[1] Shi Xiaoying. Latest Jurassic to Early Cretaceous depositional sequence and environment evolution in Qomolongma Area, South XiZang(Tibet)[C]//Proceedings of The Third National Stratigraphical Conference of China, Editorial Committee of the Proceedings of the Third National Stratigraphical Conference of China.Beijing:Geological Publishing House, 2000:260-264.[史晓颖.藏南珠峰地区侏罗纪晚期至白垩纪早期层序地层序列及沉积环境演化[C]//第三届全国地层会议论文集编委会编, 第三届全国地层会议论文集. 北京: 地质出版社, 2000:260-264]. [2] Liu G H, Einsele G. Sedimentary history of the Tethyan Basin in the Tibetan Himalayas[J]. Geological Rundschau,1994:83(1): 32-61. [3] Jadoul F, Berra F, Garzanti E. The tethys himalayan passive margin from late triassic to early cretaceous (South Tibet)[J].Journal of Asian Earth Sciences,1998,16(2/3): 173-194. [4] Shi X Y, Yin J R, Jia C P. Mesozoic and cenozoic sequence stratigraphy and sea-level changes in the Northern Himalayas, South Tibet, China[J].Newsl Stratigr, 1996, 33(1): 13-61. [5] Bureau of Geology and Mineral Resources of Xizang. Regional Geology of Xizang Autonomous Region[M].Beijing:Geological Publishing House, 1993:613-626.[西藏地质矿产局. 西藏自治区区域地质志\[M\]. 北京: 地质出版社, 1993:613-626.] [6] Jiang Xinsheng, Yan Yangji, Pan Guitang, et al. Sedimentary Environment of the late jurassic weimei formation in the South Tibetan Tethys[J].Geological Bulletin of China, 2003, 22(11/12): 900-907.[江新胜, 颜仰基, 潘桂棠,等.藏南特提斯晚侏罗世维美组沉积环境[J]. 地质通报, 2003, 22(11/12): 900-907.] [7] Fu Derong, Liu Xun, Yao Peiyi. The Late Jurassic-Cretaceous Sedimentart-tectonic devopement of the Southern Xizang[J].Bulletin of the Chinese Academy of Geological Science,1990, (21): 21-38.[傅德荣, 刘训, 姚培毅. 西藏南部晚侏罗世—白垩纪沉积与构造背景探讨[J]. 中国地质科学院院报, 1990, (21): 21-38.] [8] Hu Xiumian, Wang Chengshan, Li Xianghui, et al. Sedimentary facies of the uppermost jurassic and Lower Cretaceous in Gucuo area, Southern Tibet[J]. Journal of Palaeogeography,2006, 8(2): 175-186.[胡修棉, 王成善, 李祥辉, 等. 藏南古错地区上侏罗统上部和下白垩统沉积相[J]. 古地理学报, 2006, 8(2): 175-186.] [9] Lin Xinwang. Sedimentary chaotic melanges and their tectonic significance: Upper Cretaceous Zongzhuo formation, Gyangze, Xizang[J]. Journal of Palaeogeography,1998, 18(3): 28-33.[蔺新望. 西藏江孜地区上白垩统宗卓组沉积混杂堆积基本特征及构造意义[J]. 岩相古地理, 1998, 18(3): 28-33.] [10] Liu G, Einsele G. Various types of olistostromes in a closing ocean basin, Tethyan Himalaya (Cretaceous, Tibet) [J]. Sedimentary Geology,1996, 104(1/4): 203-226. [11] Shi Xiaoying. The finding of the Lower Cretaceous sediments of submarine fan in Qomolongma area[J]. Geoscience,2000a, 14(2): 140.[史晓颖. 藏南珠峰地区下白垩统发现海底扇沉积[J]. 现代地质, 2000a, 14(2):140.] [12] Willems H. Sedimentary History of the Tibetan Tethys Himalaya Continental Shelf in South Tibet (Gamba, Tingri) during Upper Cretaceous and Lower Tertiary (Xizang Autonomous Region, PR China)[C]//Willems H, ed. Geoscientific Investigation in the Tethyan Himalayas. Berichte der Fachbereich Geowissenschaften, Universitat Bremen,1993, 38: 49-183. [13] Yu Guangming, Lan Bolong, Wang Chengshan. A Brief Discussion of the Cretaceous Deep Sea Olistostrome and Turbidite Sedimentation in Gyangze, Xizang(Tibet)[C]//Contribution to the Geology of the Qinghai-Xizang(Tibet) Plataeu(15). Beijing:Geological Publishing House, 1984:13-26.