皖南志留系唐家坞组物源分析:来自碎屑锆石年代学和岩石地球化学的制约
|
摘要
分布于皖南泾县地区的唐家坞组为志留系顶部最晚沉积,其沉积时代和物质来源仍存在争议。对其进行了岩相学、岩石地球化学以及锆石U-Pb年代学等综合研究。岩相学特征表明:研究砂岩以波状消光的石英和变质岩屑为主,磨圆度和分选程度较好;岩石地球化学特征显示砂岩的成分成熟度较高,物源区主要以长英质组分为主,并发生了强烈的化学风化或沉积循环;LA-ICP-MS锆石U-Pb测年获得最年轻的单颗粒锆石年龄为424 Ma,可作为唐家坞组沉积时代的下限。结合地层接触关系,限定唐家坞组沉积时代应为志留纪晚期,可能接近华南早古生代造山事件的结束时间。79颗碎屑锆石U-Pb年龄获得主要年龄峰值为981 Ma和756 Ma,次级年龄峰值为2 476 Ma、517 Ma和453 Ma,结合区域上年代学信息,暗示了唐家坞组砂岩的主要物源区为早—中新元古代岩浆岩、新元古代裂谷层序以及震旦纪—奥陶纪沉积岩,同造山期岩浆岩或变质岩也为唐家坞组提供了物源。华南早古生代陆内造山作用导致中奥陶世之前的盆地沉积物、部分盆地基底以及造山期侵入其中的岩浆岩发生强烈的隆升,从而为陆内前陆盆地沉积提供了主要物源,表明华南早古生代造山带与扬子地块东南缘前陆盆地两个构造单元存在盆山物质耦合关系。
Provenance and sedimentary age are still debated about Tangjiawu Formation from the South Anhui. The study focused on the petrography,geochemical features and detrital zircon ages of the sandstones in the Tangjiawu Formation. The sandstones,which are highly rounded and sorted,are essentially composed of metamorphic detritus and quartz with wave extinction. They exhibited relatively high compositional maturity. Their provenances were dominated by felsic materials that had undergone intensive chemical weathering or sedimentary recycling. LA-ICP-MS zircon UPb dating yields a youngest age of 424 Ma,which represents the lower limit of deposition age. In addition to the zircon ages,the Tangjiawu Formation uncomfortably overlain by the Devonian Guanshan Formation,suggesting that it should be deposited in Late Silurian that approached to the termination timing of the early Palaeozoic orogenic event. Seventynine detrital zircons with discordance <10% display a broadly age spectrum of 2 912 Ma to 424 Ma. Most of the detrital zircons have U-Pb age grouped between 731 and 1 031 Ma,with two clusters peaking at 981 and 756 Ma. A few populations with peak ages of 2 476 Ma,517 Ma and 453 Ma are present as well. This suggested that the provenances of the Tangjiawu Formation were mainly derived from the early-to middle-Neoproterozoic igneous rocks,Late Neoproterozoic rift sequence and Sinian to Ordovician sediments with subordinate synorogenic magmatic or sedimentary rocks.The early Palaeozoic intra-continental orogeny caused the uplifting of the sediments in the pre-middle-Ordovician basins,which mostly contributed to sources of the deposits in the intra-continental foreland basin. The deposition and evolution of the foreland basin in the South China were controlled by the early Palaeozoic orogeny,reflecting the coupled material recycling between the orogen and the foreland basin.
Provenance and sedimentary age are still debated about Tangjiawu Formation from the South Anhui. The study focused on the petrography,geochemical features and detrital zircon ages of the sandstones in the Tangjiawu Formation. The sandstones,which are highly rounded and sorted,are essentially composed of metamorphic detritus and quartz with wave extinction. They exhibited relatively high compositional maturity. Their provenances were dominated by felsic materials that had undergone intensive chemical weathering or sedimentary recycling. LA-ICP-MS zircon UPb dating yields a youngest age of 424 Ma,which represents the lower limit of deposition age. In addition to the zircon ages,the Tangjiawu Formation uncomfortably overlain by the Devonian Guanshan Formation,suggesting that it should be deposited in Late Silurian that approached to the termination timing of the early Palaeozoic orogenic event. Seventynine detrital zircons with discordance <10% display a broadly age spectrum of 2 912 Ma to 424 Ma. Most of the detrital zircons have U-Pb age grouped between 731 and 1 031 Ma,with two clusters peaking at 981 and 756 Ma. A few populations with peak ages of 2 476 Ma,517 Ma and 453 Ma are present as well. This suggested that the provenances of the Tangjiawu Formation were mainly derived from the early-to middle-Neoproterozoic igneous rocks,Late Neoproterozoic rift sequence and Sinian to Ordovician sediments with subordinate synorogenic magmatic or sedimentary rocks.The early Palaeozoic intra-continental orogeny caused the uplifting of the sediments in the pre-middle-Ordovician basins,which mostly contributed to sources of the deposits in the intra-continental foreland basin. The deposition and evolution of the foreland basin in the South China were controlled by the early Palaeozoic orogeny,reflecting the coupled material recycling between the orogen and the foreland basin.
引文
[1]Wang J,Li Z X.Sequence stratigraphy and evolution of the Neoproterozoic marginal basins along southeastern Yangtze Craton,South China[J].Gondwana Research,2001,4(1):17-26.
[2]Wang J,Li Z X.History of Neoproterozoic rift basins in South China:implications for Rodinia break-up[J].Precambrian Research,2003,122(1/2/3/4):141-158.
