[1]蒲心纯, 周浩达, 王熙林.中国南方寒武纪岩相古地理与成矿作用 [M].北京:地质出版社,1993: 40-100.
[2]Aharon P, Schidlo wski M, Singh I B. Chronostratigraphic markers in the endPrecambrian carbon isotope record of the Lesser Himalaya [J]. Nature, 1987, 327:699-702.
[3]Magaritz M, Holser W T, Kirschvink J L. Carbonisotope events across the Precambrian/Cambrian boundary on the Siberian platform [J]. Nature, 1986, 320: 258-259.
[4]Magaritz M, Kirschvink J L, Latham A J,et al. Precambrian/Cambrian boundary problem: Carbon isotope correlations for Vendian and Tommotian time between Siberia and Morocco [J]. Geology, 1991, 19: 847-850.
[5]Brasier M D. Global oceanatmosphere change across the PrecambrianCambrian transition [J]. Geological Magazine, 1992,129: 161-168.
[6]Brasier M D. Nutrientenriched waters and the early skeletal fossil record [J]. Journal of the Geological Society, London, 1992, 149: 621-629.
[7]Knoll A H, Walter M R. Late Proterozoic stratigraphy and Earth history [J]. Nature, 1992, 356: 673-678.
[8]Kaufman A J, Knoll A H, Semikhatov M A, et al. Integrated chronostratigraphy of ProterozoicCambrian boundary beds in the western Anabar region, northern Siberia [J]. Geological Magazine, 1996, 133: 505-553.
[9]Kaufman A J, Knoll A H. Neoproterozoic variations in the carbon isotopic composition of seawater: stratigraphic and biogeochemical implications [J]. Precambrian Research, 1995, 73: 27-49.
[10]Conway M S, Mcilroy D, Rushton A W A. Lower Cambrian halkieriids from Oxfordshire, UK [J]. Geological Magazine , 1998, 135(4): 501-508.
[11]Xiao S H, Zhang Y, Knoll A H. Threedimensional preservation of algae and animal embryos in a Neoproterozoic phosphorite [J]. Nature, 1998, 291: 553-558.
[12]Shu D G, Luo H L, Conway M S, et al. Lower Cambrian vertebrates from South China [J].Nature, 1999, 402:42-46.
[13]Brasier M D, Shields G. Neoproterozoic chemostratigraphy and correlation of the Port Askaig glaciation, Dalradian Supergroup of Scotland [J]. Journal of the Geological Society, London, 2000, 157: 909-914.
[14]Corsetti F A, Awramik S M, Pierce D, et al. Using chemostratigraphy to correlate and calibrate unconformities in Neoproterozoic strata from the Southern Great Basin of the United States [J]. International Geology Review, 2000, 42:516-533.
[15]Corsetti F A, Hagadorn J W. Precambrian-Cambrian transition: Death Valley, United States [J]. Geology, 2000, 28(4): 299 -302.
[16]Shen Y, Schidlowski M. New C isotope stratigraphy from southwest China: Implications for the placement of the Precambrian-Cambrian boundary on the Yangtze Platform and global correlations [J]. Geology, 2000, 28(7): 623-626.
[17]Walter M R, Veevers J J, Calver C R, et al. Dating the 840-544 Ma Neoproterozoic interval by isotopes of strontium, carbon, and sulfur in seawater, and some interpretative models [J]. Precambrian Research, 2000, 100: 371-433.
[18]Melezhik V A, Gorokhov I M, Kuznetsov A B, et al. Chemostratigraphy of the Neoproterozoic carbonates: implications for ‘blind dating’ [J]. Terra Nova, 2001, 13:1-11.
[19]Melezhik V A, Gorokhov I M, Fallick A E, et al. Isotopic shtratigraphy suggests Neoproterozoic ages and Laurentian ancestry for highgrade marbles from the NorthCentral Norwegian Caledonides [J]. Geological Magazine, 2002, 139(4):375-393.
[20]Yuan X L, Xiao S H, Parsley R L, et al. Towering sponges in an Early Cambrian Lagerstatte: Disparity between nonbilaterian and bilaterian epifaunal tierers at the NeoproterozoicCambrian transition [J]. Geology, 2002, 30: 363-366.