[余光明, 兰伯龙, 王成善. 西藏江孜地区白垩系深海中滑塌堆积和浊流沉积作用[C]//青藏高原地质文集(15).北京: 地质出版社, 1984:13-26.] [14] Yue Laiqun, Shi Xiaoying, Wang Hongzhen. Sedimentary environment of submarin fan of the Lower Cretaceous in Norhtern Himalayas[J]. Journal of Palaeogeography,2003, 5(4): 391-403.[岳来群, 史晓颖, 王鸿祯. 北喜马拉雅地区下白垩统海底扇沉积环境[J]. 古地理学报, 2003, 5(4): 391-403.] [15] Zhou Zhiguang, Liang Dingyi, Liu Wencan, et al. Characters of slumping accumulation of Upper Cretaceous Zongzuo formation and demonstrate its caused by large break-up and earthquakes, Southern Xizang (Tibet) [J]. Geological Review,2006, 52(3): 314-321.[周志广, 梁定益, 刘文灿, 等. 藏南晚白垩世宗卓组巨型混杂堆积的特征及其地裂—地震成因论证[J]. 地质论评, 2006, 52(3): 314-321.] [16] Li Guobiao, Wan Xiaoqiao, Yu Chao. Sequence stratigraphy of the Cretaceous strata in the Tethyan Himalayas[J]. Sedimentary Geology and Tethyan Geology,2003, 23(3): 21-34.[李国彪, 万晓樵, 于潮. 特提斯喜马拉雅白垩纪层序地层分析[J]. 沉积与特提斯地质, 2003, 23(3): 21-34.] [17] Li Xianghui, Wang Chengshan, Wan Xiaoqiao, et al. Verification of stratigraphical Sequence and Classification of the Chuangde section of Gyangze, South Tibet[J]. Journal of Stratigraphy,1999, 23(4): 303-309.[李祥辉,王成善,万晓樵,等.藏南江孜县床得剖面侏罗—白垩纪地层层序及地层划分[J]. 地层学杂志,1999, 23(4): 303-309.] [18] Li X H, Wang C S, Hu X M, Stratigraphy of deep-water Cretaceous deposits in Gyangze, Southern Tibet, China[J].Cretaceous Research,2006, 26(1):33-41. [19] Liu Xianbin, Gao Lianfeng, Wan Xiaoqiao, et al. Sequence stratigraphy of the boundary between the Jurassic and the Cretaceous strata in the Northern Tethys-Himalayas Sea area[J].Journal of Mineralogy and Petrology,2006, 26(4): 62-68.[刘宪斌, 高莲凤, 万晓樵, 等. 特提斯—喜马拉雅北带侏罗纪—白垩纪界线层序地层分析[J].矿物岩石, 2006, 26(4): 62-68.] [20] Hao Yichun, Wan Xiaoqiao. The marine Cretaceous and Tertiary Strata of Tingri, Xizang(Tibet)[C]//Contribution to the Geology of the Qinghai-Xizang(Tibet) Plataeu(15). Beijing:Geological Publishing House, 1985:227-232.[郝诒纯, 万晓樵. 西藏定日地区的海相地区的海相白垩、第三系[C]//青藏高原地质文集(17). 北京: 地质出版社, 1985:227-232.] [21] Shi He, Huang Sijing, Shen Licheng. Stratigraphical significance of the Sr isotopic evolutional curve of the Late Cretaceous of Gangba, Tibet with discussions on some problems[J].Journal of Stratigraphy,2005, 29(1): 28-33.[石和, 黄思静, 沈立成. 西藏岗巴晚白垩世锶同位素曲线的地层学意义及问题讨论[J]. 地层学杂志, 2005, 29(1): 28-33.] [22] Wan Xiaoqiao. Cretaceous Strata and Foraminifera of Gangba Region, Xizang(Tibet)[C]//Contribution to the Geology of the Qinghai-Xizang(Tibet) Plataeu(16).Beijing:Geological Publishing House, 1985:203-228.[万晓樵. 西藏岗巴地区白垩纪地层及有孔虫动物群[C]//青藏高原地质文集(16).北京: 地质出版社, 1985:203-228.] [23] Wan Xiaoqiao, Zhao Wenjin, Li Guobiao. Restudy of the Upper Cretaceous in Gamba, Tibet[J].Geoscience,2000, 14(3): 281-285.