扬子板块北缘早—中志留世硅质岩成因及古沉积环境的地球化学研究
|
摘要
本文对四川省若尔盖县北部-甘肃省迭部县中-下志留统[兰多维列统(Llandovery)-温洛克统(Wenlock)]富有机碳硅质岩进行了无机化学研究,目的是探讨其成因及形成环境,并建立研究区硅质岩形成及相关元素富集模式。主要对1个钻孔、2个剖面共28件硅质岩的岩相学、扫描电镜、主量、微量、稀土元素、有机碳及Si、O稳定同位素特征进行了研究。(1)岩相学、扫描电镜分析,Fe/Ti、Al/(Al+Fe+Mn)(0.08~0.79)均值0.31、(Fe+Mn)/Ti,(La/Yb)N(0.12~1.41)均值0.54、δEu(0.81~3.36)均值1.55、∑REE(7.59~253.48)均值82.90,Si同位素(-0.2‰~2.1‰)均值0.66‰、O同位素(13.5‰~21.8‰)均值19.53‰、同位素对成岩温度的反演,显示硅质岩为热水沉积成因,并伴有生物作用(Si、O稳定同位素显示),益哇硅质岩形成时陆源物质供给适量,导致与碳酸盐相关生物繁盛,少量样品受陆源物质影响显著。(2)岩相学、扫描电镜分析,MnO_2/TiO_2、Al2O3/(Al2O3+Fe2O3)、Al/(Al+Fe)(0.08~0.80)均值0.33、Th/U、V(28.6×10~(-6)~2261×10~(-6))均值454.42×10~(-6)、Ti/V,δCe(0.65~1.58)均值1.01、(La/Ce)N(0.60~1.314)均值0.97、有机碳(TOC)-微量元素二元图解,显示研究区硅质岩形成于大陆边缘的热水喷流导致海底局部水动力较强的缺氧环境[特别是δCe、(La/Ce)N、稀土配分模式],部分硅质岩由于富集热液元素导致其具有洋脊、大洋盆地硅质岩的特征。结合前人研究成果,认为研究区硅质岩形成于扬子板块北缘(古商丹洋南缘)热水喷流系统发育(导致海底水动能较强的)、缺氧状态的陆缘拉张裂陷环境,这种环境有利于U、V、Mo、Cu、Ni等变价元素的富集,扬子板块北缘早古生代(寒武纪-志留纪)黑色页岩系产自扩张的大陆边缘缺氧-还原环境。
In this study,we performed an inorganic geochemical study of Early-Middle Silurian bedded organic C-enriched cherts in the region between northern Ruoergai(Zoigê)County and Diebu(Têwo)County,central China.The goal of this study is to determine the origin and paleodepositional environment of the chert beds and to establish a depositional model for the Yangchanggou Formation-Lalong Formation in the study area.An integrated study,involving petrographic analysis,scanning electron microscopy(SEM)analysis,major,trace and rare earth element analyses,organic carbon content analysis,and Si,and O isotopic analyses,has been performed on twenty-eight chert samples from the Yangchanggou Formation,Taer Formation and Lalong Formation of the Bailongjiang Group.Based on the petrographic,SEM,Fe/Ti,Al/(Al+Fe+ Mn)(0.08~0.79;average 0.31),(Fe+ Mn)/Ti(4.20~205.23;average 61.94),(La/Yb)N(0.12~1.41;average 0.54),δEu(0.81~3.36;average 1.55),∑REE(7.59~253.48;average 82.90),Si isotope(-0.2‰~2.1‰;average 0.66‰),and O isotope(13.5‰~21.8‰)average19.53‰)results and the diagenetic temperatures inverted from the O and Si isotopic data,the chert samples are primarily hydrothermal in origin,with some evidence of biogenic chert(based on the Si and O isotopic compositions).During the deposition of the Taer Formation,terrigenous material mixed with the paleo-seawater,promoting the growth of carbonate-producing organisms.Minor samples exhibit effect of terrigenous detrital material.Additionally,the petrographic,SEM,MnO_2/TiO_2,Al2 O3/(Al2 O3+Fe2 O3)(0.11~0.84;average 0.37),Al/(Al+Fe)(0.08~0.80;average 0.33),Th/U,V(28.6×10~(-6)~2261×10~(-6);average 454.42 ×10~(-6)),Ti/V,δCe(0.65~1.58;average 1.01),and(La/Ce)N(0.60~1.314;average 0.97)results and the REE,TOC,and trace element(U,V,Mo,Cu,Ni)patterns indicate that the chert samples were deposited on a continental margin in an anoxic environment with strong hydrodynamic conditions.Portions of the chert samples have characteristics typical of mid-ocean ridge and ocean basin environments(i.e.,they are enriched in hydrothermal elements).In combination with previous research results,we conclude that the siliceous rock formed in a continental margin extensional environment on the northern margin of the Yangtze Block.This environment was characterized by well developed hydrothermal activity and anaerobic condition,which was conducive to enrichment of U,V,Mo,Cu,and Ni.The lower Paleozoic(Cambrian-Silurian)black shale in the northern margin of the Yangtze Block deposited in anoxic to reducing conditions in the extensional continent margin.
In this study,we performed an inorganic geochemical study of Early-Middle Silurian bedded organic C-enriched cherts in the region between northern Ruoergai(Zoigê)County and Diebu(Têwo)County,central China.The goal of this study is to determine the origin and paleodepositional environment of the chert beds and to establish a depositional model for the Yangchanggou Formation-Lalong Formation in the study area.An integrated study,involving petrographic analysis,scanning electron microscopy(SEM)analysis,major,trace and rare earth element analyses,organic carbon content analysis,and Si,and O isotopic analyses,has been performed on twenty-eight chert samples from the Yangchanggou Formation,Taer Formation and Lalong Formation of the Bailongjiang Group.Based on the petrographic,SEM,Fe/Ti,Al/(Al+Fe+ Mn)(0.08~0.79;average 0.31),(Fe+ Mn)/Ti(4.20~205.23;average 61.94),(La/Yb)N(0.12~1.41;average 0.54),δEu(0.81~3.36;average 1.55),∑REE(7.59~253.48;average 82.90),Si isotope(-0.2‰~2.1‰;average 0.66‰),and O isotope(13.5‰~21.8‰)average19.53‰)results and the diagenetic temperatures inverted from the O and Si isotopic data,the chert samples are primarily hydrothermal in origin,with some evidence of biogenic chert(based on the Si and O isotopic compositions).During the deposition of the Taer Formation,terrigenous material mixed with the paleo-seawater,promoting the growth of carbonate-producing organisms.Minor samples exhibit effect of terrigenous detrital material.Additionally,the petrographic,SEM,MnO_2/TiO_2,Al2 O3/(Al2 O3+Fe2 O3)(0.11~0.84;average 0.37),Al/(Al+Fe)(0.08~0.80;average 0.33),Th/U,V(28.6×10~(-6)~2261×10~(-6);average 454.42 ×10~(-6)),Ti/V,δCe(0.65~1.58;average 1.01),and(La/Ce)N(0.60~1.314;average 0.97)results and the REE,TOC,and trace element(U,V,Mo,Cu,Ni)patterns indicate that the chert samples were deposited on a continental margin in an anoxic environment with strong hydrodynamic conditions.Portions of the chert samples have characteristics typical of mid-ocean ridge and ocean basin environments(i.e.,they are enriched in hydrothermal elements).In combination with previous research results,we conclude that the siliceous rock formed in a continental margin extensional environment on the northern margin of the Yangtze Block.This environment was characterized by well developed hydrothermal activity and anaerobic condition,which was conducive to enrichment of U,V,Mo,Cu,and Ni.The lower Paleozoic(Cambrian-Silurian)black shale in the northern margin of the Yangtze Block deposited in anoxic to reducing conditions in the extensional continent margin.
引文
Adachi M,Yanlamoto K,Sujgisk R.1986.Hydrothermal chert andassociated siliceous rocksfrom the North Pacific:Their geologicalsignificance as indication of ocean ridge activity.SedimentaryGeology,47(1~2):125~148.
Baldwin G J,Thurston P C,Kamber B S.2011.High-precision rare earth element,nickel,and chromium chemistry of chert microbands pre-screened with in-situ analysis.Chemical Geology,285:133~143.
Bau M,Alexander B W.2009.Distribution of high field strength elements(Y,Zr,REE,Hf,Ta,Th,U)in adjacent magnetite and chert bands and in reference standards FeR-3and FeR-4from the Temagami iron-formation,Canada,and the redox level of the Neoarchean ocean.Precambrian Research,174:337~346
Bostrom K.1973.Provenance and accumulation rates of opaline silica:Al,Fe,Mn,Cu,Ni,and Co in Pacific pelagic sediment.Chemical Geology,11:123~148.
Boynton W V,1984.Cosmochemistry of the Rare Earth Elements.In:Henderson P ed.Rare Earth Element Geochemistry.Developments in Geochemistry 2.Elsvier,Amsterdam,63~114.
Bruce M C,Percival I G.2014.Geochemical evidence for provenance of Ordovician cherts in southeastern Australia.Australian Journal of Earth Sciences,61:927~950.
Calvert S E,Pedersen T F.1993.Geochemistry of Recent Oxic and Anoxic Marine Sediments:Implications for the Geological Record.Marine Geology,113:67~88.
Carbonnea J,Robertb M F,Chaussidonc M.2014.The silicon and oxygen isotope compositions of Precambrian cherts:A record of oceanic paleo-temperatures?Precambrian Research,247:223~234.
Chen Youliang,Hou Mingcai,Zhu Xiyang,Zhao Jianbo,2007.Petrology and genesis of ore-bearing rock series in the Zoige uranium ore field,Sichuan,China.Journal of Chengdu University(Natural Science Edition),34(5):553~558(in Chinese with English abstract).
Cheng Lixue,Wang Yuanjun,Chen Hongde,Wang Yue,Zhong Yijiang,2013.Sedimentary and burial environment of black shales of Sinian to Early Palaeozoic in Upper Yangtze region.Acta Petrologica Sinica,29(8):2906~2912(in Chinese with English abstract).
Ding Tiping,Jiang Shaoyong,Wan Defang,Li Yanhe,Li Jincheng,Song Hebing,Liu Zhijian,Yao Xiaonei,1988.Silicon Isotope Geochemistry.Beijing:Geology Publishing House(in Chinese),31~42.
Ding Tiping,Wan Defang,Li Jincheng,Jiang Shaoyong,Song Hebing,Li Yanhe,Liu Zhijian,1988.The analytical method of silicon isotopes and its geological application.Mineral Deposits,7(4):90~95(in Chinese with English abstract).
Ding Zhenju,and Liu Congqiang,2000b.Bikou group developed ancient hydrothermal system from REE evidence of iron riched chert.Progress in Natural Science,10(5):427~434(in Chinese with English abstract).
Ding Zhenju,Liu Congqiang,Yao Shuzhen,Zhou Zonggui,2000a.Rare earth elements compositions of high temperature hydrothermal fluids in seafloor and control factors.Advance in Earth Sciences),15(3):307~312(in Chinese with English abstract).
