogenesis and Mineralization[J].Journal of Earth Sciences and Environment,2021,43(6):927-961.
[28] 张保涛,胡兆国,姜晓平,等.青海团宝山花岗岩年代学、地球化学特征及其地质意义[J].现代地质,2021,35(2):504-513.
ZHANG Bao-tao,HU Zhao-guo,JIANG Xiao-ping,et al.Geochronological and Geochemical Characteristics of Tuanbaoshan Granite Pluton in Qinghai and Geological Implications[J].Geoscience,2021,35(2):504-513.
[29] TAYLOR S R,MCLENNAN S M.The Continental Crust:Its Composition and Evolution,an Examination of the Geochemical Record Preserved in Sedimentary Rocks[M].Oxford:Blackwell,1985.
[30] 迟清华,鄢明才.应用地球化学元素丰度数据手册[M].北京:地质出版社,2007.
CHI Qing-hua,YAN Ming-cai.Handbook of Elemental Abundance for Applied Geochemistry[M].Beijing:Geological Publishing House,2007.
[31] SUN S S,MCDONOUGH W F.Chemical and Isoto-pic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J].Geological Society,London,Special Publications,1989,42:313-345.
[32] NESBITT H W,YOUNG G M.Early Proterozoic Climates and Plate Motions Inferred from Major Element Chemistry of Lutites[J].Nature,1982,299:715-717.
[33] BOCK B,MCLENNAN S M,HANSON G N.Geochemistry and Provenance of the Middle Ordovician Austin Glen Member(Normanskill Formation)and the Taconian Orogeny in New England[J].Sedimentology,1998,45(4):635-655.
[34] COX R,LOWE D R,CULLERS R L.The Influence of Sediment Recycling and Basement Composition on Evolution of Mudrock Chemistry in the Southwestern United States[J].Geochimica et Cosmochimica Acta,1995,59(14):2919-2940.
[35] MCLENNAN S M.Rare Earth Elements in Sedimentary Rocks:Influence of Provenance and Sedimentary Processes[J].Reviews in Mineralogy and Geochemistry,1989,21(1):169-200.
[36] FRALICK P W,KRONBERG B I.Geochemical Discrimination of Clastic Sedimentary Rock Sources[J].Sedimentary Geology,1997,113(1/2):111-124.
[37] ROSER B P,KORSCH R J.Determination of Tecto-nic Setting of Sandstone-mudstone Suites Using SiO₂ Content and K₂O/Na₂O Ratio[J].The Journal of Geology,1986,94(5):635-650.
[38] CULLERS R L,PODKOVYROV V N.Geochemistry of the Mesoproterozoic Lakhanda Shales in Southeast-ern Yakutia,Russia:Implications for Mineralogical and Provenance Control,and Recycling[J].Precambrian Research,2000,104(1/2):77-93.
[39] 冯连君,储雪蕾,张启锐,等.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,2003,10(4):539-544.
FENG Lian-jun,CHU Xue-lei,ZHANG Qi-rui,et al.CIA(Chemical Index of Alteration)and Its Applications in the Neoproterozoic Clastic Rocks[J].Earth Science Frontiers,2003,10(4):539-544.
[40] FEDO C M,NESBITT H W,YOUNG G M.Unraveling the Effects of Potassium Metasomatism in Sedimentary Rocks and Paleosols,with Implications for Paleoweathering Conditions and Provenance[J].Geo-logy,1995,23(10):921-924.
[41] BHATIA M R.Plate Tectonics and Geochemical Com-position of Sandstones[J].Journal of Geology,1983,91(6):611-627.
[42] 刘春发.赞比亚Chambishi矿区新元古代Roan群沉积作用及其对铜钴成矿的贡献[D].北京:中国地质大学,2019.
LIU Chun-fa.The Sedimentation of the Neoprotero-zoic Roan Group and Its Contribution to the Metallogeny of Copper and Cobalt in Zambia[D].Beijing:China University of Geosciences,2019.
[43] MCLENNAN S M,TAYLOR S R.Sedimentary Ro-cks and Crustal Evolution:Tectonic Setting and Secular Trends[J].The Journal of Geology,1991,99(1):1-21.
[44] MCLENNAN S M,HEMMING S,MCDANIEL D K,et al.Geochemical Approaches to Sedimentation,Pro-venance, and Tectonics[C]∥JOHNSSON M J,BASU A.Processes Controlling the Composition of Clastic Sediments.Washington DC:Geological Society of America,1993:21-40.