[万晓樵, 赵文金, 李国彪. 对西藏岗巴晚白垩世地层的新认识[J]. 现代地质, 2000, 14(3): 281-285.] [24] Wan Xiaoqiao, Ding Lin, Li Jianguo, et al. Latest Cretaceous to Early Eocene marine strata in the Zhongba region, Tibet[J].Journal of Stratigraphy,2001, 25(4): 267-272.[万晓樵, 丁林, 李建国, 等. 西藏仲巴地区白垩纪末期—始新世早期海相地层[J]. 地层学杂志, 2001, 25(4): 267-272.] [25] Wang Chengshan, Li Xianghui, Wan Xiaoqiao, et al. The Cretaceous in Gyangze, Southern Xizang (Tibet): Redefined[J].Acta Geologica Sinica,2000, 74(1): 97-107.[王成善, 李祥辉, 万晓樵, 等. 西藏南部江孜地区白垩系的厘定[J]. 地质学报, 2000, 74(1): 97-107.] [26] Wang Naiwen.The Tethyan Cretaceous Stratigraphy of China[C]//Contribution to the Geology of the Qinghai-Xizang(Tibet) Plataeu(3). Beijing:Geological Publishing House, 1983:148-180.[王乃文. 中国白垩纪特提斯地层学问题[C]//青藏高原地质文集(3). 北京: 地质出版社, 1983:148-180.] [27] Willems H, Zhou Z, Zhang B, et al. Stratigraphy of the Upper Cretaceous and Lower Tertiary strata in the Tethyan Himalayas of Tibet (Tingri area, China)[J]. Geologische Rundschau,1996,85(4): 723-754. [28] Wu Haoruo, Wang Dong′an, Wang Liancheng. The Cretaceous along the Lhaze-Gyangze area, Southern Xizang(Tibet)[J].Scientia Geologica Sinica,1977, 67(3): 250-261.[吴浩若, 王东安, 王连城. 西藏南部拉孜—江孜一带的白垩系[J]. 地质科学, 1977, 67(3): 250-261.] [29] Wu Haoruo. Later late Cretaceous and early Tertiary strata in Gyangze area, Southern Xizang(Tibet)[J].Journal of Stratigraphy,1987, 11(2): 147-149.[吴浩若. 西藏南部江孜地区晚白垩世晚期及早第三纪(?)地层[J]. 地层学杂志, 1987, 11(2): 147-149.] [30] Xu Yulin, Wan Xiaoqiao, Gou Zonghai, et al. The Jurassic, Cretaceous and Tertiary Biostratigraphical Strata, Xizang(Tibet)[M]. Wuhan:Publishing House of University of Geology of China, 1989:1-147.[徐钰林, 万晓樵, 苟宗海, 等. 西藏侏罗、白垩、第三纪生物地层[M]. 武汉: 中国地质大学出版社, 1989:1-147.] [31] Gou Zonghai. A Cretaceous bivalve Fauna in Gangba Region, Xizang[C]//Contribution to the Geology of the Qinghai-Xizang(Tibet) Plataeu(18).Beijing:Geological Publishing House, 1983:146-170.[苟宗海. 西藏岗巴地区白垩纪双壳类动物群[C]//青藏高原地质文集(18).北京: 地质出版社,1983:146-170.][32] Li Guobiao, Wan Xiaoqiao, Liu Wencan, et al. Discovery of Cretaceous radiolarians in“mélanges”in Saiqu, Sa gya, Southern Tibet,and its geological significance [J].Geological Bulletin of China,2003, 22(11/12): 949-955.[李国彪, 万晓樵, 刘文灿, 等. 藏南萨迦县赛区”混杂岩”放射虫的发现及其意义[J]. 地质通报, 2003, 22(11/12): 949-955.] [33] Zhong Shilan, Zhou Zhicheng, Willenms H, et al. The Middle Cretaceous calcareous nannofossil zones in Gamba area, Southern Xizang (Tibet), China and the Cenomanian-Turonian boundary[J]. Acta Palaeontologica Sinica,2000, 39(3): 313-325.[钟石兰, 周志澄, Willems H, 等. 西藏南部岗巴地区白垩纪中期钙质超微化石Cenomanian-Turonian界线[J]. 古生物学报, 2000, 39(3): 313-325.] [34] Si Jialiang, Gao Lianfeng, Wan Xiaoqiao. Late Cretaceous biotic response to marine dissolved oxygen content in Southern Tibet[J].Earth Science Frontiers,2005, 12(2): 113-122.[司家亮, 高莲凤, 万晓樵. 西藏南部晚白垩世大洋氧含量变化的生物特征[J]. 