[3]郭令智,施央申,马瑞士.华南大地构造格架和地壳演化[C]//国际交流地质学术论文集(一).北京:地质出版社,1980:109-116.[Guo Lingzhi,Shi Yangshen,Ma Ruishi.Geotectonic framework and crust evolution of South China[C].Beijing:Geological Publishing House,1980:109-116.]
[4]郭令智,施央申,马瑞士,等.中国东南部地体构造的研究[J].南京大学学报(自然科学),1984,20(4):732-739.[Guo Lingzhi,Shi Yangshen,Ma Ruishi,et al.Tectonostratigraphic terranes of southeast China[J].Journal of Nanjing University(Natural Sciences),1984,20(4):732-739.]
[5]郭令智,舒良树,卢华复,等.中国地体构造研究进展综述[J].南京大学学报(自然科学),2000,36(1):1-17.[Guo Lingzhi,Shu Liangshu,Lu Huafu,et al.A synthetical review on research advances on the terrane tectonics in China[J].Journal of Nanjing University(Natural Sciences),2000,36(1):1-17.]
[6]王鹤年,周丽娅.华南地质构造的再认识[J].高校地质学报,2006,12(4):457-465.[Wang Henian,Zhou Liya.A further understanding in geological structure of South China[J].Geological Journal of China Universities,2006,12(4):457-465.]
[7]Charvet J,Shu Liangshu,Faure M,et al.Structural development of the Lower Paleozoic belt of South China:genesis of an intracontinental orogen[J].Journal of Asian Earth Sciences,2010,39(4):309-330.
[8]Li Zhengxiang,Li Xianhua,Wartho J A,et al.Magmatic and metamorphic events during the early Paleozoic Wuyi-Yunkai orogeny,southeastern South China:new age constraints and pressure-temperature conditions[J].Geological Society of America Bulletin,2010,122(5/6):772-793.
[9]李三忠,李玺瑶,赵淑娟,等.全球早古生代造山带(Ⅲ):华南陆内造山[J].吉林大学学报(地球科学版),2016,46(4):1005-1025.[Li Sanzhong,Li Xiyao,Zhao Shujuan,et al.Global early Paleozoic orogens(Ⅲ)intracontinental orogen in South China[J].Journal of Jilin University(Earth Science Edition),2016,46(4):1005-1025.]
[10]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,1994:10-11.[Liu Baojun,Xu Xiaosong.Atlas of Lithofacies and palegeography of south of China[M].Beijing:Science Press,1994:10-11.]
[11]舒良树,于津海,贾东,等.华南东段早古生代造山带研究[J].地质通报,2008,27(10):1581-1593.[Shu Liangshu,Yu Jinhai,Jia Dong,et al.Early Paleozoic Orogenic belt in the eastern segment of South China[J].Geological Bulletin of China,2008,27(10):1581-1593.]
[12]Yao W H,Li Z X.Tectonostratigraphic history of the Ediacaran-Silurian Nanhua foreland basin in South China[J].Tectonophysics,2016,674:31-51.
[13]Tucker R T,Roberts E M,Hu Yi,et al.Detrital zircon age constraints for the Winton Formation,Queensland:contextualizing Australia's Late Cretaceous dinosaur faunas[J].Gondwana Research,2013,24(2):767-779.
[14]Nelson D R.An assessment of the determination of depositional ages for Precambrian clastic sedimentary rocks by U-Pb dating of detrital zircons[J].Sedimentary Geology,2001,141-142:37-60.
[15]Dickinson W R,Gehrels G E.Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata:a test against a Colorado Plateau Mesozoic database[J].Earth and Planetary Science Letters,2009,288(1):115-125.
[16]段太忠,曾允孚,高振中.根据沉积历史分析华南古大陆边缘的构造演化[J].石油与天然气地质,1988,9(4):410-420.[Duan Taizhong,Zeng Yunfu,Gao Zhenzhong.Analysis of tectonic evolution of Paleo-continental margin in South China[J].Oil&Gas Geology,1988,9(4):410-420.]
[17]王剑,刘宝珺,潘桂棠.华南新元古代裂谷盆地演化-Rodinia超大陆解体的前奏[J].矿物岩石,2001,21(3):135-145.[Wang Jian,Liu Baojun,Pan Guitang.Neoproterozoic rifting history of South China significance to Rodinia breakup[J].Journal of Mineralogy and Petrology,2001,21(3):135-145.]
[18]任纪舜,李崇.华夏古陆及相关问题—中国南部前泥盆纪大地构造[J].地质学报,2016,90(4):607-614.[Ren Jishun,Li Chong.Cathaysia old land and relevant problems:pre-Devonian tectonics of southern China[J].Acta Geologica Sinica,2016,90(4):607-614.]
[19]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(D辑):地球科学,2013,43(10):1553-1582.[Zhang Guowei,Guo Anlin,Wang Yuejun,et al.Tectonics of South China continent and its implications[J].Science China(Seri.D):Earth Sciences,2013,43(10):1553-1582.]
[20]耿元生,沈其韩,杜利林,等.区域变质作用与中国大陆地壳的形成与演化[J].岩石学报,2016,32(9):2579-2608.[Geng Yuansheng,Shen Qihan,Du Lilin,et al.Regional metamorphism and continental growth and assembly in China[J].Acta Petrologica Sinica,2016,32(9):2579-2608.]