[45] FLOYD P A,LEVERIDGE B E.Tectonic Environment of the Devonian Gramscatho Basin,South Cornwall:Framework Mode and Geochemical Evidence from Turbiditic Sandstones[J].Journal of the Geolo-gical Society,1987,144(4):531-542.
[46] 刘奕志,庞崇进,冯佐海,等.桂东北晚震旦世—寒武纪砂岩物源特征:对华南早古生代构造演化的制约[J].大地构造与成矿学,2021,45(4):761-785.
LIU Yi-zhi,PANG Chong-jin,FENG Zuo-hai,et al.Provenance of Late Sinian-Cambrian Sandstones in Northeastern Guangxi:Constraints on Early Paleozoic Tectonic Evolution of South China Block[J].Geotectonica et Metallogenia,2021,45(4):761-785.
[47] 王雅迪,于津海,李晓玲,等.扬子地块与华夏地块的西段界线:来自桂北和桂东新元古界—寒武系沉积岩的证据[J].地质学报,2021,95(6):1712-1726.
WANG Ya-di,YU Jin-hai,LI Xiao-ling,et al.Western Boundary Between the Yangtze and Cathaysia Blocks Constrained by Neoproterozoic to Cambrian Sedimentary Rocks in the Northern and Eastern Guangxi Province,South China[J].Acta Geologica Sinica,2021,95(6):1712-1726.
[48] 李献华,李武显,何 斌.华南陆块的形成与Rodinia超大陆聚合-裂解——观察、解释与检验[J].矿物岩石地球化学通报,2012,31(6):543-559.
LI Xian-hua,LI Wu-xian,HE Bin.Building of the South China Block and Its Relevance to Assembly and Breakup of Rodinia Supercontinent:Observations,Interpretations and Tests[J].Bulletin of Mineralogy,Petrology and Geochemistry,2012,31(6):543-559.
[49] WANG X L,ZHOU J C,GRIFFIN W L,et al.Detrital Zircon Geochronology of Precambrian Basement Sequences in the Jiangnan Orogen:Dating the Assembly of the Yangtze and Cathaysia Blocks[J].Precambrian Research,2007,159(1/2):117-131.
[50] YU J H,O'REILLY S Y,WANG L J,et al.Components and Episodic Growth of Precambrian Crust in the Cathaysia Block,South China:Evidence from U-Pb Ages and Hf Isotopes of Zircons in Neoproterozoic Sediments[J].Precambrian Research,2010,181:97-114.
[51] WANG W,ZHOU M F,YAN D P,et al.Depositional Age,Provenance,and Tectonic Setting of the Neopro-terozoic Sibao Group,Southeastern Yangtze Block,South China[J].Precambrian Research,2012,192/193/194/195:107-124.
[52] SUN J J,SHU L S,SANTOSH M,et al.Precambrian Crustal Evolution of the Central Jiangnan Orogen(South China):Evidence from Detrital Zircon U-Pb Ages and Hf Isotopic Compositions of Neoproterozoic Metasedimentary Rocks[J].Precambrian Research,2018,318:1-24.
[53] 魏震洋,于津海,王丽娟,等.南岭地区新元古代变质沉积岩的地球化学特征及构造意义[J].地球化学,2009,38(1):1-19.
WEI Zhen-yang,YU Jin-hai,WANG Li-juan,et al.Geochemical Features and Tectonic Significances of the Neoproterozoic Metasedimentary Rocks from Nan-ling Range[J].Geochimica,2009,38(1):1-19.
[54] YAN C L,SHU L S,SANTOSH M,et al.The Precambrian Tectonic Evolution of the Western Jiangnan Orogen and Western Cathaysia Block:Evidence from Detrital Zircon Age Spectra and Geochemistry of Cla-stic Rocks[J].Precambrian Research,2015,268:33-60.
[55] WANG K X,SUN L Q,SUN T,et al.Provenance,Weathering Conditions,and Tectonic Evolution History of the Cambrian Meta-sediments in the Zhuguang-shan Area,Cathaysia Block[J].Precambrian Resear-ch,2018,311:195-210.
[56] CONDIE K C.Chemical Composition and Evolution of the Upper Continental Crust:Contrasting Results from Surface Samples and Shales[J].Chemical Geology,1993,104(1/2/3/4):1-37.
[57] LIU C F,QING M,LIU S F,et al.Genesis of Sediment-hosted Stratiform Cu-Co Deposits of the Zambia Copperbelt:Geochemistry and S-Pb Isotopes Constraints from the Chambishi Deposit[J].Geological Journal,2021,56(7):3902-3921.