Du Yuansheng,Sheng Jihu,Feng Qinglai,Wang Zhiping,Gu Songzhu,1998.New recognition of Non-Smith stratigraphy and paleoceanography of Mianxian-Lueyang paleosuture in Southern Qinling,China.Geoscience,12(1):26~31(in Chinese with English abstract).
Elderfield H,Greaves M J.1982.The rare earth elements in seawater.Nature,296,214~219.
Emerson S R,Huested,S S.1991.Ocean Anoxia and the Concentration of Molybdenum and Vanadium in Seawater.Marine Chemistry,34:177~196.
Feng Shengbin,Zhou Hongrui,Yan Changhai,Peng Yi,Yuan Xiaoqi,He Jing,2007.Geochemical characteristics of hydrothermal cherts of Erlangping Group in East Qinling and their geologic significance.Acta Sedimentologica Sinica,25(4):564~573(in Chinese with English abstract).
Garbán G,Martínez M,Márquez G.2017.Geochemical signatures of bedded cherts of the upper La Luna Formation in Táchira State,western Venezuela:Assessing material provenance and paleodepositional setting.Sedimentary Geology,347:130~147.
He Junguo,Zhou Yongzhang,Li Hongzhong.2011.Study on Geochemical Characteristics and Depositional Environment of Pengcuolin Chert,Southern Tibet.Journal of Geography and Geology,3(1):178~188.
He Junguo,Zhou Yongzhang,Yang Zhijun,Li Hongzhong,Wang Xiaoyue,2009.Study on geochemical characteristics and depositional environment of Pengcuolin chert,Southern Tibet.Journal of Jilin University(Earth Science Edition),39(6):1055~1065(in Chinese with English abstract).
He Xinyi,Chen Jianqiang,1999.Early Silurian Rugose Coral Fauna of Tewo area,West Qinling.Acta Palaeontologica Sinica,38(4):423~434(in Chinese with English abstract).
Hecht A D,Savin S M.1970.Oxygen-18 studies of recent planktonic Foraminifera:comparisons of phenotypes and of test parts.Science,170(3953):69~71.
Hoyle J,Elderfield H,Gledhill A,Greaves M.1984.Thebehavior of the rare~earth elements during the mixing of river and sea waters.Geochimica et Cosmochimica Acta,48,143~149.
Hu Jianmin,Meng Qingren,Bai Wuming,Zhao Guochun,2002.Mid-Late Paleozoic extension of the Wudang block in the South Qinling tectonic belt,China.Regional Geology of China,21(8~9):471~477(in Chinese with English abstract).
Huang Hu,Du Yuansheng,Huang Zhiqiang,Yang Jianghai,Huang Hongwei,Xie Chunxia,Hu Lisha.2013.Depositional chemistry of chert during late Paleozoic from western Guangxi and its implication for the tectonic evolution of the Youjiang Basin.Science in China:Series D Earth Sciences,56(3):479~493.
Ikeda M,Tada R,Sakuma H.2010.Astronomical cycle origin of bedded chert:A middle Triassic bedded chert sequence,Inuyama,Japan.Earth and Planetary Science Letters,297:369~378.
Jin Youzhong,Tian Wenhao,2011.An analysis of metallogenic conditions and resource of the Zoige uranium deposit.Geology in China,38(3):681~691(in Chinese with English abstract).
Kakuwa Y,Webb J.2010.Evolution of Cambrian to Ordovician trace fossils in pelagic deep-sea chert,Australia.Australian Journal of Earth Sciences,57:615~625.
Kang Jianli,Zhang Zhaochong,Zhang Dongyang,Hang He,Dong Shuyu,Zhang Su.2011.Geochronology and Geochemistry of the Radiolarian Cherts of the Madar’er Area,Southwestern Tianshan:Implications for Depositional Environment.Acta Geologica Sinica(English Edition),85(4):801~813.
Kemkin I V,Kemkina1 R A.2015.Depositional Environment of Cherts of the Sikhote~Alin Region(Russia Far East):Evidence from Major,Trace and Rare Earth Elements Geochemistry.Journal of Earth Science,26(2):259~272.
Klinkhammer G P,Elderfield H,Edmond J M,Mitra A.1994.Geochemical implications of rare earth element patterns in hydrothermal fluids from mid-ocean ridges.Geochimica et Cosmochimica Acta,58(23):5105~5113.
Klinkhammer G P,Elderfield H,Edmond J M,Mitra A.1994.Geochemical implications of rare earth element patterns in hydrothermal fluids from mid-ocean ridges.Geochimica et Cosmochimica Acta,58(23),5105~5113.
Krings M,Taylor T N.2015.A fungal reproductive unit from the Lower Devonian Rhynie chert(Aberdeenshire,Scotland)that demonstrates an unusual hyphal investment pattern.Scottish Journal of Geology,51:131~139.
Ledevin M,Arndt N,Simionovici A.2014.Silica precipitation triggered by clastic sedimentation in the Archean:New petrographic evidence from cherts of the Kromberg type section,South Africa.Precambrian Research,255:316~334.
Lewis K H,Garwood R J,Brasier M D,Goral T,Jiang H,McLoughlin N,Wacey D.2016.Carbonaceous microstructures from sedimentary laminated chert within the 3.46 Ga Apex Basalt,Chinaman Creek locality,Pilbara,Western Australia.Precambrian Research,278:161~178.
Li Hongzhong,Zhou Yongzhang,Yang Zhijun,He Junguo,Ma Zhanwu,Li Wenchao,Zhou Guofu,An Yanfei,Li Wen,Liang Jin,Wang Chi,2010.A study of micro-area compositional characteristics and the evolution cherts from Bafangshan-Erlihe Pb-Zn ore deposition Western Qinling Orogen.Earth Science Frontiers,17(4):290~298(in Chinese with English abstract).
Li Hongzhong,Zhou Yongzhang,Yang Zhijun,Zhou Guofu,He Junguo,Ma Zhanwu,Li Wenchao,Liang Jin,Li Wen,2011.Diagenesis and metallogenesis evolution of chert in west Qinling Orogenic Belt:A case from Bafangshan-Erlihe Pb-Zn ore deposit.Journal of Jilin University(Earth Science Edition),41(3):715~723(in Chinese with English abstract).
Li Hongzhong,Zhou Yongzhang,YangZhijun,GuZhihong,Lu Wenchao,He Junguo,Li Wen,An Yanfei,2009.Geochemical characteristics and their geological implications of cherts from Bafangshan-Erlihe area in western Qingling orogeny.Acta Petrologica,25(11):3094~3102(in Chinese with English abstract).
Li Xianhua,2000.Geochemistry of the Late Paleozoic radiolarian cherts within the NE Jiangxi ophiolite melange and its tectonic significance.Science in China:Series D Earth Sciences(English edition),30(3):1~5.
Li Yanhe,Ding Tiping,Wan Defang,1995.Experimental study of silicon isotope dynamic fractionation and its geological application.Chinese Journal of Geochemistry,13(3):282~288(in Chinese with English abstract).
Liang Bin,Feng Qinglai,Wang Quanwei,Guo Jianqiu,Zhong Changhong,Li Zhenjing.2005.Ladinian radiolarian,siliceous rock from the Xianshuihe Belt,West Sichuan and their tectonic significance.Science in China:Series D Earth Sciences,48(1):42~47.
Lin Li,Zhu Lidong,Zhu Dicheng,1998.Study of molecular paleontology in thermal chert in Laerma gold deposit of West Qinling.Earth Science-Journal of China University of Geosciences,23(5):503~507(in Chinese with English abstract).
Liu Hanbin,Jin Guishan,Li Junjie,Han Juan,Zhang Jianfeng,Zhang Jia,Zhong Fangwen,Guo Dongqiao,2013.Determination of stable isotope composition in uranium geological samples.World Nuclear Geoscience,30(3):174~179(in Chinese with English abstract).
Liu Jiajun,Feng Caixia,Liu Jianming,Zheng Minghua,Li Chaoyang,2004.Reidentification of the ore-hosted strata age and metallogenic age of the strata bound Au~Se deposits,the Western Qinling mountains.Earth Science Frontiers,11(2):435~443(in Chinese with English abstract).
Liu Jiajun,Zheng Minghua,Liu Jianming,Zhou Yufeng,Gu Xuexiang,Zhang Bin,1999.The geological and geochemical characteristics of Cambrian chert and their sedimentary environmental implications in western Qinling.Acta Petrologica Sinica,15(1):145~154(in Chinese with English abstract).
Liu Shuwen,Xue Chunji,Zeng Rong,Li Qiang,Zhu Jingxiang,Wang Tao,Zhao Guobin,2005.Petrology and geochemistry of siliceous rocks in Silurian lead-zinc deposits of southern Qinling region.Mineral Deposits,24(5):490~500(in Chinese with English abstract).
Lu Songnian,Yu Haifeng,Li Huaikun,Chen Zhihong,Wang Huichu,Zhang Chuanlin,Xiang Zhenqun.Early Paleozoic suture zones and tectonic divisions in the“Central China Origen”.Geological Bulletin of China,2006,25(12):1368~1380(in Chinese with English abstract).
Lu Zhicheng,Liu Congqiang,Liu Jiajun,Wu Fengchang,2004.Geochemical Studies on the Lower Cambrian Witherite-bearing Cherts in the Northern Daba Mountains.Acta Geologica Sinica,78(3):390~406(in Chinese with English abstract).
Lyons T W,Werne J P.,David J H,Murray R W.2003.Contrasting sulfur geochemistry and Fe/Al and Mo/Al ratios across the last oxic-to-anoxic transition in the Cariaco Basin,Venezuela.Chemical Geology,195:131~157.
Mao Liguang,Xiao Ancheng,Wei Guoqi,Shen Zhongyan,Wang Liang,Zhang Lin,Qian Junfeng,2011.Distribution and origin of the Late Paleozoic~Mesozoic rift systems in the northern margin of theYangtze block.Acta Petrologica Sinica,27(3):721~731(in Chinese with English abstract).
Marchig V.1982.Some geochemistry indicators for discriminational between diagenetic andhydrothermal metalliferous sediments.Marine Geology,58(3):241~256.
Marin-Carbonne J,Chaussidon M,Boiron M C,Robert F.2011.Acombined in situ oxygen,silicon isotopic and fluid inclusion study of a chert sample from Onverwacht Group(3.35 Ga,South Africa):New constraints on fluid circulation.Chemical Geology,286:59~71.
Marshall C P,Emry J R,Marshall A O.2011.Haematite pseudomicrofossils present in the 3.5-billion-year-old Apex Chert.Nature Geoscience,1~4.
Michard A.1989.Rare earth ekment systematics in hydrothermalfluids.Geochimica et Cosmochimica Acta,53:745~750.
Miroshnichenko N V,Perevoznikova Y V.2010.The Intermetallic Compound Ni3Au and Gold-Nickel Solid Solutions in Metalliferous Sediments of the Triassic Chert Formation in Sikhote-Alin in the Far East.Russian Journal of Pacific Geology,4(1):56~62.