[21]Li H B,Jia D,Wu L,et al.Detrital zircon provenance of the Lower Yangtze foreland basin deposits:constraints on the evolution of the early Palaeozoic Wuyi-Yunkai orogenic belt in South China[J].Geological Magazine,2013,150(6):959-974.
[22]Ludwig K R.User’s Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel[M].Berkeley:Berkeley Geochronology Center Special Publication,2003(4):1-70.
[23]Andersen T.Correction of common lead in U-Pb analyses that do not report204Pb[J].Chemical Geology,2002,192(1/2):59-79.
[24]Black L P,Kamo S L,Williams I S,et al.The application of SHRIMP to Phanerozoic geochronology:a critical appraisal of four zircon standards[J].Chemical Geology,2003,200(1/2):171-188.
[25]Ronov A B,Yaroshevskiy A A,Migdisov A A,et al.Chemical constitution of the Earth's crust and geochemical balance of the major elements[J].International Geology Review,1991,33(10):941-1048.
[26]Taylor S R,Mc Lennan S M.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell,1985:1-312.
[27]Herron M M.Geochemical classification of terrigenous sands and shales from core or log data[J].Journal of Sedimentary Research,1988,58(5):820-829.
[28]Mc Lennan S M,Hemming S R,Taylor S R,et al.Early Proterozoic crustal evolution:geochemical and Nd-Pb isotopic evidence from metasedimentary rocks,southwestern North America[J].Geochimica et Cosmochimica Acta,1995,59(6):1153-1177.
[29]Boynton W V.Cosmochemistry of the rare earth elements:meteorite studies[J].Developments in Geochemistry,1984,2(2):63-114.
[30]Sun S S,Mac Donough W F.Chemical and isotopic systematics of oceanic basalts;implications for mantle composition and processes[J].Geological Society,London,Special Publications,1989,42(1):313-345.
[31]安徽省地质矿产局.安徽省岩石地层[M].武汉:中国地质大学出版社,1997:126-165.[Bureau of Geology and Mineral Resource of Anhui Province.Multiple classification and correlation on the stratigraphy of China(34):stratigraphy(lithostratic)of Anhui province[M].Wuhan:China University of Geoscience Press,1997:126-165.]
[32]夏树芳.苏南、浙北、皖南地区志留系与泥盆系的分界问题[J].地层学杂志,1978,2(2):152-159.[Xia Shufang.The Silurian and Devonian boundary in south Jiangsu,north Zhejiang and south Anhui[J].Journal of Stratigraphy,1978,2(2):152-159.]
[33]安徽省地质矿产局区域地质调查队.安徽省岩相古地理图册[M].合肥:安徽科学技术出版社,1990:129-133.[Regional Geological Surveying Party,Bureau of Geology and Mineral Resource of Anhui Province.The lithofacies paleogeographic atlas of Anhui province[M].Hefei:Anhui Publishing House of Science and Technology,1990:129-133.]
[34]安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社,1987:1-721.[Bureau of Geology and Mineral Resource of Anhui Province.Regional geology of Anhui province[M].Beijing:Geological Publishing House,1987:1-721.]
[35]方晓思,何胜策.浙西唐家坞组的微古植物及其时代[J].地质论评,1988,34(4):327-333.[Fang Xiaosi,He Shengce.The microflora of the Tangjiawu Formation in western Zhejiang province and its chronologic significance[J].Geological Review,1988,34(4):327-333.]
[36]颜铁增.杭州地区唐家坞组、西湖组的微古植物组合特征及其时代[J].浙江地质,1991,7(2):28-33.[Yan Tiezeng.The microflora assemblages character and their age of Tangjiawu and Xihu Formations in Hangzhou region,Zhejiang province[J].Geology of Zhejiang,1991,7(2):28-33.]
[37]颜铁增.浙江唐家坞组西湖组的微古植物及其地层划分对比[J].中国区域地质,1992(2):111-117.[Yan Tiezeng.The microflora of Tangjiawu and Xihu Formations in Zhejiang and their stratigraphical division and correlation[J].Regional Geology of China,1992(2):111-117.]
[38]颜铁增,何圣策,尹磊明,等.浙江早古生代孢粉型化石的研究[J].地层学杂志,2011,35(1):19-30.[Yan Tiezeng,He Shengce,Yin Leiming,et al.Early Paleozoic palynomorphs of Zhejiang province,China[J].Journal of Stratigraphy,2011,35(1):19-30.]
[39]孙乘云,杜森官,王有生.安徽省黄山地区唐家坞组生物地层[J].地层学杂志,2008,32(3):290-293.[Sun Chengyun,Du Senguan,Wang Yousheng.Biostratigraphy of the Tangjiawu Formation in the Huangshan area,Anhui province[J].Journal of Stratigraphy,2008,32(3):290-293.]
[40]戎嘉余,陈旭.中国志留纪年代地层学述评[J].地层学杂志,2000,24(1):27-35.[Rong Jiayu,Chen Xu.Comments on Silurian chronostratigraphy of China[J].Journal of Stratigraphy,2000,24(1):27-35.]
[41]吴跃东,江来利.皖西南地区泥盆纪─三叠纪层序地层[J].成都理工大学学报(自然科学版),2009,36(1):19-28.[Wu Yaodong,Jiang Laili.Sequence stratigraphy of the Devonian-Triassic strata in Southwest Anhui,China[J].Journal of Chengdu University of Technology(Science&Technology Edition),2009,36(1):19-28.]