地学前缘, 2005, 12(2): 113-122.] [35] Wan Xiaoqiao. Cretaceous-Early Tertiary foraminifera of Xizang (Tibet) and evolution of the Tethys-Himalayan sea [J]. Acta Micropalaeontologica Sinica,1990, 7(2): 169-186.[万晓樵. 西藏白垩纪—早第三纪有孔虫与特提斯喜马拉雅海的演化[J]. 微体古生物学报, 1990, 7(2): 169-186.] [36] Wan Xiaoqiao. Cretaceous foraminifera from Southern Xizang (Tibet): A study on eustatic change[J].Geoscience,1992, 6(4): 392-398.[万晓樵. 从有孔虫分析西藏南部白垩纪海平面升降[J]. 现代地质, 1992, 6(4): 392-398.] [37] Wan Xiaoqiao, Yin Jiarun. Mid-Cretaceous microfossil assemblages and paleoceanographic event in Gamba, Tibet [J].Acta Micropalaeontologica Sinica,1996, 13(1): 43-56.[万晓樵, 阴家润. 西藏岗巴地区白垩纪中期微体生物群与古海洋事件[J]. 微体古生物学报, 1996, 13(1): 43-56.] [38] Wan Xiaoqiao, Ding Lin. Discovery of the Latest Cretaceous planktonic foraminifera from gyirong of Southern Tibet and its chronostratigraphic significance[J].Acta Palaeontologica Sinica,2002, 41(10): 89-95.[万晓樵, 丁林. 西藏吉隆白垩纪末期浮游有孔虫的发现及其年代意义[J]. 古生物学报, 2002, 41(10): 89-95.] [39] Wan X Q, Lamolda M A, Si J L, et al. Foraminiferal stratigraphy of Cretaceous red beds in Southern Tibet[J].Cretaceous Research,2005, 26(1): 43-48. [40] Wu Haoruo, Li Hongsheng. Radiolaria from the olistostrome of the Zongzhuo formation, Gyangze, Southern Xizang (Tibet) [J].Acta Palaeontologica Sinica,1982, 21(1): 64-71.[吴浩若, 李红生. 藏南宗卓组滑塌堆积中的放射虫化石[J]. 古生物学报, 1982, 21(1): 64-71.] [41] Zhao Wenjin. Late Cretaceous foraminiferal faunas and eustatic change in Gamba area, Southern Tibet[J].Geological Journal of China Universities,2001, 7(1): 106-117.[赵文金. 西藏岗巴晚白垩世有孔虫动物群与海平面变化[J]. 高校地质学报, 2001, 7(1): 106-117.] [42] Zhao Wenjin, Wan Xiaoqiao. Recovery of foraminifera from the Late Cretaceous Cenomanian-Turonian mass extinction in Gamba, Southern Tibet[J]. Acta Palaeontologica Sinica,2001, 40(2): 189-194.[赵文金, 万晓樵. 西藏南部岗巴地区晚白垩世Cenomanian-Turonian集群灭绝事件后有孔虫动物群的复苏[J]. 古生物学报, 2001, 40(2): 189-194.] [43] Zhao Wenjin, Wan Xiaoqiao. Bio palaeooceanographic events near the Cenomanian-Turonian boundary in Tingri, Southern Tibet, China [J]. Scientia Geologica Sinica,2003, 38(2): 155-164.[赵文金, 万晓樵. 藏南定日地区Cenomanian-Turonian界线附近的生物古海洋事件[J]. 地质科学, 2003, 38(2): 155-164.] [44] Hu X M, Jansa L, Wang C S, et al. Upper cretaceous oceanic red beds(CORBs) in the tethys: Occurrences, lithofacies, age, and environments[J]. Cretaceous Research,2005. 26(1): 3-20. [45] Hu Xiumian, Wang Chengshan, Li Xianghui, et al. The Upper Cretaceous oceanic red beds, Xizang(Tibet): Lithological types, sedimentary environment and color orgin[J]. Science in China(Series D), 2006, 36(9): 811-821.[胡修棉, 王成善, 李祥辉, 等. 藏南上白垩统大洋红层: 岩石类型、沉积环境与颜色成因[J]. 中国科学:D辑, 2006, 36(9): 811-821.] [46] Hu Xiumian, Wang Chengshan. Cretaceous oceanic red beds: Characters, occurrences, and origin[J]. Geological Journal of China Universities,2007,13(1):1-13.[胡修棉, 王成善. 白垩纪大洋红层: 特征、分布与成因[J]. 