Morford J L,Emerson S.1999.The Geochemistry of Redox Sensitive Trace Metals in Sediments.Geochimica et Cosmochimica Acta,63:1735~1750.
Murray R W.1994.Chemical criteria to identify the depositionalenvironment of chert:general principles and application.Sediment Geology,90:213~232.
Murry R W,Buchholtz T,Brink M R,Gerlach D C,Russ G P,Jones D L.1990.Rare earth elements as indicators of different marine depos-itional environments in chert and shale.Geology,18:268~271.
Murry R W,Buchholtz T,Brink M R,Gerlach D C,Russ G P,Jones D L.1991.Rare earth,major,and trace elements in chert from Franciscan Complex and Monterey Group:Assessing REE sources to fine-grained marine sediments.Geochimica et Cosmochimica Acta,55:1875~1895.
Qi Fucheng,Zhang Zilong,Li Zhixing,He Zhongbo,Wang Wenquan,2012.Temporal and spatial evolution pattern of Carbonaceous-Siliceous argillaceous rock type uranium deposits in China.Uranium Geology,28(2):65~71(in Chinese with English abstract).
Qi Huawen,Hu Ruizhong,Su Wenchao,Qi Liang,Feng Jiayi.2004.Continental hydrothermal sedimentary siliceous rock and genesis of superlarge germanium(Ge)deposit hosted in coal:Astudy from the Lincang Ge deposit,Yunnan,China.Science in China:Series D Earth Sciences,47(11):973~984.
Qiu Zhen,Wang Qingchen.2011.Geochemical evidence for submarine hydrothermal origin of the Middle-Upper Permian chert in Laibin of Guangxi,China.Science in China:Series DEarth Sciences,54(7):1011~1023.
Ran Bo,Liu Shugen,Jansa Lubab,Wei Sun,Yang Di,Ye Yuehao,Wang Shiyu,Luo Chao,Zhang Xuan,Zhang Changjun.2015.Origin of the Upper Ordovician-lower Silurian cherts of the Yangtze block,South China,and their palaeogeographic significance.Journal of Asian Earth Sciences,108:1~17.
Rona P A.1978.Criteria for recognition of hydrothermal mineral deposits in ocean crust.Economic Geology,73(2):135~160.
Rong Jiayu,ChenXu,Su Yangzheng,Zhan Renbin,Ni Yunan,Zhan Renbin,Cheng Tingen.2003.Silurian paleogeography of China[M]//Landing E,Johnson M.E.Silurian Landsand Seas:Paleogeography,Outside of Laurentia.New York:New York State Museum Bulletin,493:243~298.
Rouchon V,Orberger B.2008.Origin and mechanisms of K-Simetasomatism of ca.3.4-3.3 Ga volcaniclastic deposits and implications for Archean seawater evolution:Examples from cherts of Kittys Gap(Pilbara craton,Australia)and Msauli(Barberton Greenstone Belt,South Africa).Precambrian Research,165:169~189.
Sato T,Isozaki Y,Shozugawa K.2011.57Fe Mosbauer spectroscopic analysis of deep-sea pelagic chert:Effect of secondary alteration with respect to paleo-redox evaluation.Journal of Asian Earth Sciences,42:1403~1410.
Shen B,Lee C A.,Xiao S.2011.Germanium/silica ratios in diagenetic chert nodules from the Ediacaran Doushantuo Formation,South China.Chemical Geology,280:323~335.
Sheng Jihu,Du Yuansheng,Feng Qinglai,Xu Jifeng,1997.Depositional environments of cherts in the ophiolite melange belt from Mian-Lue,Shanxi Province.Earth Science-Journal of China University of Geosciences,22(6):599~602(in Chinese with English abstract).
Sholkovitz E R.1988.Rare earth elements in the sediments of the North Atlantic Ocean,Amazon Delta,and East China Sea;reinterpretation of terrigenous input patterns to the oceans.American Journal of Science,288(3),236~281.
Shu Liangshu,2010.Physical Geology(third edition).Beijing:Geology Publishing House,1~292(in Chinese).
Song Tianrui,Ding Tiping,1989.A new probe of application of Silicon isotopic(δ30Si)in siliceous rocks to sedimentary facies analysis.Chinese Science Bulletin,34(18):1408~1411(in Chinese with English abstract).
Sun ShengLi,Chen Jianfa,Zheng Jianjing,Liu Wenhui.2009.The noble gas isotope geochemical composition of chert at the bottom of Cambrian in Tarim Basin,China.Science in China:Series D Earth Sciences,52:115~119.
Tayloy S R,Mclennan S M.1981.The composition and evolution of the continental crust:rare earth element evidence from sedimentary rocks.Phil.Trans.R.Soc.London,A301,381~399.
Tayloy S R,Mclennan S M.1981.The composition and evolution of the continental crust:rare earth element evidence from sedimentary rocks.Phil.Trans.R.Soc.London,A301,381~399.
Tekin U K,Goncuoglu M C.2009.Late Middle Jurassic(Late Bathonian-Early Callovian)Radiolarian Cherts from the Neotethyan Bornova Flysch Zone,Spil Mountains,Western Turkey.Geologicheskaya Korrelyatsiya,17(3):70~80.
Tessalina1SG,Bourdon B,Kranendonk M V.2010.Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton.NATURE GEOSCIENCE,3:214~217.
Thassanapak H,Mongkol U,Chonglakmani C,Feng Q.2011.Geochemistry of Middle Triassic Radiolarian Cherts from Northern Thailand:Implication for Depositional Environment.Journal of Earth Science,22(6):688~703.
Thomson J,Higgs N C,Croudace I W,Colley S,Hydes D J,1993.Redox Zonation of Elements at an Oxic/Post-Oxic Boundary in Deep-Sea Sediments.Geochimica et Cosmochimica Acta,57:579~595.
Tribovillard N,Algeo T J,Lyons T,Riboulleau A.2006.Trace Metals as Paleoredox and Paleoproductivity Proxies:An Update.Chemical Geology,232:12~32.
Udchachon M,Thassanapak H,Feng Q.2011.Geochemical constraints on the depositional environment of Upper Devonian radiolarian cherts from Loei,north-eastern Thailand.Front.Earth Sci.5(2):178~190.
Wang Nianzhong,Wang Junqing,Zhang Guorui,1998.The first discovery of Silurian and Early Devonian Acanthodians from Zoige and Tewo counties,West Qinling mountains.Vertebrata Palasiatica,36(4):268~281(in Chinese with English abstract).
Wang Xinwei,Wo Yujin,Zhang Rongqiang,2008.Tectonicsedimentary cycle of the Yangtze Craton from Nanhuaan to the Early Palaeozoic.Geoscience,22(4):525~533(in Chinese with English abstract).
Wang Zongqi,Yan Quanren,Yan Zhen,Wang Tao,Jiang Chunfa,Gao Lianda,Li Qiugen,Chen Junlu,Zhang Yingli,Liu Ping,Xie Chunlin,Xiang Zhongjin,2009.New division of the main tectonic units of the Qinling Orogenic Belt,Central China.Acta Geologica Sinica,83(11):1527~1546(in Chinese with English abstract).
Wen Hanjie,Fan Haifeng,Tian Shihong,Wang Qilian,Hu Ruizhong,2016.The formation conditions of the early Ediacaran cherts,South China.Chemical Geology,430:45~69.
Wen Hanjie,Fan Haifeng,Tian Shihong,Wang Qilian,Hu Ruizhong.2016.The formation conditions of the early Ediacaran cherts,South China.Chemical Geology,430:45~69.
Xiang Lei,Cai Chunfang,He Xunyun,Jiang Lei,Yuan Yuyang,Yu Lei,2016.Evolution of redox state during the Terreneuvian epoch at Zhalagou section,South China.Acta Geologica Sinica,24(3):600~608(in Chinese with English abstract).
Xiang Lei,Cai Chunfeng,He Xunyun,Jiang Lei.2012.The mechanisms for the enrichment of trace elements in the Lower Cambrian black chert successions from Zhalagou section,Guizhou Province.Acta Petrologica Sinica,28(3):971~980(in Chinese with English abstract).
Xiao Shuhai,Schiffbauer James D.,McFadden Kathleen A.,et al.2010.Petrographic and SIMS pyrite sulfur isotope analyses of Ediacaran chert nodules:Implications for microbial processes in pyrite rim formation,silicification,and exceptional fossil preservation Earth and Planetary Science Letters,297:481~495.
Xie Xiaomin,Tenger,Qian Jianzhong,Zhang Qingzhen,Bian Lizeng,Yin Leiming,2015.Depositional environment,organisms components and source rock formation of siliceous rocks in the base of the Cambrian Niutitang Formation,Kaili,Guizhou.Acta Geologica Sinica,89(2),425~439(in Chinese with English abstract).
Xue Chunji,Jiang Shaoyong,Li Yanhe,1998.Devonian chert Silicon,Oxygen isotope geochemical study,Qinling.Journal of Xi’an Engineering University,20(1):10~13(in Chinese with English abstract).
Yamamoto K.1987.Geochemical characteristics and depositional environnlents of cherts and associated rocks in the Franciscan and Shimanto lerrenes.Sedimentary Geology,52:65~108.
Yang Liqiang,Ji Xingzhong,Santosh M.,Li Nan,Zhang Zhichao,Yu Jinyuan.2015.Detrital zircon U-Pb ages,Hf isotope,and geochemistry of Devonian chert from the Mianlue suture:Implications for tectonic evolution of the Qinling orogeny.Journal of Asian Earth Sciences,113:589~609.
Yang Ruidong,Wei Huairui,Bao Miao,Wang Wei,Wang Qiang,2007.Submarine Hydrothermal venting-flowing sedimentary characters of the Cambrian Shanggongtang and Dahebian barite deposits,Tianzhu County,Guizhou Province.Geological Review,53(5):675~680.
Yang Ruidong,Zhang Chuanlin,Luo Xing Rong,Tian Jingquan,Bao Yafan,Song Guoqi,2006.Geochemical Characteristics of Early Cambrian Cherts in Quruqtagh,Xinjiang,West China.Acta Geologica Sinica,80(4):598~605.
Yang Ruidong,Zhu Lijun,Gao Hui,Zhang Weihua,Jiang Lijun,Wang Qiang,Bao Miao,2005.Yang R,Zhu L,Gao H,et al.A study on characteristics of the hydrothermal vent and relating biota at the Cambrian bottom in Songlin,Zunyi County,Guizhou Province.Geological Review,51(5):481~492.
Yao Chunyan,Ma Dongsheng,Ding Haifeng,Zhang Xiaoyong,Huang Hui.2014.Trace elements and stable isotopic geochemistry of an Early Cambrian chert-phosphorite unit from the lower Yurtus Formation of the Sugetbrak section in the Tarim Basin.57(3):454~464
Yao Zhongyou,1994.A preliminary discussion on geological characteristics and genesis of the Laerma gold deposit in Luqu county,Gansu province.Mineral Deposits,13(1):19~27(in Chinese with English abstract).