[42]李海滨.下扬子地区早古生代前陆盆地与油气前景分析[D].南京:南京大学,2013.[Li Haibin.Analyses of the early Paleozoic foreland basin and hydrocarbon prospect in the lower Yangtze region[D].Nanjing:Nanjing University,2013.]
[43]Mc Lennan S M,Hemming S,Mcdaniel D K,et al.Geochemical approaches to sedimentation,provenance,and tectonics[J].Special Paper of the Geological Society of America,1993,284:21-40.
[44]Naqvi S M,Sawkar R H,Rao D V S,et al.Geology,geochemistry and tectonic setting of Archaean greywackes from Karnataka nucleus,India[J].Precambrian Research,1988,39(3):193-216.
[45]Wronkiewicz D J,Condie K C.Geochemistry and mineralogy of sediments from the Ventersdorp and Transvaal Supergroups,South Africa:cratonic evolution during the early Proterozoic[J].Geochimica et Cosmochimica Acta,1990,54(2):343-354.
[46]Cullers R L.The geochemistry of shales,siltstones and sandstones of Pennsylvanian-Permian age,Colorado,USA:implications for provenance and metamorphic studies[J].Lithos,2000,51(3):181-203.
[47]Nesbitt H W,Young G M.Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J].Geochimica et Cosmochimica Acta,1984,48(7):1523-1534.
[48]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].Geology,1995,23(10):921-924.
[49]Panahi A,Young G M,Rainbird R H.Behavior of major and trace elements(including REE)during Paleoproterozoic pedogenesis and diagenetic alteration of an Archean granite near Ville Marie,Québec,Canada[J].Geochimica et Cosmochimica Acta,2000,64(13):2199-2220.
[50]Roser B P,Korsch R J.Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data[J].Chemical Geology,1988,67(1/2):119-139.
[51]Bhatia M R,Crook K A W.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J].Contributions to Mineralogy and Petrology,1986,92(2):181-193.
[52]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 Geological Society,1987,144(4):531-542.
[53]Dickinson W R,Beard L S,Brakenridge G R,et al.Provenance of North American Phanerozoic sandstones in relation to tectonic setting[J].Geological Society of America Bulletin,1983,94(2):222-235.
[54]Mc Lennan S M.Rare earth elements and sedimentary rocks:influence of provenance and sedimentary processes[J].Reviews in Mineralogy and Geochemistry,1989,21(8):169-200.
[55]陈小勇,陈国华,舒立旻,等.江南东段华夏与扬子陆块碰撞时间的研究[J].新疆地质,2015,33(4):520-528.[Chen Xiaoyong,Chen Guohua,Shu Limin,et al.A study of the collision timing of Yangtze and Cathaysia Blocks in the Eastern Jiangnan Orogenic Belt,South China[J].Xinjiang Geology,2015,33(4):520-528.]
[56]Wu L,Jia D,Li H B,et al.Provenance of detrital zircons from the late Neoproterozoic to Ordovician sandstones of South China:implications for its continental affinity[J].Geological Magazine,2010,147(6):974-980.
[57]Wang W,Zhou M F,Yan D P,et al.Depositional age,provenance,and tectonic setting of the Neoproterozoic Sibao Group,southeastern Yangtze Block,South China[J].Precambrian Research,2012,192-195:107-124.
[58]刘邦秀,刘春根,邱永泉.江西南部鹤仔片麻状花岗岩类Pb-Pb同位素年龄及地质意义[J].火山地质与矿产,2001,22(4):264-268.[Liu Bangxiu,Liu Chungen,Qiu Yongquan.The Pb-Pb isotopic ages and geologic significance of gneissic granite in Hezi,Jiangxi[J].Volcanology&Mineral Resources,2001,22(4):264-268.]
[59]陈志洪,郭坤一,董永观,等.江山—绍兴拼合带平水段可能存在新元古代早期板片窗岩浆活动:来自锆石LA-ICP-MS年代学和地球化学的证据[J].中国科学(D辑):地球科学,2009,39(7):994-1008.[Chen Zhihong,Guo Kunyi,Dong Yongguan,et al.Possible early Neoproterozoic magmatism associated with slab window in the Pingshui segment of the Jiangshan-Shaoxing suture zone:Evidence from zircon LA-ICP-MS U-Pb geochronology and geochemistry[J].Science China(Seri.D):Earth Sciences,2009,39(7):994-1008.]
[60]Li Z X,Bogdanova S V,Collins A S,et al.Assembly,configuration,and break-up history of Rodinia:a synthesis[J].Precambrian Research,2008,160(1/2):179-210.
[61]Sun W H,Zhou M F,Gao J F,et al.Detrital zircon U-Pb geochronological and Lu-Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze Block,SW China[J].Precambrian Research,2009,172(1/2):99-126.
[62]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.
[63]向磊,舒良树.华南东段前泥盆纪构造演化:来自碎屑锆石的证据[J].中国科学(D辑):地球科学,2010,40(10):1377-1388.[Xiang Lei,Shu Liangshu.Pre-Devonian tectonic evolution of the eastern South China Block:Geochronological evidence from detrital zircons[J].Science China(Seri.D):Earth Sciences,2010,40(10):1377-1388.]
[64]徐先兵,张岳桥,舒良树,等.武夷山地区前寒武纪地层沉积时代研究[J].地层学杂志,2010,34(3):254-267.[Xu Xianbing,Zhang Yueqiao,Shu Liangshu,et al.Precambrian geochronology and stratigraphy in the Wuyishan area,South China[J].Journal of Stratigraphy,2010,34(3):254-267.]