[21] Yang R D, Gao H, Wang Q, et al. REE accumulation of the Early Cambrian Gezhongwu Formation phosphorous rocks in Sanjia,Zhijin County, Guizhou Province,China [J]. Journal of Rare Earths, 2005, 23(6):760-767.
[22]Coveney R M, Murowchick J B, Grauch R I , et al. Field relations,origins, and resource implications for platiniferous molybdenumnickel ores in black shales of South China [J]. Exploration and Mining Geology, 1992, 1(1):21-28.
[23]李胜荣, 高振敏. 湘黔地区牛蹄塘组黑色岩系稀土特征——兼论海相热水沉积岩稀土模式[J]. 矿物学报,1995,15(2):225-229.
[24]胡清洁. 新晃贡溪超大型重晶石矿床的岩石学特征与沉积成岩作用 [J]. 湖南地质,1997,16(2):106-111.
[25]Lott D A, Coveney R M, Murowchick J B, et al. Sedimentary exhalative nickelmolybdenum ores in South China [J]. Economic Geology, 1999, 94: 1051-1066.
[26]彭军, 夏文杰, 伊海生. 湖南新晃贡溪重晶石矿床地质地球化学特征及成因分析 [J]. 成都理工学院学报, 1999, 26(1):92-96.
[27]Kao L S, Peacor D R, Coveney Jr R M, et al. A C/MoS2 mixedlayer phase (MoSC) occurring in metalliferous black shales from southern China, and new data on jordisite [J]. American Mineralogist, 2001, 86: 852-861.
[28]Steiner M, Wallis E, Erdtmann B D, et al. Submarinehydrothermal exhalative ore layers in black shales from South China and associated fossilsinsights into a Lower Cambrian facies and bioevolution [J]. Palaeogeography, Palaeoclimatology,Palaeoecology, 2001, 169: 165-191.
[29]Mao J W, Lehmann B, Du A D, et al. ReOs dating of polymetallic NiMoPGEAu mineralization in Lower Cambrian black shales of South China and its geological significance [J]. Economic Geology, 2002, 97: 1051-1061.
[30]Jiang S Y, Yang J H, Ling H F, et al. Extreme enrichment of polymetallic NiMoPGEAu in Lower Cambrian black shales of South China: an Os isotope and PGE geochemical investigation [J]. Palaeogeography, Palaeoclimatology,Palaeoecology, 2007, 254: 217-228.
[31]Kribek B, Korova S, Machovi V, et al. Organic geochemistry and petrography of barren and MoNiPGE mineralized marine black shales of the Lower Cambrian Niutitang Formation (South China) [J]. International Journal of Coal Geology, 2007, 72: 240-256.
[32]Orberger B, Vymazalova A, Wagner C, et al. Biogenic origin of intergrown Mosulphideand carbonaceous matter in Lower Cambrian black shales (Zunyi Formation, southern China) [J]. Chemical Geology, 2007, 238(3/4): 213-231.
[33]吴朝东, 杨承运, 陈其英. 新晃贡溪—天柱大河边重晶石矿床热水沉积成因探讨 [J]. 北京大学学报:自然科学版, 1999, 35(6):774-785.
[34]方维萱, 胡瑞忠, 苏文超, 等. 大河边—新晃超大型重晶石矿床地球化学特征及形成的地质背景 [J]. 岩石学报, 2002, 18(2):247-256.
[35]夏菲, 马东升, 潘家永, 等. 贵州天柱大河边和玉屏重晶石矿床热水沉积成因的锶同位素证据 [J]. 科学通报, 2004, 49(24):2592-2595.
[36]夏菲, 马东升, 潘家永, 等.天柱大河边—新晃重晶石矿床矿物组成特征的电子探针研究 [J]. 矿物学报, 2005, 25(3):289-294.
[37]夏菲, 马东升, 潘家永, 等. 天柱大河边重晶石矿床铅同位素特征及来源探讨 [J]. 地球化学, 2005, 34(5):501-507.
[38]陈永权, 蒋少涌, 凌洪飞, 等. 华南寒武纪海洋中沉积矿床及其古环境 [J]. 海洋地质与第四纪地质, 2005, 25(1):79-84.
[39]畅斌,温汉捷. 贵州遵义黄家湾下寒武统牛蹄塘组镍-钼富集层电子探针研究[J]. 矿物学报,2008,28(4):439-446.