Ye Yongqin,Chen Youliang,Zhao Cong,2015.Vertical zoning features of the mineral assemblages in the Zoige 510-1uranium deposit and its prospecting significance.Acta Mineralogica Sinica,35(2):239~244(in Chinese with English abstract).
Yin Leiming,Borjiginb Tenger,Knollc Andrew H.,Bian Lizeng,Xie Xiaomin,Bao Fang,Ou Zhiji.2016.Sheet-like microfossils from hydrothermally influenced basinal cherts of thelower Cambrian(Terreneuvian)Niutitang Formation,Guizhou,South China.Palword,350:1~11.
Yu Bingsong,Dong Hailiang,Widom Elisabeth.2009.Geochemistry of basal Cambrian black shales and cherts from the Northern Tarim Basin,Northwest China:Implications for depositional setting and tectonic history.Journal of Asian Earth Sciences,34:418~436.
Zhang Chengjiang,Chen Youliang,2010.Discovery of vertical zoning in the 510-1 uranium deposit and its geological implications.Geology and Explomolar ratiosn,46(3):434~441(in Chinese with English abstract).
Zhang Chengli,Gao Shan,Zhang Guowei,Guo Anlin,Yuan Honglin,Liu Xiaoming,Wang Jianqi.2004.Geochemistry of ophiolite cherts from the Qinling orogenic belt and implications for their tectonic settings.Science in China:Series D Earth Sciences,47(4):329~337.
Zhang Chengli,Gao Shan,Zhang Guowei,Liu Xiaoming,Yu Zaiping.2003.Geochemistry of early Paleozoic alkali dyke swarms in south Qinling and its geological significance.Science in China:Series D Earth Sciences,46(12):1292~1306.
Zhang Chengli,Zhou Dingwu,Lu Guanxiang,Wang Juli,Wang Ruisan,2006.Geochemical characteristics and sedimentary environments of cherts from Kumishi ophiolitic mélange in southern Tianshan.Acta Petrologica Sinica,22(1):57~64(in Chinese with English abstract).
Zhang Guowei,Dong Yunpeng,Lai Shaocong,2004.Mianlue tectonic zone and Mianlue suture zone on southern margin of Qinling-Dabie orogenic belt.Science in China:Series D Earth Sciences(English edition),47:300~316.
Zhang Guowei,Meng Qingren,Lai Shaocong,1995.Structure and tectonics of the Qinling Orogenic belt.Science in China.(Series B),25:994~1003(in Chinese with English abstract).
Zhang Guowei,Meng Qingren,Yu Zaiping,Sun Yong,Zhou Dingwu,Guo Anlin,1996.Orogenesis and dynamics of Qinling orogen.Science in China:Series D Earth Sciences(English edition),26:193~200.
Zhang Guowei,Yu Zaiping,Dong Yunpeng,Yao Anlin,2000.On Precambrian framework and evolution of the Qinling belt.Acta Petrologica Sinica,16:11~21(in Chinese with English abstract).
Zhang Yaguan,Du Yuansheng,Xu Yajun,Yu Wenchao,Huang Hu,Jiao Liangxuan,2015.Geochemical characteristics of siliceous rocks during the transition from Sinian(Ediacaran)to Cambrian in central Hunan and its implication for genesis and sedimentary environment..Geological Review,61(3),499~510(in Chinese with English abstract).
Zhang Yan,Qi Fucheng,Zhang Zilong,Li Zhixing,Wang Wenquan,Yang Zhiqiang,2015a.Geochemical Characteristics of Hot Water Deposited Siliceous Rock in Jiangzha Uranium Deposit.Uranium Geology,31(2):81~88(in Chinese with English abstract).
Zhang Yan,Qi Fucheng,Zhang Zilong,Li Zhixing,Wang Wenquan,Yang Zhiqiang,2015b.Geochemical characteristics and genesis analysis of the Silurian siliceous rock in Diebu.Journal of East China Institute of Technology,38(4):375~460(in Chinese with English abstract).
Zhang Zilong,Qi Fucheng,Fu Jin,He Zhongbo,Wang Wenquan,Su Xiangli,Li Zhixing,2011.Analysis on geological conditions and orientaion of uranium explomolar ratiosn in Diebu ore field.Uranium Geology,27(5):257~264(in Chinese with English abstract).
Zheng Minghua,Liu Jiajun,1993.On the submarine exhalative sedimentation nature of silicalites from the gold-copper-uranium metallogenic belt in the south subzone of Western Qinling.Journal of Chengdu University(Natural Science Edition),20(2):9~16(in Chinese with English abstract).
Zhou Yijun,He Guoqi,Zhang Xueqin,Li Jihua,2000.Tectonic and gold mineralization in triangle regional of Chuan-Shan-Gan.Mineral Deposits,21:319~322(in Chinese with English abstract).
Zhou Yongzhang,Fu Wei,Yang Zhijun,He Junguo,Nie Fengjun,Li Wen,Zhao Wenxia,2008.Microfabrics of chert from Yarlung Zangbo Suture Zone and southern Tiebet and its geological implications.Acta Petrologica Sinica,24(3):600~608(in Chinese with English abstract).
Zhu Jie,Du Yuansheng,Liu Zaoxue,Feng Qinglai,Tian Wangxue,Li Jinping,Wang Changping.2006.Mesozoic radiolarian chert from the middle sector of the Yarlung Zangbo suture zone,Tibet and its tectonic implications.Science in China:Series DEarth Sciences,49(4):348~357.
陈友良,侯明才,朱西养,赵剑波.2007.若尔盖铀矿田含矿岩系的岩石特征及成因探讨.成都理工大学学报(自然科学版),34(5):553~558.
程立雪,王元君,陈洪德,王约,钟怡江.2013.上扬子地区震旦系-早古生界黑色页岩的沉积和埋藏环境.岩石学报,29(8):2906~2912.
丁悌平,蒋少涌,万德芳,李金城,宋鹤彬,刘志坚.1994.硅同位素地球化学.北京:地质出版社,31~42.
丁悌平,万德芳,李金城,蒋少涌,宋鹤彬,李延河,刘志坚.1988.硅同位素测量方法及其地质应用.矿床地质,7(4):90~95.
丁振举,刘丛强,姚书振,周宗桂.2000a.海底热液系统高温流体的稀土元素组成及其控制因素.地球科学进展,15(3):307~312.
丁振举,刘丛强.2000b.碧口群古热水系统发育的富铁硅岩稀土元素地球化学证据.自然科学进展,10(5):427~434.
杜远生,盛洁虎,冯庆来,王治平,顾松竹.1998.南秦岭勉略古缝合带非史密斯地层和古海洋新知.现代地质,12(1):26~31.
冯胜斌,周洪瑞,燕长海,彭翼,袁效奇,贺静.2007.东秦岭二郎坪群硅质岩热水沉积地球化学特征及其地质意义.沉积学报,25(4):564~573.
何俊国,周永章,杨志军,李红中,王晓悦.2009.藏南彭错林硅质岩地球化学特征及沉积环境分析.吉林大学学报:地球科学版,39(6):1055~1065.
何心一,陈建强.1999.西秦岭迭部地区早志留世四射珊瑚动物群.古生物学报,38(4):423~434.
胡健民,孟庆任,白武明,赵国春.2002.南秦岭构造带中-晚古生代伸展构造作用.地质通报,21(8~9):471~477.
金有忠,田文浩.2011.若尔盖铀矿田成矿地质条件及资源潜力分析.中国地质,38(3):681~691.
李红中,周永章,杨志军,古志宏,吕文超,何俊国,李文,安燕飞.2009.秦岭造山带西段八方山-二里河地区硅质岩的地球化学特征及其地质意义.岩石学报,25(11):3094~3102.
李红中,周永章,杨志军,何俊国,马占武,吕文超,周国富,安燕飞,李文,梁锦,王驰.2010.西秦岭八方山-二里河Pb-Zn矿区硅质岩的微区成分特征及演化.地学前缘,17(4):290~298.
李红中,周永章,杨志军,周国富,何俊国,马占武,吕文超,李文,梁锦,卢文姬.2011.西秦岭造山带硅质岩的成岩成矿演化特征-以八方山-二里河矿区赋矿硅质岩为例.吉林大学学报,41(3):715~723.
李献华.2000.赣东北蛇绿混杂岩带中硅质岩的地球化学特征及构造意义.中国科学(D辑),30(3):1~5.
李延河,丁悌平,万德芳.1994.硅同位素动力学分馏的实验研究及其地质应用.矿床地质,13(3):282~288.
林丽,朱利东,朱弟成.1998.西秦岭拉尔玛金矿热水硅质岩中的分子古生物学研究.地球科学,23(5):503~507.
刘汉彬,金贵善,李军杰,韩娟,张建锋,张佳,钟芳文,郭东侨.2013.铀矿地质样品的稳定同位素组成测试方法.世界核地质科学,30(3):174~179.
刘家军,冯彩霞,刘建明,郑明华,李朝阳.2004.西秦岭南亚带层控金硒矿床的赋矿地层年代与成矿时代.地学前缘,11(2):435~443.
刘家军,郑明华,刘建明,何俊国,马占武,吕文超,周国富,安燕飞,李文,梁锦,王驰.1999.西秦岭寒武系金矿床中硅岩的地质地球化学特征及其沉积环境意义.岩石学报,15(1):145~154.
刘淑文,薛春纪,曾荣,李强,朱经祥,王涛,赵国斌.2005.南秦岭志留纪铅锌矿床中硅质岩岩石学及地球化学.矿床地质,24(5):490~500.
陆松年,于海峰,李怀坤,陈志宏,王惠初,张传林,相振群.2006.“中央造山带”早古生代缝合带及构造分区概述.地质通报,25(12):1368~1380.
吕志成,刘丛强,刘家军,吴丰昌.2004.北大巴山下寒武统毒重石矿床赋矿硅质岩地球化学研究.地质学报,78(3):390~406.
毛黎光,肖安成,魏国齐,沈中延,王亮,张林,钱俊锋.2011.扬子地块北缘晚古生代-早中生代裂谷系统的分布及成因分析.岩石学报,27(3):721~731.
孟庆任,张国伟,于在平,梅志超.1996.秦岭南缘晚古生代裂谷-有限洋盆沉积作用及构造演化.中国科学(D辑),26(增刊):28~33.
漆富成,张字龙,李治兴,何中波,王文全.2012.中国碳硅泥岩型铀矿床时空演化规律.铀矿地质,28(2):65~71.
胜吉虎,杜远生,冯庆来,许继锋.1997.南秦岭勉略蛇绿混杂岩带硅质岩沉积环境研究.地球科学,22(6):599~602.
舒良树.2010.普通地质学.第三版.北京:地质出版社,1~292.
宋天锐,丁悌平.1989.硅质岩的硅同位素(δ30Si)应用于沉积相分析的新尝试.科学通报,34(18):1408~1411.
汪新伟,沃玉进,张荣强.2008.扬子克拉通南华纪-早古生代的构造-沉积旋回.现代地质,22(4):525~533.