[65]Yao J L,Shu L S,Santosh M.Detrital zircon U-Pb geochronology,Hf-isotopes and geochemistry-new clues for the Precambrian crustal evolution of Cathaysia Block,South China[J].Gondwana Research,2011,20(2/3):553-567.
[66]Yao W H,Li Z X,Li W X,et al.From Rodinia to gondwanaland:a tale of detrital zircon provenance analyses from the southern Nanhua Basin,South China[J].American Journal of Science,2014,314(1):278-313.
[67]Yao W H,Li Z X,Li W X,et al.Detrital provenance evolution of the Ediacaran-Silurian Nanhua foreland basin,South China[J].Gondwana Research,2015,28(4):1449-1465.
[68]张芳荣,舒良树,王德滋,等.华南东段加里东期花岗岩类形成构造背景探讨[J].地学前缘,2009,16(1):248-260.[Zhang Fangrong,Shu Liangshu,Wang Dezi,et al.Discussions on the tectonic setting of Caledonian granitoids in the eastern segment of South China[J].Earth Science Frontiers,2009,16(1):248-260.]
[69]胡艳华,顾明光,徐岩,等.浙江诸暨地区陈蔡群加里东期变质年龄的确认及其地质意义[J].地质通报,2011,30(11):1661-1670.[Hu Yanhua,Gu Mingguang,Xu Yan,et al.The confirmation of the age of Caledonian Chencai Group in Zhuji area of Zhejiang province and its geological significance[J].Geological Bulletin of China,2011,30(11):1661-1670.]
[70]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.
[71]龚根辉.华南早古生代前陆盆地沉积与构造演化[D].杭州:浙江大学,2015.[Gong Genhui.Sedimentary and tectonic evolution of the early Paleozoic foreland basin in the South China Block[D].Hangzhou:Zhejiang University,2015.]
[72]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 Liangshu.An analysis of principal features of tectonic evolution in South China Block[J].Geological Bulletin of China,2012,31(7):1035-1053.]
[73]Xu Y J,Du Y S,Cawood P A,et al.Detrital zircon provenance of upper Ordovician and Silurian Strata in the northeastern Yangtze Block:response to orogenesis in South China[J].Sedimentary Geology,2012,267-268:63-72.
[74]Wang Y J,Zhang F F,Fan W M,et al.Tectonic setting of the South China Block in the early Paleozoic:resolving intracontinental and ocean closure models from detrital zircon U-Pb geochronology[J].Tectonics,2010,29(6):TC6020,doi:10.1029/2010TC002750.
[2]Wang J,Li Z X.History of Neoproterozoic rift basins in South China:implications for Rodinia break-up[J].Precambrian Research,2003,122(1/2/3/4):141-158.
[3]郭令智,施央申,马瑞士.华南大地构造格架和地壳演化[C]//国际交流地质学术论文集(一).北京:地质出版社,1980:109-116.[Guo Lingzhi,Shi Yangshen,Ma Ruishi.Geotectonic framework and crust evolution of South China[C].Beijing:Geological Publishing House,1980:109-116.]
[4]郭令智,施央申,马瑞士,等.中国东南部地体构造的研究[J].南京大学学报(自然科学),1984,20(4):732-739.[Guo Lingzhi,Shi Yangshen,Ma Ruishi,et al.Tectonostratigraphic terranes of southeast China[J].Journal of Nanjing University(Natural Sciences),1984,20(4):732-739.]
[5]郭令智,舒良树,卢华复,等.中国地体构造研究进展综述[J].南京大学学报(自然科学),2000,36(1):1-17.[Guo Lingzhi,Shu Liangshu,Lu Huafu,et al.A synthetical review on research advances on the terrane tectonics in China[J].Journal of Nanjing University(Natural Sciences),2000,36(1):1-17.]
[6]王鹤年,周丽娅.华南地质构造的再认识[J].高校地质学报,2006,12(4):457-465.[Wang Henian,Zhou Liya.A further understanding in geological structure of South China[J].Geological Journal of China Universities,2006,12(4):457-465.]
[7]Charvet J,Shu Liangshu,Faure M,et al.Structural development of the Lower Paleozoic belt of South China:genesis of an intracontinental orogen[J].Journal of Asian Earth Sciences,2010,39(4):309-330.
[8]Li Zhengxiang,Li Xianhua,Wartho J A,et al.Magmatic and metamorphic events during the early Paleozoic Wuyi-Yunkai orogeny,southeastern South China:new age constraints and pressure-temperature conditions[J].Geological Society of America Bulletin,2010,122(5/6):772-793.
[9]李三忠,李玺瑶,赵淑娟,等.全球早古生代造山带(Ⅲ):华南陆内造山[J].吉林大学学报(地球科学版),2016,46(4):1005-1025.[Li Sanzhong,Li Xiyao,Zhao Shujuan,et al.Global early Paleozoic orogens(Ⅲ)intracontinental orogen in South China[J].Journal of Jilin University(Earth Science Edition),2016,46(4):1005-1025.]
[10]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,1994:10-11.[Liu Baojun,Xu Xiaosong.Atlas of Lithofacies and palegeography of south of China[M].Beijing:Science Press,1994:10-11.]