高校地质学报, 2007,13(1):1-13.] [47] Wang Chengshan, Hu Xiumian, Wan Xiaoqiao, et al. Mid-Cretaceous Cenomanian-Turonian oceanic anoxic event in south Tibet[J].Nature Magazine,1999,21(4):244-246.[王成善,胡修棉,万晓樵,等.西藏南部中白垩世Cenomanian-Turonian缺氧事件研究[J].自然杂志,1999,21(4):244-246.] [48] Wang C S, Hu X M, Jansa L, et al. The Cenomanian-Turonian anoxic event in south Tibet[J].Cretaceous Research,2001,22(4): 481-490. [49] Wang C S, Hu X M, Massimo Sarti, et al. Upper Cretaceous oceanic red beds in Southern Tibet: A major change from anoxic to oxic, deep-sea environments[J]. Cretaceous Research, 2005, 26 (1): 21-32. [50] Li Xianghui,Wang Chengshan, Yin Haisheng, et al. Middle Cretaceous and Eocene Lithofacies and paleogeography in Tibet [J].Regional Geology of China, 2001, 20(1): 82-89.[李祥辉, 王成善,伊海生,等. 西藏中白垩世和始新世岩相古地理[J]. 中国区域地质, 2001, 20(1): 82-89.] [51] Patzelt A, Li H, Wang J, et al. Palaeomagnetism of Cretaceous to tertiary sediments from Southern Tibet, evidence for the extent of the northern margin of India prior the collision with eurasia[J].Tectonophysics,1996, 259(4): 259-284. [52] Li Xianghui, Wang Chengshan, Hugh C, et al. Bulk carbon isotope excursions of the Cenomanian through Turonian of mid-Cretaceous in Southern Tibet[J].Earth Science—Journal of China University of Geosciences,2005, 30(3): 63-73.[李祥辉, 王成善, Hugh C, 等. 西藏特提斯喜马拉雅白垩纪中期Cenomanian-Turonian期碳同位素偏移[J]. 地球科学:中国地质大学学报, 2005, 30(3): 63-73.] [53] Li Xianghui, Wang Chengshan, Hugh C, et al. High-resolution bulk carbon isotope stratigraphy of Upper Cretaceous in Southern Xizang(Tibet)[J].Geological Review,2006,52(3): 304-313.[李祥辉, 王成善, Hugh C, 等. 西藏南部上白垩统高分辨率全岩碳同位素地层学[J]. 地质论评, 2006,52(3): 304-313.] [54] Li Xianghui, Jenkyns H C, Wang Chengshan, et al. Carbon isotope excursion of Late Cretaceous Campanian in Southern Xizang and its Implication[J].Geochimica,2007,36(3): 279-285.[李祥辉, Jenkyns H C, 王成善, 等. 西藏南部晚白垩世坎潘期碳同位素偏移及其意义[J]. 地球化学, 2007,36(3): 279-285.] [55] Hu Xiumian, Wang Chengshan, Li Xianghui. Stable carbon isotope response to oceanic anoxic events[J].Journal of Chengdu University of Technology,2001, 28(1):1-6.[胡修棉, 王成善, 李祥辉.大洋缺氧事件的碳稳定同位素响应[J]. 成都理工学院学报, 2001, 28(1):1-6.] [56] Hu Xiumian, Wang Chengshan, Li Xianghui. The stable carbon isotope of Cretaceous carbonate and its response to paleo-ocean dissolvedoxygen events in Southern Tibet[J].Progress in Natural Science,2001,10(7): 341-349.[胡修棉, 王成善, 李祥辉. 藏南海相白垩纪碳酸盐碳稳定同位素演化与古海洋溶解氧事件[J]. 自然科学进展, 2001, 10(7): 341-349.] [57] Huang Sijing, Shi He, Zhang Meng, et al. Strontium isotope age calibration of rudist bivalves from Late Cretaceous section in Southern Tibet[J].Earth Science—Journal of China University of Geosciences,2005, 30(4): 437-442.[黄思静, 石和, 张萌, 等. 西藏南部晚白垩世厚壳蛤的锶同位素年龄标定[J]. 地球科学:中国地质大学学报, 2005, 30(4): 437-442.] [58] Huang Sijing, Qing Hairuo, Hu Zuowei, et al. Geochemistry in different shellLayers of rudist bivalve from Late Cretaceousin the south of Tibet and preservation for the information of sea water[J].Acta Sedimentologica Sinica,2006, 24(1): 68-74.