王念忠,王俊卿,张国瑞,王世涛.1998.西秦岭若尔盖、迭部志留纪和早泥盆世棘鱼类的首次报道-西秦岭志留纪和泥盆纪脊椎动物研究之一.古脊椎动物学报,36(4):268~281.
王宗起,闫全人,闫臻,王涛,姜春发,高联达,李秋根,陈隽璐,张英利,刘平,谢春林,向忠金.2009.秦岭造山带主要大地构造单元的新划分.地质学报,83(11):1527~1546.
向雷,蔡春芳,贺训云,姜磊,袁余洋,于雷.2016.华南渣拉沟剖面纽芬兰世沉积水体氧化还原状态演化.地质学报,89(6),1120~1133.
向雷,蔡春芳,贺训云,姜磊.2012.贵州渣拉沟剖面下寒武统黑色硅质岩微量元素富集机制.岩石学报,28(3):971-980.
谢小敏,腾格尔,秦建中,张庆珍,边立曾,尹磊明.2015.贵州凯里寒武系底部硅质岩系生物组成、沉积环境与烃源岩发育关系研究.地质学报,89(2),425~439.
薛春纪,蒋少勇,李延河.1998.秦岭泥盆纪硅质岩硅、氧同位素地球化学研究.西安工程学院学报,20(1):10~13.
杨瑞东,魏怀瑞,鲍淼,王伟,王强.2007.贵州天柱上公塘-大河边寒武纪重晶石矿床海底热水喷流沉积结构、构造特征.地质论评,53(5):675~680.
杨瑞东,张传林,罗新荣,田敬全,包亚范,宋果奇,2006.新疆库鲁克塔格地区早寒武世硅质岩地球化学特征及其意义.地质学报,80(4):598~605.
杨瑞东,朱立军,高慧,张位华,姜立君,王强,鲍淼.2005.贵州遵义松林寒武系底部热液喷口及与喷口相关生物群特征.地质论评,51(5):481~492.
姚仲友.1994.甘肃碌曲拉尔玛金矿地质特征及成因探讨.矿床地质,13(1):19~27.
叶永钦,陈友良,赵聪.2015.若尔盖地区510-1铀矿床矿物组合垂直分带特征及找矿意义.矿物学报,35(2):239~244.
张成江,陈友良.2010.510-铀矿床垂直分带规律的发现及其成因意义.地质与勘探,46(3):434~441.
张成立,周鼎武,陆关祥,王居里,王润三.2006.南天山库米什蛇绿混杂岩带中硅质岩的元素地球化学特征及其形成环境.岩石学报,22(1):57~64.
张国伟,孟庆任,赖少聪.1995.秦岭造山带的结构构造.中国科学(B辑),25(9):994~1003.
张国伟,于在平,董云鹏,姚安平.2000.秦岭区前寒武纪构造格局与演化问题探讨.岩石学报,16(1):11~21.
张亚冠,杜远生,徐亚军,余文超,黄虎,焦良轩.2015.湘中震旦纪-寒武纪之交硅质岩地球化学特征及成因环境研究.地质论评,61(3),499~510.
张岩,漆富成,张子龙,李治兴,王文全,杨志强.2015a.降扎铀矿床热水沉积硅质岩的地球化学特征.铀矿地质,31(2):81~88.
张岩,漆富成,张子龙,李治兴,王文全,杨志强.2015b.迭部志留系硅质岩地球化学特征及成因分析.东华理工大学学报(自然科学版),38(4):375~460.
张字龙,漆富成,付锦,何中波,王文全,苏香丽,李治兴.2011.迭部矿田成矿地质条件及资源量扩大方向分析.铀矿地质,27(5):258~264.
郑明华,刘家军.1993.西秦岭南亚带金一铜一铀成矿带中硅岩的海底喷流沉积特征研究.成都理工大学学报,20(2):9~16.
周遗军,何国琦,张秀琴,李己华.2000.川、陕、甘三角区构造与金矿成矿.矿床地质,21(增刊):319~322.
周永章,付伟,杨志军,何俊国,聂凤军,李,赵文霞.2008.藏南地区中生代硅质岩的地球化学特征及其成因意义.岩石学报,24(3):600~608.
Baldwin G J,Thurston P C,Kamber B S.2011.High-precision rare earth element,nickel,and chromium chemistry of chert microbands pre-screened with in-situ analysis.Chemical Geology,285:133~143.
Bau M,Alexander B W.2009.Distribution of high field strength elements(Y,Zr,REE,Hf,Ta,Th,U)in adjacent magnetite and chert bands and in reference standards FeR-3and FeR-4from the Temagami iron-formation,Canada,and the redox level of the Neoarchean ocean.Precambrian Research,174:337~346
Bostrom K.1973.Provenance and accumulation rates of opaline silica:Al,Fe,Mn,Cu,Ni,and Co in Pacific pelagic sediment.Chemical Geology,11:123~148.
Boynton W V,1984.Cosmochemistry of the Rare Earth Elements.In:Henderson P ed.Rare Earth Element Geochemistry.Developments in Geochemistry 2.Elsvier,Amsterdam,63~114.
Bruce M C,Percival I G.2014.Geochemical evidence for provenance of Ordovician cherts in southeastern Australia.Australian Journal of Earth Sciences,61:927~950.
Calvert S E,Pedersen T F.1993.Geochemistry of Recent Oxic and Anoxic Marine Sediments:Implications for the Geological Record.Marine Geology,113:67~88.
Carbonnea J,Robertb M F,Chaussidonc M.2014.The silicon and oxygen isotope compositions of Precambrian cherts:A record of oceanic paleo-temperatures?Precambrian Research,247:223~234.
Chen Youliang,Hou Mingcai,Zhu Xiyang,Zhao Jianbo,2007.Petrology and genesis of ore-bearing rock series in the Zoige uranium ore field,Sichuan,China.Journal of Chengdu University(Natural Science Edition),34(5):553~558(in Chinese with English abstract).
Cheng Lixue,Wang Yuanjun,Chen Hongde,Wang Yue,Zhong Yijiang,2013.Sedimentary and burial environment of black shales of Sinian to Early Palaeozoic in Upper Yangtze region.Acta Petrologica Sinica,29(8):2906~2912(in Chinese with English abstract).
Ding Tiping,Jiang Shaoyong,Wan Defang,Li Yanhe,Li Jincheng,Song Hebing,Liu Zhijian,Yao Xiaonei,1988.Silicon Isotope Geochemistry.Beijing:Geology Publishing House(in Chinese),31~42.
Ding Tiping,Wan Defang,Li Jincheng,Jiang Shaoyong,Song Hebing,Li Yanhe,Liu Zhijian,1988.The analytical method of silicon isotopes and its geological application.Mineral Deposits,7(4):90~95(in Chinese with English abstract).
Ding Zhenju,and Liu Congqiang,2000b.Bikou group developed ancient hydrothermal system from REE evidence of iron riched chert.Progress in Natural Science,10(5):427~434(in Chinese with English abstract).
Ding Zhenju,Liu Congqiang,Yao Shuzhen,Zhou Zonggui,2000a.Rare earth elements compositions of high temperature hydrothermal fluids in seafloor and control factors.Advance in Earth Sciences),15(3):307~312(in Chinese with English abstract).
Du Yuansheng,Sheng Jihu,Feng Qinglai,Wang Zhiping,Gu Songzhu,1998.New recognition of Non-Smith stratigraphy and paleoceanography of Mianxian-Lueyang paleosuture in Southern Qinling,China.Geoscience,12(1):26~31(in Chinese with English abstract).
Elderfield H,Greaves M J.1982.The rare earth elements in seawater.Nature,296,214~219.
Emerson S R,Huested,S S.1991.Ocean Anoxia and the Concentration of Molybdenum and Vanadium in Seawater.Marine Chemistry,34:177~196.
Feng Shengbin,Zhou Hongrui,Yan Changhai,Peng Yi,Yuan Xiaoqi,He Jing,2007.Geochemical characteristics of hydrothermal cherts of Erlangping Group in East Qinling and their geologic significance.Acta Sedimentologica Sinica,25(4):564~573(in Chinese with English abstract).
Garbán G,Martínez M,Márquez G.2017.Geochemical signatures of bedded cherts of the upper La Luna Formation in Táchira State,western Venezuela:Assessing material provenance and paleodepositional setting.Sedimentary Geology,347:130~147.
He Junguo,Zhou Yongzhang,Li Hongzhong.2011.Study on Geochemical Characteristics and Depositional Environment of Pengcuolin Chert,Southern Tibet.Journal of Geography and Geology,3(1):178~188.
He Junguo,Zhou Yongzhang,Yang Zhijun,Li Hongzhong,Wang Xiaoyue,2009.Study on geochemical characteristics and depositional environment of Pengcuolin chert,Southern Tibet.Journal of Jilin University(Earth Science Edition),39(6):1055~1065(in Chinese with English abstract).
He Xinyi,Chen Jianqiang,1999.Early Silurian Rugose Coral Fauna of Tewo area,West Qinling.Acta Palaeontologica Sinica,38(4):423~434(in Chinese with English abstract).
Hecht A D,Savin S M.1970.Oxygen-18 studies of recent planktonic Foraminifera:comparisons of phenotypes and of test parts.Science,170(3953):69~71.
Hoyle J,Elderfield H,Gledhill A,Greaves M.1984.Thebehavior of the rare~earth elements during the mixing of river and sea waters.Geochimica et Cosmochimica Acta,48,143~149.
Hu Jianmin,Meng Qingren,Bai Wuming,Zhao Guochun,2002.Mid-Late Paleozoic extension of the Wudang block in the South Qinling tectonic belt,China.Regional Geology of China,21(8~9):471~477(in Chinese with English abstract).
Huang Hu,Du Yuansheng,Huang Zhiqiang,Yang Jianghai,Huang Hongwei,Xie Chunxia,Hu Lisha.2013.Depositional chemistry of chert during late Paleozoic from western Guangxi and its implication for the tectonic evolution of the Youjiang Basin.Science in China:Series D Earth Sciences,56(3):479~493.
Ikeda M,Tada R,Sakuma H.2010.Astronomical cycle origin of bedded chert:A middle Triassic bedded chert sequence,Inuyama,Japan.Earth and Planetary Science Letters,297:369~378.
Jin Youzhong,Tian Wenhao,2011.An analysis of metallogenic conditions and resource of the Zoige uranium deposit.Geology in China,38(3):681~691(in Chinese with English abstract).
Kakuwa Y,Webb J.2010.Evolution of Cambrian to Ordovician trace fossils in pelagic deep-sea chert,Australia.Australian Journal of Earth Sciences,57:615~625.
Kang Jianli,Zhang Zhaochong,Zhang Dongyang,Hang He,Dong Shuyu,Zhang Su.2011.Geochronology and Geochemistry of the Radiolarian Cherts of the Madar’er Area,Southwestern Tianshan:Implications for Depositional Environment.Acta Geologica Sinica(English Edition),85(4):801~813.
Kemkin I V,Kemkina1 R A.2015.Depositional Environment of Cherts of the Sikhote~Alin Region(Russia Far East):Evidence from Major,Trace and Rare Earth Elements Geochemistry.Journal of Earth Science,26(2):259~272.