[11]舒良树,于津海,贾东,等.华南东段早古生代造山带研究[J].地质通报,2008,27(10):1581-1593.[Shu Liangshu,Yu Jinhai,Jia Dong,et al.Early Paleozoic Orogenic belt in the eastern segment of South China[J].Geological Bulletin of China,2008,27(10):1581-1593.]
[12]Yao W H,Li Z X.Tectonostratigraphic history of the Ediacaran-Silurian Nanhua foreland basin in South China[J].Tectonophysics,2016,674:31-51.
[13]Tucker R T,Roberts E M,Hu Yi,et al.Detrital zircon age constraints for the Winton Formation,Queensland:contextualizing Australia's Late Cretaceous dinosaur faunas[J].Gondwana Research,2013,24(2):767-779.
[14]Nelson D R.An assessment of the determination of depositional ages for Precambrian clastic sedimentary rocks by U-Pb dating of detrital zircons[J].Sedimentary Geology,2001,141-142:37-60.
[15]Dickinson W R,Gehrels G E.Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata:a test against a Colorado Plateau Mesozoic database[J].Earth and Planetary Science Letters,2009,288(1):115-125.
[16]段太忠,曾允孚,高振中.根据沉积历史分析华南古大陆边缘的构造演化[J].石油与天然气地质,1988,9(4):410-420.[Duan Taizhong,Zeng Yunfu,Gao Zhenzhong.Analysis of tectonic evolution of Paleo-continental margin in South China[J].Oil&Gas Geology,1988,9(4):410-420.]
[17]王剑,刘宝珺,潘桂棠.华南新元古代裂谷盆地演化-Rodinia超大陆解体的前奏[J].矿物岩石,2001,21(3):135-145.[Wang Jian,Liu Baojun,Pan Guitang.Neoproterozoic rifting history of South China significance to Rodinia breakup[J].Journal of Mineralogy and Petrology,2001,21(3):135-145.]
[18]任纪舜,李崇.华夏古陆及相关问题—中国南部前泥盆纪大地构造[J].地质学报,2016,90(4):607-614.[Ren Jishun,Li Chong.Cathaysia old land and relevant problems:pre-Devonian tectonics of southern China[J].Acta Geologica Sinica,2016,90(4):607-614.]
[19]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(D辑):地球科学,2013,43(10):1553-1582.[Zhang Guowei,Guo Anlin,Wang Yuejun,et al.Tectonics of South China continent and its implications[J].Science China(Seri.D):Earth Sciences,2013,43(10):1553-1582.]
[20]耿元生,沈其韩,杜利林,等.区域变质作用与中国大陆地壳的形成与演化[J].岩石学报,2016,32(9):2579-2608.[Geng Yuansheng,Shen Qihan,Du Lilin,et al.Regional metamorphism and continental growth and assembly in China[J].Acta Petrologica Sinica,2016,32(9):2579-2608.]
[21]Li H B,Jia D,Wu L,et al.Detrital zircon provenance of the Lower Yangtze foreland basin deposits:constraints on the evolution of the early Palaeozoic Wuyi-Yunkai orogenic belt in South China[J].Geological Magazine,2013,150(6):959-974.
[22]Ludwig K R.User’s Manual for Isoplot 3.00:A Geochronological Toolkit for Microsoft Excel[M].Berkeley:Berkeley Geochronology Center Special Publication,2003(4):1-70.
[23]Andersen T.Correction of common lead in U-Pb analyses that do not report204Pb[J].Chemical Geology,2002,192(1/2):59-79.
[24]Black L P,Kamo S L,Williams I S,et al.The application of SHRIMP to Phanerozoic geochronology:a critical appraisal of four zircon standards[J].Chemical Geology,2003,200(1/2):171-188.
[25]Ronov A B,Yaroshevskiy A A,Migdisov A A,et al.Chemical constitution of the Earth's crust and geochemical balance of the major elements[J].International Geology Review,1991,33(10):941-1048.
[26]Taylor S R,Mc Lennan S M.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell,1985:1-312.
[27]Herron M M.Geochemical classification of terrigenous sands and shales from core or log data[J].Journal of Sedimentary Research,1988,58(5):820-829.
[28]Mc Lennan S M,Hemming S R,Taylor S R,et al.Early Proterozoic crustal evolution:geochemical and Nd-Pb isotopic evidence from metasedimentary rocks,southwestern North America[J].Geochimica et Cosmochimica Acta,1995,59(6):1153-1177.
[29]Boynton W V.Cosmochemistry of the rare earth elements:meteorite studies[J].Developments in Geochemistry,1984,2(2):63-114.
[30]Sun S S,Mac Donough W F.Chemical and isotopic systematics of oceanic basalts;implications for mantle composition and processes[J].Geological Society,London,Special Publications,1989,42(1):313-345.
[31]安徽省地质矿产局.安徽省岩石地层[M].武汉:中国地质大学出版社,1997:126-165.[Bureau of Geology and Mineral Resource of Anhui Province.Multiple classification and correlation on the stratigraphy of China(34):stratigraphy(lithostratic)of Anhui province[M].Wuhan:China University of Geoscience Press,1997:126-165.]
[32]夏树芳.苏南、浙北、皖南地区志留系与泥盆系的分界问题[J].地层学杂志,1978,2(2):152-159.[Xia Shufang.The Silurian and Devonian boundary in south Jiangsu,north Zhejiang and south Anhui[J].Journal of Stratigraphy,1978,2(2):152-159.]