[黄思静,卿海若,胡作维,等.西藏南部晚白垩世厚壳蛤不同壳层的地球化学特征及其对古海洋信息的保存性[J].沉积学报, 2006, 24(1): 68-74.] [59] Wan Xiaoqiao,Liu Wencan, Li Guobiao, et al. Cretaceous black shale and dissolved oxygen content—A case study in southern Tibet[J].Chinese Geology,2003, 30(1): 36-47.[万晓樵, 刘文灿, 李国彪, 等. 白垩纪黑色页岩与海水含氧量变化——以西藏南部为例[J]. 中国地质, 2003, 30(1): 36-47.] [60] Wan X Q, Wei M R, Li G B. δ13C values from the cenomanian-turonian passage beds of Southern Tibet[J].Journal of Asian Earth Sciences,2003,21(8): 861-866. [61] Wang Chengshan, Hu Xiumian, Li Xianghui. Dissolved oxygen in palaeo ocean: Anoxic events and high oxic problems[J].Marine Geology & Quaternary Geology,1999, 19(3): 39-47.[王成善, 胡修棉, 李祥辉. 古海洋溶解氧与缺氧和含氧问题研究[J]. 海洋地质与第四纪地质, 1999, 19(3): 39-47.] [62] Yin Guan, Wang Chengshan. The composition of carbon and oxygen isotope and the discussion about the oceanic anoxic events in the Middle Cretaceous black shale, South Tibet[J].Journal of Mineralogy and Petrology,1998, 71(1): 95-101.[尹观, 王成善. 西藏南部中白垩世黑色页岩的碳氧同位素组成及大洋缺氧事件的讨论[J]. 矿物岩石, 1998, 71(1): 95-101.] [63] Zou Y R, Kong F, Ping P A, et al. Organic geochemical characterization of Upper Cretaceous oxic oceanic Sediments in Tibet, China: A preliminary study[J].Cretaceous Research,2006,26(1): 65-71. [64] Fu Peigang, Song Zhiguang, Hu Xiumian, et al. The composition and distribution of organic matter of the Cretaceous black and red bed sediments from Southern Tibet [J]. Acta Geologica Sinica,2008, 82(1): 85-91.[傅培刚, 宋之光, 胡修棉,等.藏南白垩系黑—红层沉积岩有机质组成分布特征[J]. 地质学报, 2008, 82(1): 85-91.] [65] Yue Laiqun, Li Yongtie, Shi Xiaoying. Geologic characteristics and their hydrocarbon implication of black shales of the Lower Cretaceous in Kuco-Gamba basin, Tibet[J].Journal of Palaeogeography, 2006, 8(3): 307-316.[岳来群, 李永铁, 史晓颖. 西藏古错—岗巴盆地下白垩统黑色页岩地质特征及其油气资源意义[J]. 古地理学报, 2006, 8(3): 307-316.] [66] Chen Nansheng, Dong Zhensheng. Sedimentological geochemistry of the strata from Ordovician to Tertiary in Nyanang-Gamba area, Southern Xizang[J].Geochimica,1982,(1): 105-113.[陈南生, 董振生. 西藏南部聂拉木—岗巴地区奥陶纪—老第三纪地层沉积地球化学[J]. 地球化学, 1982, (1): 105-113.] [67] Zhao Wenjin, Wan Xiaoqiao. Mid-Cretaceous geochemical anomaly and their responses to sealevel changes in Tingri of Tibet [J].Advances in Earth Science,2002, 17(3): 331-338.[赵文金, 万晓樵. 藏南定日地区白垩纪中期地球化学异常对海平面上升的响应[J]. 地球科学进展, 2002, 17(3): 331-338.] [68] Zhao Zhenhua, Chen Nansheng, Dong Zhensheng, et al. Ree Geochemistry of Ordovician-Tertiary strata in Nyalam-Gamba area, South Xizang[J].Geochimica,1985,(2): 27-37.[赵振华, 陈南生, 董振生, 等. 西藏南部聂拉木—岗巴地区奥陶纪—老第三纪沉积地层稀土元素地球化学[J]. 地球化学, 1985, (2): 27-37.] [69] Chen Lei, Hu Xiumian, Huang Zhicheng. Constrains from Early Cretaceous volcaniclastic sandstones in Southern Tibet on a volcanic event in the northern Margin of the Indian Continent [J].Acta Geologica Sinica,2007, 81(4): 501-510.[陈蕾, 胡修棉, 黄志诚. 藏南早白垩世火山岩屑砂岩对印度大陆北缘火山事件的约束[J]. 