Klinkhammer G P,Elderfield H,Edmond J M,Mitra A.1994.Geochemical implications of rare earth element patterns in hydrothermal fluids from mid-ocean ridges.Geochimica et Cosmochimica Acta,58(23):5105~5113.
Klinkhammer G P,Elderfield H,Edmond J M,Mitra A.1994.Geochemical implications of rare earth element patterns in hydrothermal fluids from mid-ocean ridges.Geochimica et Cosmochimica Acta,58(23),5105~5113.
Krings M,Taylor T N.2015.A fungal reproductive unit from the Lower Devonian Rhynie chert(Aberdeenshire,Scotland)that demonstrates an unusual hyphal investment pattern.Scottish Journal of Geology,51:131~139.
Ledevin M,Arndt N,Simionovici A.2014.Silica precipitation triggered by clastic sedimentation in the Archean:New petrographic evidence from cherts of the Kromberg type section,South Africa.Precambrian Research,255:316~334.
Lewis K H,Garwood R J,Brasier M D,Goral T,Jiang H,McLoughlin N,Wacey D.2016.Carbonaceous microstructures from sedimentary laminated chert within the 3.46 Ga Apex Basalt,Chinaman Creek locality,Pilbara,Western Australia.Precambrian Research,278:161~178.
Li Hongzhong,Zhou Yongzhang,Yang Zhijun,He Junguo,Ma Zhanwu,Li Wenchao,Zhou Guofu,An Yanfei,Li Wen,Liang Jin,Wang Chi,2010.A study of micro-area compositional characteristics and the evolution cherts from Bafangshan-Erlihe Pb-Zn ore deposition Western Qinling Orogen.Earth Science Frontiers,17(4):290~298(in Chinese with English abstract).
Li Hongzhong,Zhou Yongzhang,Yang Zhijun,Zhou Guofu,He Junguo,Ma Zhanwu,Li Wenchao,Liang Jin,Li Wen,2011.Diagenesis and metallogenesis evolution of chert in west Qinling Orogenic Belt:A case from Bafangshan-Erlihe Pb-Zn ore deposit.Journal of Jilin University(Earth Science Edition),41(3):715~723(in Chinese with English abstract).
Li Hongzhong,Zhou Yongzhang,YangZhijun,GuZhihong,Lu Wenchao,He Junguo,Li Wen,An Yanfei,2009.Geochemical characteristics and their geological implications of cherts from Bafangshan-Erlihe area in western Qingling orogeny.Acta Petrologica,25(11):3094~3102(in Chinese with English abstract).
Li Xianhua,2000.Geochemistry of the Late Paleozoic radiolarian cherts within the NE Jiangxi ophiolite melange and its tectonic significance.Science in China:Series D Earth Sciences(English edition),30(3):1~5.
Li Yanhe,Ding Tiping,Wan Defang,1995.Experimental study of silicon isotope dynamic fractionation and its geological application.Chinese Journal of Geochemistry,13(3):282~288(in Chinese with English abstract).
Liang Bin,Feng Qinglai,Wang Quanwei,Guo Jianqiu,Zhong Changhong,Li Zhenjing.2005.Ladinian radiolarian,siliceous rock from the Xianshuihe Belt,West Sichuan and their tectonic significance.Science in China:Series D Earth Sciences,48(1):42~47.
Lin Li,Zhu Lidong,Zhu Dicheng,1998.Study of molecular paleontology in thermal chert in Laerma gold deposit of West Qinling.Earth Science-Journal of China University of Geosciences,23(5):503~507(in Chinese with English abstract).
Liu Hanbin,Jin Guishan,Li Junjie,Han Juan,Zhang Jianfeng,Zhang Jia,Zhong Fangwen,Guo Dongqiao,2013.Determination of stable isotope composition in uranium geological samples.World Nuclear Geoscience,30(3):174~179(in Chinese with English abstract).
Liu Jiajun,Feng Caixia,Liu Jianming,Zheng Minghua,Li Chaoyang,2004.Reidentification of the ore-hosted strata age and metallogenic age of the strata bound Au~Se deposits,the Western Qinling mountains.Earth Science Frontiers,11(2):435~443(in Chinese with English abstract).
Liu Jiajun,Zheng Minghua,Liu Jianming,Zhou Yufeng,Gu Xuexiang,Zhang Bin,1999.The geological and geochemical characteristics of Cambrian chert and their sedimentary environmental implications in western Qinling.Acta Petrologica Sinica,15(1):145~154(in Chinese with English abstract).
Liu Shuwen,Xue Chunji,Zeng Rong,Li Qiang,Zhu Jingxiang,Wang Tao,Zhao Guobin,2005.Petrology and geochemistry of siliceous rocks in Silurian lead-zinc deposits of southern Qinling region.Mineral Deposits,24(5):490~500(in Chinese with English abstract).
Lu Songnian,Yu Haifeng,Li Huaikun,Chen Zhihong,Wang Huichu,Zhang Chuanlin,Xiang Zhenqun.Early Paleozoic suture zones and tectonic divisions in the“Central China Origen”.Geological Bulletin of China,2006,25(12):1368~1380(in Chinese with English abstract).
Lu Zhicheng,Liu Congqiang,Liu Jiajun,Wu Fengchang,2004.Geochemical Studies on the Lower Cambrian Witherite-bearing Cherts in the Northern Daba Mountains.Acta Geologica Sinica,78(3):390~406(in Chinese with English abstract).
Lyons T W,Werne J P.,David J H,Murray R W.2003.Contrasting sulfur geochemistry and Fe/Al and Mo/Al ratios across the last oxic-to-anoxic transition in the Cariaco Basin,Venezuela.Chemical Geology,195:131~157.
Mao Liguang,Xiao Ancheng,Wei Guoqi,Shen Zhongyan,Wang Liang,Zhang Lin,Qian Junfeng,2011.Distribution and origin of the Late Paleozoic~Mesozoic rift systems in the northern margin of theYangtze block.Acta Petrologica Sinica,27(3):721~731(in Chinese with English abstract).
Marchig V.1982.Some geochemistry indicators for discriminational between diagenetic andhydrothermal metalliferous sediments.Marine Geology,58(3):241~256.
Marin-Carbonne J,Chaussidon M,Boiron M C,Robert F.2011.Acombined in situ oxygen,silicon isotopic and fluid inclusion study of a chert sample from Onverwacht Group(3.35 Ga,South Africa):New constraints on fluid circulation.Chemical Geology,286:59~71.
Marshall C P,Emry J R,Marshall A O.2011.Haematite pseudomicrofossils present in the 3.5-billion-year-old Apex Chert.Nature Geoscience,1~4.
Michard A.1989.Rare earth ekment systematics in hydrothermalfluids.Geochimica et Cosmochimica Acta,53:745~750.
Miroshnichenko N V,Perevoznikova Y V.2010.The Intermetallic Compound Ni3Au and Gold-Nickel Solid Solutions in Metalliferous Sediments of the Triassic Chert Formation in Sikhote-Alin in the Far East.Russian Journal of Pacific Geology,4(1):56~62.
Morford J L,Emerson S.1999.The Geochemistry of Redox Sensitive Trace Metals in Sediments.Geochimica et Cosmochimica Acta,63:1735~1750.
Murray R W.1994.Chemical criteria to identify the depositionalenvironment of chert:general principles and application.Sediment Geology,90:213~232.
Murry R W,Buchholtz T,Brink M R,Gerlach D C,Russ G P,Jones D L.1990.Rare earth elements as indicators of different marine depos-itional environments in chert and shale.Geology,18:268~271.
Murry R W,Buchholtz T,Brink M R,Gerlach D C,Russ G P,Jones D L.1991.Rare earth,major,and trace elements in chert from Franciscan Complex and Monterey Group:Assessing REE sources to fine-grained marine sediments.Geochimica et Cosmochimica Acta,55:1875~1895.
Qi Fucheng,Zhang Zilong,Li Zhixing,He Zhongbo,Wang Wenquan,2012.Temporal and spatial evolution pattern of Carbonaceous-Siliceous argillaceous rock type uranium deposits in China.Uranium Geology,28(2):65~71(in Chinese with English abstract).
Qi Huawen,Hu Ruizhong,Su Wenchao,Qi Liang,Feng Jiayi.2004.Continental hydrothermal sedimentary siliceous rock and genesis of superlarge germanium(Ge)deposit hosted in coal:Astudy from the Lincang Ge deposit,Yunnan,China.Science in China:Series D Earth Sciences,47(11):973~984.
Qiu Zhen,Wang Qingchen.2011.Geochemical evidence for submarine hydrothermal origin of the Middle-Upper Permian chert in Laibin of Guangxi,China.Science in China:Series DEarth Sciences,54(7):1011~1023.
Ran Bo,Liu Shugen,Jansa Lubab,Wei Sun,Yang Di,Ye Yuehao,Wang Shiyu,Luo Chao,Zhang Xuan,Zhang Changjun.2015.Origin of the Upper Ordovician-lower Silurian cherts of the Yangtze block,South China,and their palaeogeographic significance.Journal of Asian Earth Sciences,108:1~17.
Rona P A.1978.Criteria for recognition of hydrothermal mineral deposits in ocean crust.Economic Geology,73(2):135~160.
Rong Jiayu,ChenXu,Su Yangzheng,Zhan Renbin,Ni Yunan,Zhan Renbin,Cheng Tingen.2003.Silurian paleogeography of China[M]//Landing E,Johnson M.E.Silurian Landsand Seas:Paleogeography,Outside of Laurentia.New York:New York State Museum Bulletin,493:243~298.
Rouchon V,Orberger B.2008.Origin and mechanisms of K-Simetasomatism of ca.3.4-3.3 Ga volcaniclastic deposits and implications for Archean seawater evolution:Examples from cherts of Kittys Gap(Pilbara craton,Australia)and Msauli(Barberton Greenstone Belt,South Africa).Precambrian Research,165:169~189.
Sato T,Isozaki Y,Shozugawa K.2011.57Fe Mosbauer spectroscopic analysis of deep-sea pelagic chert:Effect of secondary alteration with respect to paleo-redox evaluation.Journal of Asian Earth Sciences,42:1403~1410.
Shen B,Lee C A.,Xiao S.2011.Germanium/silica ratios in diagenetic chert nodules from the Ediacaran Doushantuo Formation,South China.Chemical Geology,280:323~335.
Sheng Jihu,Du Yuansheng,Feng Qinglai,Xu Jifeng,1997.Depositional environments of cherts in the ophiolite melange belt from Mian-Lue,Shanxi Province.Earth Science-Journal of China University of Geosciences,22(6):599~602(in Chinese with English abstract).
Sholkovitz E R.1988.Rare earth elements in the sediments of the North Atlantic Ocean,Amazon Delta,and East China Sea;reinterpretation of terrigenous input patterns to the oceans.American Journal of Science,288(3),236~281.
Shu Liangshu,2010.Physical Geology(third edition).Beijing:Geology Publishing House,1~292(in Chinese).