[33]安徽省地质矿产局区域地质调查队.安徽省岩相古地理图册[M].合肥:安徽科学技术出版社,1990:129-133.[Regional Geological Surveying Party,Bureau of Geology and Mineral Resource of Anhui Province.The lithofacies paleogeographic atlas of Anhui province[M].Hefei:Anhui Publishing House of Science and Technology,1990:129-133.]
[34]安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社,1987:1-721.[Bureau of Geology and Mineral Resource of Anhui Province.Regional geology of Anhui province[M].Beijing:Geological Publishing House,1987:1-721.]
[35]方晓思,何胜策.浙西唐家坞组的微古植物及其时代[J].地质论评,1988,34(4):327-333.[Fang Xiaosi,He Shengce.The microflora of the Tangjiawu Formation in western Zhejiang province and its chronologic significance[J].Geological Review,1988,34(4):327-333.]
[36]颜铁增.杭州地区唐家坞组、西湖组的微古植物组合特征及其时代[J].浙江地质,1991,7(2):28-33.[Yan Tiezeng.The microflora assemblages character and their age of Tangjiawu and Xihu Formations in Hangzhou region,Zhejiang province[J].Geology of Zhejiang,1991,7(2):28-33.]
[37]颜铁增.浙江唐家坞组西湖组的微古植物及其地层划分对比[J].中国区域地质,1992(2):111-117.[Yan Tiezeng.The microflora of Tangjiawu and Xihu Formations in Zhejiang and their stratigraphical division and correlation[J].Regional Geology of China,1992(2):111-117.]
[38]颜铁增,何圣策,尹磊明,等.浙江早古生代孢粉型化石的研究[J].地层学杂志,2011,35(1):19-30.[Yan Tiezeng,He Shengce,Yin Leiming,et al.Early Paleozoic palynomorphs of Zhejiang province,China[J].Journal of Stratigraphy,2011,35(1):19-30.]
[39]孙乘云,杜森官,王有生.安徽省黄山地区唐家坞组生物地层[J].地层学杂志,2008,32(3):290-293.[Sun Chengyun,Du Senguan,Wang Yousheng.Biostratigraphy of the Tangjiawu Formation in the Huangshan area,Anhui province[J].Journal of Stratigraphy,2008,32(3):290-293.]
[40]戎嘉余,陈旭.中国志留纪年代地层学述评[J].地层学杂志,2000,24(1):27-35.[Rong Jiayu,Chen Xu.Comments on Silurian chronostratigraphy of China[J].Journal of Stratigraphy,2000,24(1):27-35.]
[41]吴跃东,江来利.皖西南地区泥盆纪─三叠纪层序地层[J].成都理工大学学报(自然科学版),2009,36(1):19-28.[Wu Yaodong,Jiang Laili.Sequence stratigraphy of the Devonian-Triassic strata in Southwest Anhui,China[J].Journal of Chengdu University of Technology(Science&Technology Edition),2009,36(1):19-28.]
[42]李海滨.下扬子地区早古生代前陆盆地与油气前景分析[D].南京:南京大学,2013.[Li Haibin.Analyses of the early Paleozoic foreland basin and hydrocarbon prospect in the lower Yangtze region[D].Nanjing:Nanjing University,2013.]
[43]Mc Lennan S M,Hemming S,Mcdaniel D K,et al.Geochemical approaches to sedimentation,provenance,and tectonics[J].Special Paper of the Geological Society of America,1993,284:21-40.
[44]Naqvi S M,Sawkar R H,Rao D V S,et al.Geology,geochemistry and tectonic setting of Archaean greywackes from Karnataka nucleus,India[J].Precambrian Research,1988,39(3):193-216.
[45]Wronkiewicz D J,Condie K C.Geochemistry and mineralogy of sediments from the Ventersdorp and Transvaal Supergroups,South Africa:cratonic evolution during the early Proterozoic[J].Geochimica et Cosmochimica Acta,1990,54(2):343-354.
[46]Cullers R L.The geochemistry of shales,siltstones and sandstones of Pennsylvanian-Permian age,Colorado,USA:implications for provenance and metamorphic studies[J].Lithos,2000,51(3):181-203.
[47]Nesbitt H W,Young G M.Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J].Geochimica et Cosmochimica Acta,1984,48(7):1523-1534.
[48]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].Geology,1995,23(10):921-924.
[49]Panahi A,Young G M,Rainbird R H.Behavior of major and trace elements(including REE)during Paleoproterozoic pedogenesis and diagenetic alteration of an Archean granite near Ville Marie,Québec,Canada[J].Geochimica et Cosmochimica Acta,2000,64(13):2199-2220.
[50]Roser B P,Korsch R J.Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data[J].Chemical Geology,1988,67(1/2):119-139.
[51]Bhatia M R,Crook K A W.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J].Contributions to Mineralogy and Petrology,1986,92(2):181-193.
[52]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 Geological Society,1987,144(4):531-542.
[53]Dickinson W R,Beard L S,Brakenridge G R,et al.Provenance of North American Phanerozoic sandstones in relation to tectonic setting[J].Geological Society of America Bulletin,1983,94(2):222-235.
[54]Mc Lennan S M.Rare earth elements and sedimentary rocks:influence of provenance and sedimentary processes[J].Reviews in Mineralogy and Geochemistry,1989,21(8):169-200.
[55]陈小勇,陈国华,舒立旻,等.江南东段华夏与扬子陆块碰撞时间的研究[J].新疆地质,2015,33(4):520-528.[Chen Xiaoyong,Chen Guohua,Shu Limin,et al.A study of the collision timing of Yangtze and Cathaysia Blocks in the Eastern Jiangnan Orogenic Belt,South China[J].Xinjiang Geology,2015,33(4):520-528.]