地质学报, 2007, 81(4): 501-510.] [70] Pan Guitang, Li Xingzhen, Wang Liquan, et al. Preliminary division of tectonic units of the Qinghai-Tibet Plateau and its adjacent regions[J].Geological Bulletin of China,2002, 21(11): 701-707.[潘桂棠, 李兴振, 王立全, 等. 青藏高原及邻区大地构造单元初步划分[J]. 地质通报, 2002, 21(11): 701-707.] [71] Pan Guitang, Ding Jun, Wang Liquan, et al. Mannual Book of 1∶1500000 Geological Map of the Qinghai-Tibet Plateau and its adjacent regions[M].Chengdu:Chengdu Mapping Publishing House,2004:7-12.[潘桂棠, 丁俊, 王立全, 等. 1∶150万青藏高原及邻区地质图说明书[M]. 成都:成都地图出版社, 2004: 7-12] [72] Wang Jian, Tan Fuwen, Li Yalin, et al. The Potential of the Oil and Gas Resources in Major Sedimentary Basins on the Qinghai-Xizang(Tibet) Plateau[M]. Beijing: Geological Publishing House, 2004:248-282.[王剑, 谭富文, 李亚林, 等. 青藏高原重点沉积盆地油气资源潜力分析[M]. 北京: 地质出版社, 2004:248-282.] [73] Tribovillard N, Algeo T J, Lyons T,et al. Trace metals as paleoredox and paleoproductivity proxies—An update[J].Chemical Geology,2006, 232(1/2): 12-32. [74] Dean W E, Gardner J V, Pipers D Z. Inorganic geochemical indicators of glacial-interglacial changes in productivity and anoxia on the california continental margin[J].Geochimica et Cosmochimica Acta,1997, 61(21): 4 507-4 518. [75] Crusius J, Calvert S, Pedersen T,et al. Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic, and sulfidic conditions of deposition[J].Earth and Planetary Science Letters,1996, 145(1/4): 65-78. [76] Bruland K W. Trace Elements in Seawater, In Chemical Oceanography[M]. Academic Press, 1983:157-220. [77] Meyers S R, Sageman B B, Lyons T W. Organic carbon burial rate and the molybdenum proxy: Theoretical framework and application to cenomanian-turonian oceanic event 2[J].Paleoceanography, 2005, 20(2): 2 002-2 020. [78] Koide M, Hodge V, Yang J S, et al. Some comparative marine chemistries of rhenium, gold, silver and molybdenum[J].Applied Geochemisty,1986, 1(6): 705-714. [79] Turgeon S, Brumsack H J. Anoxic vs dysoxic events reflected in sediment geochemistry during the cenomanian-turonian boundary event (Cretaceous) in the Umbria-Marche Basin of central Italy[J].Chemical Geology,2006, 234(3/4): 321-339. [80] Calvert S E, Pedersen T F. Geochemistry of recent oxic and anoxic marine sediments:Implications for the geological record[J].Marine Geology,1993,113(1/2): 67-88. [81] Rosenthal Y, Lam P, Boyle E A, et al. Authigenic cadmium enrichments in suboxic sediments: Precipitation and postdepositional mobility[J].Earth and Planetary Science Letters,1995,132(1/4): 99-111. [82] Russell A D , Morford J l, The behavior of redox-sensitive metals across a laminated-massive-laminated transition in saanich inlet, British Columbia[J].Marine Geology,2001,174 (1/4): 341-354. [83] Chaillou G, Anschutz P, Lavaux G, et al. The distribution of Mo, U, and Cd in relation to major redox species in muddy sediments of the Bay of Biscay[J]. Marine Chemistry,2002,80(1): 41-59. [84] Middelburg J J,Comans R J