Song Tianrui,Ding Tiping,1989.A new probe of application of Silicon isotopic(δ30Si)in siliceous rocks to sedimentary facies analysis.Chinese Science Bulletin,34(18):1408~1411(in Chinese with English abstract).
Sun ShengLi,Chen Jianfa,Zheng Jianjing,Liu Wenhui.2009.The noble gas isotope geochemical composition of chert at the bottom of Cambrian in Tarim Basin,China.Science in China:Series D Earth Sciences,52:115~119.
Tayloy S R,Mclennan S M.1981.The composition and evolution of the continental crust:rare earth element evidence from sedimentary rocks.Phil.Trans.R.Soc.London,A301,381~399.
Tayloy S R,Mclennan S M.1981.The composition and evolution of the continental crust:rare earth element evidence from sedimentary rocks.Phil.Trans.R.Soc.London,A301,381~399.
Tekin U K,Goncuoglu M C.2009.Late Middle Jurassic(Late Bathonian-Early Callovian)Radiolarian Cherts from the Neotethyan Bornova Flysch Zone,Spil Mountains,Western Turkey.Geologicheskaya Korrelyatsiya,17(3):70~80.
Tessalina1SG,Bourdon B,Kranendonk M V.2010.Influence of Hadean crust evident in basalts and cherts from the Pilbara Craton.NATURE GEOSCIENCE,3:214~217.
Thassanapak H,Mongkol U,Chonglakmani C,Feng Q.2011.Geochemistry of Middle Triassic Radiolarian Cherts from Northern Thailand:Implication for Depositional Environment.Journal of Earth Science,22(6):688~703.
Thomson J,Higgs N C,Croudace I W,Colley S,Hydes D J,1993.Redox Zonation of Elements at an Oxic/Post-Oxic Boundary in Deep-Sea Sediments.Geochimica et Cosmochimica Acta,57:579~595.
Tribovillard N,Algeo T J,Lyons T,Riboulleau A.2006.Trace Metals as Paleoredox and Paleoproductivity Proxies:An Update.Chemical Geology,232:12~32.
Udchachon M,Thassanapak H,Feng Q.2011.Geochemical constraints on the depositional environment of Upper Devonian radiolarian cherts from Loei,north-eastern Thailand.Front.Earth Sci.5(2):178~190.
Wang Nianzhong,Wang Junqing,Zhang Guorui,1998.The first discovery of Silurian and Early Devonian Acanthodians from Zoige and Tewo counties,West Qinling mountains.Vertebrata Palasiatica,36(4):268~281(in Chinese with English abstract).
Wang Xinwei,Wo Yujin,Zhang Rongqiang,2008.Tectonicsedimentary cycle of the Yangtze Craton from Nanhuaan to the Early Palaeozoic.Geoscience,22(4):525~533(in Chinese with English abstract).
Wang Zongqi,Yan Quanren,Yan Zhen,Wang Tao,Jiang Chunfa,Gao Lianda,Li Qiugen,Chen Junlu,Zhang Yingli,Liu Ping,Xie Chunlin,Xiang Zhongjin,2009.New division of the main tectonic units of the Qinling Orogenic Belt,Central China.Acta Geologica Sinica,83(11):1527~1546(in Chinese with English abstract).
Wen Hanjie,Fan Haifeng,Tian Shihong,Wang Qilian,Hu Ruizhong,2016.The formation conditions of the early Ediacaran cherts,South China.Chemical Geology,430:45~69.
Wen Hanjie,Fan Haifeng,Tian Shihong,Wang Qilian,Hu Ruizhong.2016.The formation conditions of the early Ediacaran cherts,South China.Chemical Geology,430:45~69.
Xiang Lei,Cai Chunfang,He Xunyun,Jiang Lei,Yuan Yuyang,Yu Lei,2016.Evolution of redox state during the Terreneuvian epoch at Zhalagou section,South China.Acta Geologica Sinica,24(3):600~608(in Chinese with English abstract).
Xiang Lei,Cai Chunfeng,He Xunyun,Jiang Lei.2012.The mechanisms for the enrichment of trace elements in the Lower Cambrian black chert successions from Zhalagou section,Guizhou Province.Acta Petrologica Sinica,28(3):971~980(in Chinese with English abstract).
Xiao Shuhai,Schiffbauer James D.,McFadden Kathleen A.,et al.2010.Petrographic and SIMS pyrite sulfur isotope analyses of Ediacaran chert nodules:Implications for microbial processes in pyrite rim formation,silicification,and exceptional fossil preservation Earth and Planetary Science Letters,297:481~495.
Xie Xiaomin,Tenger,Qian Jianzhong,Zhang Qingzhen,Bian Lizeng,Yin Leiming,2015.Depositional environment,organisms components and source rock formation of siliceous rocks in the base of the Cambrian Niutitang Formation,Kaili,Guizhou.Acta Geologica Sinica,89(2),425~439(in Chinese with English abstract).
Xue Chunji,Jiang Shaoyong,Li Yanhe,1998.Devonian chert Silicon,Oxygen isotope geochemical study,Qinling.Journal of Xi’an Engineering University,20(1):10~13(in Chinese with English abstract).
Yamamoto K.1987.Geochemical characteristics and depositional environnlents of cherts and associated rocks in the Franciscan and Shimanto lerrenes.Sedimentary Geology,52:65~108.
Yang Liqiang,Ji Xingzhong,Santosh M.,Li Nan,Zhang Zhichao,Yu Jinyuan.2015.Detrital zircon U-Pb ages,Hf isotope,and geochemistry of Devonian chert from the Mianlue suture:Implications for tectonic evolution of the Qinling orogeny.Journal of Asian Earth Sciences,113:589~609.
Yang Ruidong,Wei Huairui,Bao Miao,Wang Wei,Wang Qiang,2007.Submarine Hydrothermal venting-flowing sedimentary characters of the Cambrian Shanggongtang and Dahebian barite deposits,Tianzhu County,Guizhou Province.Geological Review,53(5):675~680.
Yang Ruidong,Zhang Chuanlin,Luo Xing Rong,Tian Jingquan,Bao Yafan,Song Guoqi,2006.Geochemical Characteristics of Early Cambrian Cherts in Quruqtagh,Xinjiang,West China.Acta Geologica Sinica,80(4):598~605.
Yang Ruidong,Zhu Lijun,Gao Hui,Zhang Weihua,Jiang Lijun,Wang Qiang,Bao Miao,2005.Yang R,Zhu L,Gao H,et al.A study on characteristics of the hydrothermal vent and relating biota at the Cambrian bottom in Songlin,Zunyi County,Guizhou Province.Geological Review,51(5):481~492.
Yao Chunyan,Ma Dongsheng,Ding Haifeng,Zhang Xiaoyong,Huang Hui.2014.Trace elements and stable isotopic geochemistry of an Early Cambrian chert-phosphorite unit from the lower Yurtus Formation of the Sugetbrak section in the Tarim Basin.57(3):454~464
Yao Zhongyou,1994.A preliminary discussion on geological characteristics and genesis of the Laerma gold deposit in Luqu county,Gansu province.Mineral Deposits,13(1):19~27(in Chinese with English abstract).
Ye Yongqin,Chen Youliang,Zhao Cong,2015.Vertical zoning features of the mineral assemblages in the Zoige 510-1uranium deposit and its prospecting significance.Acta Mineralogica Sinica,35(2):239~244(in Chinese with English abstract).
Yin Leiming,Borjiginb Tenger,Knollc Andrew H.,Bian Lizeng,Xie Xiaomin,Bao Fang,Ou Zhiji.2016.Sheet-like microfossils from hydrothermally influenced basinal cherts of thelower Cambrian(Terreneuvian)Niutitang Formation,Guizhou,South China.Palword,350:1~11.
Yu Bingsong,Dong Hailiang,Widom Elisabeth.2009.Geochemistry of basal Cambrian black shales and cherts from the Northern Tarim Basin,Northwest China:Implications for depositional setting and tectonic history.Journal of Asian Earth Sciences,34:418~436.
Zhang Chengjiang,Chen Youliang,2010.Discovery of vertical zoning in the 510-1 uranium deposit and its geological implications.Geology and Explomolar ratiosn,46(3):434~441(in Chinese with English abstract).
Zhang Chengli,Gao Shan,Zhang Guowei,Guo Anlin,Yuan Honglin,Liu Xiaoming,Wang Jianqi.2004.Geochemistry of ophiolite cherts from the Qinling orogenic belt and implications for their tectonic settings.Science in China:Series D Earth Sciences,47(4):329~337.
Zhang Chengli,Gao Shan,Zhang Guowei,Liu Xiaoming,Yu Zaiping.2003.Geochemistry of early Paleozoic alkali dyke swarms in south Qinling and its geological significance.Science in China:Series D Earth Sciences,46(12):1292~1306.
Zhang Chengli,Zhou Dingwu,Lu Guanxiang,Wang Juli,Wang Ruisan,2006.Geochemical characteristics and sedimentary environments of cherts from Kumishi ophiolitic mélange in southern Tianshan.Acta Petrologica Sinica,22(1):57~64(in Chinese with English abstract).
Zhang Guowei,Dong Yunpeng,Lai Shaocong,2004.Mianlue tectonic zone and Mianlue suture zone on southern margin of Qinling-Dabie orogenic belt.Science in China:Series D Earth Sciences(English edition),47:300~316.
Zhang Guowei,Meng Qingren,Lai Shaocong,1995.Structure and tectonics of the Qinling Orogenic belt.Science in China.(Series B),25:994~1003(in Chinese with English abstract).
Zhang Guowei,Meng Qingren,Yu Zaiping,Sun Yong,Zhou Dingwu,Guo Anlin,1996.Orogenesis and dynamics of Qinling orogen.Science in China:Series D Earth Sciences(English edition),26:193~200.
Zhang Guowei,Yu Zaiping,Dong Yunpeng,Yao Anlin,2000.On Precambrian framework and evolution of the Qinling belt.Acta Petrologica Sinica,16:11~21(in Chinese with English abstract).
Zhang Yaguan,Du Yuansheng,Xu Yajun,Yu Wenchao,Huang Hu,Jiao Liangxuan,2015.Geochemical characteristics of siliceous rocks during the transition from Sinian(Ediacaran)to Cambrian in central Hunan and its implication for genesis and sedimentary environment..Geological Review,61(3),499~510(in Chinese with English abstract).
Zhang Yan,Qi Fucheng,Zhang Zilong,Li Zhixing,Wang Wenquan,Yang Zhiqiang,2015a.Geochemical Characteristics of Hot Water Deposited Siliceous Rock in Jiangzha Uranium Deposit.Uranium Geology,31(2):81~88(in Chinese with English abstract).
Zhang Yan,Qi Fucheng,Zhang Zilong,Li Zhixing,Wang Wenquan,Yang Zhiqiang,2015b.Geochemical characteristics and genesis analysis of the Silurian siliceous rock in Diebu.Journal of East China Institute of Technology,38(4):375~460(in Chinese with English abstract).