[58] MURRAY R W,BUCHHOLTZ TEN BRINK M R,JONES D L,et al.Rare Earth Elements as Indicators of Different Marine Depositional Environments in Chert and Shale[J].Geology,1990,18(3):268-271.
[59] BHATIA M R,CROOK K A W.Trace Element Cha-racteristics of Graywackes and Tectonic Setting Discrimination of Sedimentary Basins[J].Contributions to Mineralogy and Petrology,1986,92(2):181-193.
[60] ZHAO G C,CAWOOD P A.Precambrian Geology of China[J].Precambrian Research,2012,222/223:13-54.
[61] 刘宝珺,许效松.中国南方岩相古地理图集[M].北京:科学出版社,1994.
LIU Bao-jun,XU Xiao-song.Lithofacies Paleogeography Atlas of South China[M].Beijing:Science Press,1994.
[62] 王鹏鸣,于津海,孙 涛,等.湘桂震旦—寒武纪沉积岩组成的变化:对华南构造演化的指示[J].中国科学:地球科学,2013,43(11):1893-1906.
WANG Peng-ming,YU Jin-hai,SUN Tao,et al.Composition Variations of the Sinian-Cambrian Sedimentary Rocks in Hunan and Guangxi Provinces and Their Tectonic Significance[J].Science China:Earth Sciences,2013,43(11):1893-1906.
[63] ZHANG C L,SANTOSH M,ZHU Q B,et al.The Gondwana Connection of South China:Evidence from Monazite and Zircon Geochronology in the Cathaysia Block[J].Gondwana Research,2015,28(3):1137-1151.
[64] XUE E K,WANG W,HUANG S F,et al.Detrital Zircon U-Pb-Hf Isotopes and Whole-rock Geochemistry of Neoproterozoic-Cambrian Successions in the Cathaysia Block of South China:Implications on Paleogeographic Reconstruction in Supercontinent[J].Precambrian Research,2019,331:1-18.
[65] 马 筱.黔东及其邻区早古生代构造变形机制及其演化过程[D].北京:中国地质大学,2018.
MA Xiao.The Early Paleozoic Structural Deformation Mechanism and Evolution Proccess in East Guizhou and Its Neighbor Area[D].Beijing:China University of Geosciences,2018.
[66] 王志宏,杨文强,周 岱,等.云开地块东缘寒武系—泥盆系不整合界面上下的碎屑锆石U-Pb年代学记录及对物源转换的响应[J].地球科学,2018,43(11):4193-4203.
WANG Zhi-hong,YANG Wen-qiang,ZHOU Dai,et al.Detrital Zircon U-Pb Geochronological Records and Its Response of Provenance Transformation of Strata Surrounding Cambrian-Devonian Unconformity in Eastern Margin of Yunkai Massif[J].Earth Science,2018,43(11):4193-4203.
[67] 于津海,王丽娟,魏震洋,等.华夏地块显生宙的变质作用期次和特征[J].高校地质学报,2007,13(3):474-483.
YU Jin-hai,WANG Li-juan,WEI Zhen-yang,et al.Phanerozoic Metamorphic Episodes and Characteristics of Cathaysia Block[J].Geological Journal of China Universities,2007,13(3):474-483.
[68] 陈 旭,樊隽轩,陈 清,等.论广西运动的阶段性[J].中国科学:地球科学,2014,44(5):842-850.
CHEN Xu,FAN Jun-xuan,CHEN Qing,et al.Toward a Stepwise Kwangsian Orogeny[J].Science China:Earth Sciences,2014,44(5):842-850.
[69] 贾小辉,王晓地,杨文强.广西大瑶山地区大进早古生代高分异A型花岗岩的厘定及成因[J].地球科学与环境学报,2022,44(2):171-190.
JIA Xiao-hui,WANG Xiao-di,YANG Wen-qiang.Identification and Petrogenesis of Dajin Highly Fractionated A-type Granites Formed at Early Paleozoic in Dayaoshan Area of Guangxi,China[J].Journal of Earth Sciences and Environment,2022,44(2):171-190.

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备注/Memo

备注/Memo:

收稿日期:2021-12-27; 修回日期:2022-03-16投稿网址:http:∥jese.chd.edu.cn/
基金项目:中国黄金集团有限公司项目(WKY201902)
作者简介:刘彦兵(1986-),男,陕西榆林人,高级工程师,E-mail:lyb01305114@163.com。
*通讯作者:刘春发(1985-),男,布依族,贵州独山人,高级工程师,理学博士,博士后,E-mail:lcfjlu704@163.com。

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