[56]Wu L,Jia D,Li H B,et al.Provenance of detrital zircons from the late Neoproterozoic to Ordovician sandstones of South China:implications for its continental affinity[J].Geological Magazine,2010,147(6):974-980.
[57]Wang W,Zhou M F,Yan D P,et al.Depositional age,provenance,and tectonic setting of the Neoproterozoic Sibao Group,southeastern Yangtze Block,South China[J].Precambrian Research,2012,192-195:107-124.
[58]刘邦秀,刘春根,邱永泉.江西南部鹤仔片麻状花岗岩类Pb-Pb同位素年龄及地质意义[J].火山地质与矿产,2001,22(4):264-268.[Liu Bangxiu,Liu Chungen,Qiu Yongquan.The Pb-Pb isotopic ages and geologic significance of gneissic granite in Hezi,Jiangxi[J].Volcanology&Mineral Resources,2001,22(4):264-268.]
[59]陈志洪,郭坤一,董永观,等.江山—绍兴拼合带平水段可能存在新元古代早期板片窗岩浆活动:来自锆石LA-ICP-MS年代学和地球化学的证据[J].中国科学(D辑):地球科学,2009,39(7):994-1008.[Chen Zhihong,Guo Kunyi,Dong Yongguan,et al.Possible early Neoproterozoic magmatism associated with slab window in the Pingshui segment of the Jiangshan-Shaoxing suture zone:Evidence from zircon LA-ICP-MS U-Pb geochronology and geochemistry[J].Science China(Seri.D):Earth Sciences,2009,39(7):994-1008.]
[60]Li Z X,Bogdanova S V,Collins A S,et al.Assembly,configuration,and break-up history of Rodinia:a synthesis[J].Precambrian Research,2008,160(1/2):179-210.
[61]Sun W H,Zhou M F,Gao J F,et al.Detrital zircon U-Pb geochronological and Lu-Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze Block,SW China[J].Precambrian Research,2009,172(1/2):99-126.
[62]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.
[63]向磊,舒良树.华南东段前泥盆纪构造演化:来自碎屑锆石的证据[J].中国科学(D辑):地球科学,2010,40(10):1377-1388.[Xiang Lei,Shu Liangshu.Pre-Devonian tectonic evolution of the eastern South China Block:Geochronological evidence from detrital zircons[J].Science China(Seri.D):Earth Sciences,2010,40(10):1377-1388.]
[64]徐先兵,张岳桥,舒良树,等.武夷山地区前寒武纪地层沉积时代研究[J].地层学杂志,2010,34(3):254-267.[Xu Xianbing,Zhang Yueqiao,Shu Liangshu,et al.Precambrian geochronology and stratigraphy in the Wuyishan area,South China[J].Journal of Stratigraphy,2010,34(3):254-267.]
[65]Yao J L,Shu L S,Santosh M.Detrital zircon U-Pb geochronology,Hf-isotopes and geochemistry-new clues for the Precambrian crustal evolution of Cathaysia Block,South China[J].Gondwana Research,2011,20(2/3):553-567.
[66]Yao W H,Li Z X,Li W X,et al.From Rodinia to gondwanaland:a tale of detrital zircon provenance analyses from the southern Nanhua Basin,South China[J].American Journal of Science,2014,314(1):278-313.
[67]Yao W H,Li Z X,Li W X,et al.Detrital provenance evolution of the Ediacaran-Silurian Nanhua foreland basin,South China[J].Gondwana Research,2015,28(4):1449-1465.
[68]张芳荣,舒良树,王德滋,等.华南东段加里东期花岗岩类形成构造背景探讨[J].地学前缘,2009,16(1):248-260.[Zhang Fangrong,Shu Liangshu,Wang Dezi,et al.Discussions on the tectonic setting of Caledonian granitoids in the eastern segment of South China[J].Earth Science Frontiers,2009,16(1):248-260.]
[69]胡艳华,顾明光,徐岩,等.浙江诸暨地区陈蔡群加里东期变质年龄的确认及其地质意义[J].地质通报,2011,30(11):1661-1670.[Hu Yanhua,Gu Mingguang,Xu Yan,et al.The confirmation of the age of Caledonian Chencai Group in Zhuji area of Zhejiang province and its geological significance[J].Geological Bulletin of China,2011,30(11):1661-1670.]
[70]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.
[71]龚根辉.华南早古生代前陆盆地沉积与构造演化[D].杭州:浙江大学,2015.[Gong Genhui.Sedimentary and tectonic evolution of the early Paleozoic foreland basin in the South China Block[D].Hangzhou:Zhejiang University,2015.]
[72]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 Liangshu.An analysis of principal features of tectonic evolution in South China Block[J].Geological Bulletin of China,2012,31(7):1035-1053.]
[73]Xu Y J,Du Y S,Cawood P A,et al.Detrital zircon provenance of upper Ordovician and Silurian Strata in the northeastern Yangtze Block:response to orogenesis in South China[J].Sedimentary Geology,2012,267-268:63-72.
[74]Wang Y J,Zhang F F,Fan W M,et al.Tectonic setting of the South China Block in the early Paleozoic:resolving intracontinental and ocean closure models from detrital zircon U-Pb geochronology[J].Tectonics,2010,29(6):TC6020,doi:10.1029/2010TC002750.