Zhang Zilong,Qi Fucheng,Fu Jin,He Zhongbo,Wang Wenquan,Su Xiangli,Li Zhixing,2011.Analysis on geological conditions and orientaion of uranium explomolar ratiosn in Diebu ore field.Uranium Geology,27(5):257~264(in Chinese with English abstract).
Zheng Minghua,Liu Jiajun,1993.On the submarine exhalative sedimentation nature of silicalites from the gold-copper-uranium metallogenic belt in the south subzone of Western Qinling.Journal of Chengdu University(Natural Science Edition),20(2):9~16(in Chinese with English abstract).
Zhou Yijun,He Guoqi,Zhang Xueqin,Li Jihua,2000.Tectonic and gold mineralization in triangle regional of Chuan-Shan-Gan.Mineral Deposits,21:319~322(in Chinese with English abstract).
Zhou Yongzhang,Fu Wei,Yang Zhijun,He Junguo,Nie Fengjun,Li Wen,Zhao Wenxia,2008.Microfabrics of chert from Yarlung Zangbo Suture Zone and southern Tiebet and its geological implications.Acta Petrologica Sinica,24(3):600~608(in Chinese with English abstract).
Zhu Jie,Du Yuansheng,Liu Zaoxue,Feng Qinglai,Tian Wangxue,Li Jinping,Wang Changping.2006.Mesozoic radiolarian chert from the middle sector of the Yarlung Zangbo suture zone,Tibet and its tectonic implications.Science in China:Series DEarth Sciences,49(4):348~357.
陈友良,侯明才,朱西养,赵剑波.2007.若尔盖铀矿田含矿岩系的岩石特征及成因探讨.成都理工大学学报(自然科学版),34(5):553~558.
程立雪,王元君,陈洪德,王约,钟怡江.2013.上扬子地区震旦系-早古生界黑色页岩的沉积和埋藏环境.岩石学报,29(8):2906~2912.
丁悌平,蒋少涌,万德芳,李金城,宋鹤彬,刘志坚.1994.硅同位素地球化学.北京:地质出版社,31~42.
丁悌平,万德芳,李金城,蒋少涌,宋鹤彬,李延河,刘志坚.1988.硅同位素测量方法及其地质应用.矿床地质,7(4):90~95.
丁振举,刘丛强,姚书振,周宗桂.2000a.海底热液系统高温流体的稀土元素组成及其控制因素.地球科学进展,15(3):307~312.
丁振举,刘丛强.2000b.碧口群古热水系统发育的富铁硅岩稀土元素地球化学证据.自然科学进展,10(5):427~434.
杜远生,盛洁虎,冯庆来,王治平,顾松竹.1998.南秦岭勉略古缝合带非史密斯地层和古海洋新知.现代地质,12(1):26~31.
冯胜斌,周洪瑞,燕长海,彭翼,袁效奇,贺静.2007.东秦岭二郎坪群硅质岩热水沉积地球化学特征及其地质意义.沉积学报,25(4):564~573.
何俊国,周永章,杨志军,李红中,王晓悦.2009.藏南彭错林硅质岩地球化学特征及沉积环境分析.吉林大学学报:地球科学版,39(6):1055~1065.
何心一,陈建强.1999.西秦岭迭部地区早志留世四射珊瑚动物群.古生物学报,38(4):423~434.
胡健民,孟庆任,白武明,赵国春.2002.南秦岭构造带中-晚古生代伸展构造作用.地质通报,21(8~9):471~477.
金有忠,田文浩.2011.若尔盖铀矿田成矿地质条件及资源潜力分析.中国地质,38(3):681~691.
李红中,周永章,杨志军,古志宏,吕文超,何俊国,李文,安燕飞.2009.秦岭造山带西段八方山-二里河地区硅质岩的地球化学特征及其地质意义.岩石学报,25(11):3094~3102.
李红中,周永章,杨志军,何俊国,马占武,吕文超,周国富,安燕飞,李文,梁锦,王驰.2010.西秦岭八方山-二里河Pb-Zn矿区硅质岩的微区成分特征及演化.地学前缘,17(4):290~298.
李红中,周永章,杨志军,周国富,何俊国,马占武,吕文超,李文,梁锦,卢文姬.2011.西秦岭造山带硅质岩的成岩成矿演化特征-以八方山-二里河矿区赋矿硅质岩为例.吉林大学学报,41(3):715~723.
李献华.2000.赣东北蛇绿混杂岩带中硅质岩的地球化学特征及构造意义.中国科学(D辑),30(3):1~5.
李延河,丁悌平,万德芳.1994.硅同位素动力学分馏的实验研究及其地质应用.矿床地质,13(3):282~288.
林丽,朱利东,朱弟成.1998.西秦岭拉尔玛金矿热水硅质岩中的分子古生物学研究.地球科学,23(5):503~507.
刘汉彬,金贵善,李军杰,韩娟,张建锋,张佳,钟芳文,郭东侨.2013.铀矿地质样品的稳定同位素组成测试方法.世界核地质科学,30(3):174~179.
刘家军,冯彩霞,刘建明,郑明华,李朝阳.2004.西秦岭南亚带层控金硒矿床的赋矿地层年代与成矿时代.地学前缘,11(2):435~443.
刘家军,郑明华,刘建明,何俊国,马占武,吕文超,周国富,安燕飞,李文,梁锦,王驰.1999.西秦岭寒武系金矿床中硅岩的地质地球化学特征及其沉积环境意义.岩石学报,15(1):145~154.
刘淑文,薛春纪,曾荣,李强,朱经祥,王涛,赵国斌.2005.南秦岭志留纪铅锌矿床中硅质岩岩石学及地球化学.矿床地质,24(5):490~500.
陆松年,于海峰,李怀坤,陈志宏,王惠初,张传林,相振群.2006.“中央造山带”早古生代缝合带及构造分区概述.地质通报,25(12):1368~1380.
吕志成,刘丛强,刘家军,吴丰昌.2004.北大巴山下寒武统毒重石矿床赋矿硅质岩地球化学研究.地质学报,78(3):390~406.
毛黎光,肖安成,魏国齐,沈中延,王亮,张林,钱俊锋.2011.扬子地块北缘晚古生代-早中生代裂谷系统的分布及成因分析.岩石学报,27(3):721~731.
孟庆任,张国伟,于在平,梅志超.1996.秦岭南缘晚古生代裂谷-有限洋盆沉积作用及构造演化.中国科学(D辑),26(增刊):28~33.
漆富成,张字龙,李治兴,何中波,王文全.2012.中国碳硅泥岩型铀矿床时空演化规律.铀矿地质,28(2):65~71.
胜吉虎,杜远生,冯庆来,许继锋.1997.南秦岭勉略蛇绿混杂岩带硅质岩沉积环境研究.地球科学,22(6):599~602.
舒良树.2010.普通地质学.第三版.北京:地质出版社,1~292.
宋天锐,丁悌平.1989.硅质岩的硅同位素(δ30Si)应用于沉积相分析的新尝试.科学通报,34(18):1408~1411.
汪新伟,沃玉进,张荣强.2008.扬子克拉通南华纪-早古生代的构造-沉积旋回.现代地质,22(4):525~533.
王念忠,王俊卿,张国瑞,王世涛.1998.西秦岭若尔盖、迭部志留纪和早泥盆世棘鱼类的首次报道-西秦岭志留纪和泥盆纪脊椎动物研究之一.古脊椎动物学报,36(4):268~281.
王宗起,闫全人,闫臻,王涛,姜春发,高联达,李秋根,陈隽璐,张英利,刘平,谢春林,向忠金.2009.秦岭造山带主要大地构造单元的新划分.地质学报,83(11):1527~1546.
向雷,蔡春芳,贺训云,姜磊,袁余洋,于雷.2016.华南渣拉沟剖面纽芬兰世沉积水体氧化还原状态演化.地质学报,89(6),1120~1133.
向雷,蔡春芳,贺训云,姜磊.2012.贵州渣拉沟剖面下寒武统黑色硅质岩微量元素富集机制.岩石学报,28(3):971-980.
谢小敏,腾格尔,秦建中,张庆珍,边立曾,尹磊明.2015.贵州凯里寒武系底部硅质岩系生物组成、沉积环境与烃源岩发育关系研究.地质学报,89(2),425~439.
薛春纪,蒋少勇,李延河.1998.秦岭泥盆纪硅质岩硅、氧同位素地球化学研究.西安工程学院学报,20(1):10~13.
杨瑞东,魏怀瑞,鲍淼,王伟,王强.2007.贵州天柱上公塘-大河边寒武纪重晶石矿床海底热水喷流沉积结构、构造特征.地质论评,53(5):675~680.
杨瑞东,张传林,罗新荣,田敬全,包亚范,宋果奇,2006.新疆库鲁克塔格地区早寒武世硅质岩地球化学特征及其意义.地质学报,80(4):598~605.
杨瑞东,朱立军,高慧,张位华,姜立君,王强,鲍淼.2005.贵州遵义松林寒武系底部热液喷口及与喷口相关生物群特征.地质论评,51(5):481~492.
姚仲友.1994.甘肃碌曲拉尔玛金矿地质特征及成因探讨.矿床地质,13(1):19~27.
叶永钦,陈友良,赵聪.2015.若尔盖地区510-1铀矿床矿物组合垂直分带特征及找矿意义.矿物学报,35(2):239~244.
张成江,陈友良.2010.510-铀矿床垂直分带规律的发现及其成因意义.地质与勘探,46(3):434~441.
张成立,周鼎武,陆关祥,王居里,王润三.2006.南天山库米什蛇绿混杂岩带中硅质岩的元素地球化学特征及其形成环境.岩石学报,22(1):57~64.
张国伟,孟庆任,赖少聪.1995.秦岭造山带的结构构造.中国科学(B辑),25(9):994~1003.
张国伟,于在平,董云鹏,姚安平.2000.秦岭区前寒武纪构造格局与演化问题探讨.岩石学报,16(1):11~21.
张亚冠,杜远生,徐亚军,余文超,黄虎,焦良轩.2015.湘中震旦纪-寒武纪之交硅质岩地球化学特征及成因环境研究.地质论评,61(3),499~510.
张岩,漆富成,张子龙,李治兴,王文全,杨志强.2015a.降扎铀矿床热水沉积硅质岩的地球化学特征.铀矿地质,31(2):81~88.
张岩,漆富成,张子龙,李治兴,王文全,杨志强.2015b.迭部志留系硅质岩地球化学特征及成因分析.东华理工大学学报(自然科学版),38(4):375~460.
张字龙,漆富成,付锦,何中波,王文全,苏香丽,李治兴.2011.迭部矿田成矿地质条件及资源量扩大方向分析.铀矿地质,27(5):258~264.
郑明华,刘家军.1993.西秦岭南亚带金一铜一铀成矿带中硅岩的海底喷流沉积特征研究.成都理工大学学报,20(2):9~16.
周遗军,何国琦,张秀琴,李己华.2000.川、陕、甘三角区构造与金矿成矿.矿床地质,21(增刊):319~322.
周永章,付伟,杨志军,何俊国,聂凤军,李,赵文霞.2008.藏南地区中生代硅质岩的地球化学特征及其成因意义.岩石学报,24(3):600~608.