[40]杨瑞东, 魏怀瑞, 王伟, 等. 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特征 [J]. 地质论评, 2007, 53(5): 675-680.
[41]吴祥和, 韩至均, 蔡继峰, 等. 贵州磷块岩 [M]. 北京: 地质出版社, 1999: 70-75.
[42]罗泰义, 张欢, 李晓彪,等. 遵义牛蹄塘组黑色岩系中多元素富集层的主要矿化特征 [J]. 矿物学报, 2003, 23(4): 296-302.
[43]徐兴旺, 蔡新平, 肖骑彬,等. 滇西北衙地区热水岩溶作用及其伴生的地质灾害 [J]. 地球科学进展, 2003, 18(6): 912-920.
[44]郑荣才, 文华国,范铭涛,等. 酒西盆地下沟组湖相白烟囱型喷流岩岩石学特征 [J]. 岩石学报, 2006, 22(12): 3027-3038.
[45]郑荣才, 王成善,朱利东,等. 酒西盆地首例湖相“白烟型”喷流岩——热水沉积白云岩的发现及其意义 [J]. 成都理工大学学报:自然科学版, 2003, 30(1): 1-8.
[46]谢桂青, 胡瑞忠, 方维萱, 等. 云南墨江金矿热水喷流沉积成岩成矿的地球化学证据 [J]. 沉积学报, 2002, 20(3): 387-393.
[47]范铭涛, 杨麟科, 方国玉, 等. 青西凹陷下白垩统湖相喷流岩成因探讨及其意义 [J]. 沉积学报, 2003, 21:560-564.
[48]彭润民,翟裕生.内蒙古狼山—渣尔泰山中元古代被动陆缘热水喷流成矿特征 [J].地学前缘, 2004, 11(1): 257-268.
[49]范德廉, 叶杰, 杨瑞英, 等. 扬子地台前寒武—寒武纪界限附近的地质事件及成矿作用 [J]. 沉积学报, 1987, 5(3): 81-96.
[50]杨兢红,蒋少湧,凌洪飞,等.黑色页岩与大洋缺氧事件的ReOs同位素示踪与定年研究 [J].地学前缘,2005, 12(2):143-150.
[51]肖加飞, 胡瑞忠, 宋谢炎,等.贵州早寒武世的缺氧事件沉积 [J]. 矿产与地质, 2006, 20(4/5):36.
[52]Lambert I B,Walter M R, Zang W L, et al. Paleoenvironment and carbon isotope study of the Yangtze Platform [J].Nature, 1987, 325:140-142.
[53]王琛, 林丽, 李德亮,等. 黔西纳雍地区下寒武统牛蹄塘组黑色岩系生物标志物的特征 [J]. 地质通报, 2011, 30(1):106-111.
[54]陈益平,潘家永,胡凯,等. 贵州遵义镍-钼富集层中独居石的发现及成因意义[J]. 岩石矿物学杂志,2007,26(4):340-344.
[55]Bertine K K, Turekian K K. Molybdenum in marine deposits [J]. Geochimica et Cosmochimica Acta, 1973, 37(6): 1415-1434.
[56]韩发, 沈建忠, R W 哈钦森. 冰长石——大厂锡-多金属矿床同生成因的标志矿物 [J]. 矿床地质, 1993, 12(4):330-337.
[57]Rona P A. Black smokers on the midAtlantic Ridge [J].Eos,Transactions, American Geophysical Union, 1985, 66(40):936.
[58]McConachy T F, Whitford D J, Scott S D. Particulate matter concentration in Western Woodlark Basin:evidence for hydrothermal activity [J]. Eos,Transactions, American Geophysical Union,1986, 67:1028.
[59]Leinen M, McDuff R, Delaney J, et al. Offaxial hydrothermal activity in the Mariana Mounds Field [J]. Eos, Transactions, American Geophysical Union, 1987, 68:1531.
[60]Rona P A, Scott S D. A special issue on seafloor hydrothermal mineralization: new perspectives [J]. Economic Geology, 1993, 88:1935-1976.
[61]曹红, 曹志敏. 西南印度洋中脊海底热液活动 [J]. 海洋地质与第四纪地质, 2011, 31(1): 67-76. |