N. Sorption of Cadmium on Hydroxyapatite[J].Chemical Geology,1991,90(1/2): 45-53. [85] Jarvis I, Burnett W C, Nathan Y, et al. Phosphorite Geochemistry: State of the Art and Environmental Concerns[J].Eclogae Geologicae Helvetiae,1994,87(3): 643-700. [86] Morford J L, Russell A D, Emerson S. Trace metal evidence for changes in the redox environment assocoated with the transition from terrigenous clay to diatomaceous sediments, saanich inlet, BC[J].Marine Geology,2001,174(1/4): 355-369. [87] Zheng Y, Anderson R F, van Geen A, et al. Preservation of non-lithogenic particulate uranium in marine Sediments[J].Geochim Cosmochim Acta,2002a,66(17): 3 085-3 092. [88] Zheng Y, Anderson R F, van Geen A, et al. Remobilization of authigenic uranium in marine sediments by Bioturbation[J].Geochim Cosmochim Acta,2002b,66(10): 1 759-1 772. [89] McManus J, Berelson W M, Klinkhammer G P, et al. Authigenic uranium: Relationship to oxygen penetration depth and organic carbon rain[J].Geochim Cosmochim Acta,2005, 69(1): 95-108. [90] Algeo T J, Maynard J B. Trace-element behavior and redox facies in core shales of upper pennsylvanian kansas-type cyclothems[J].Chemical Geology,2004, 206(3/4): 289-318. [91] Algeo T J, Lyons T W, Blakey R C,et al. Hydrographic conditions of the devono-carboniferous North American seaway inferred from sedimentary Mo-TOC Relationships[J].Palaeogeography Palaeoclimatology Palaeoecology,2007,256(3/4): 204-230. [92] Mongenot T, Tribovillard N P, Desprairies A,et al.Trace elements as palaeoenvironmental markers in strongly mature hydrocarbon source rocks: The cretaceous la luna formation of venezuela[J].Sedimentary Geology,1996, 103(1/2): 23-37. [93] Brumsack H J. Geochemistry of recent TOC-rich sediments from the gulf of california and the Black Sea[J]. Geologische Rundschau,1989, 78(3): 851-882 [94] Morford J L, Emerson S. The geochemistry of redox sensitive trace metals in sediments[J]. Geochimica et Cosmochimical Acta,1999, 63(11/12): 1 735-1 750. [95] Piper D Z, Perkins R B. A modern vs. Permian black Shale-the hydrography, primary productivity, and water-column chemistry of deposition[J]. Chemical Geology,2004, 206(3/4): 177-197. [96] Wedepohl K H. Environmental Influences on the Chemical Composition of Shales and Clays[M]//Ahrens L H, Press F,Runcorn S K, et al, eds. Physics and Chemistry of the Earth. Oxford: Pergamon, 1971: 305-333. [97] Brumsack H J,Gieskes J M. Interstitial water trace metal chemistry of laminated sediments from the gulf of california, Mexico[J].Marine Chemistry,1983,14(1): 89-106. [98] Shaw T J, Gieskes J M, Jahnke R A. Early diagenesis in differing depositional environments: The response of transitions metals in pore water[J]. Geochimica et Cosmochimical Acta,1990,54(5): 1233-1 246. [99] Hatch J R, Leventhal J S. Relationship between inferred redox potential of the depositional environment and geochemistry of the upper pennsylvanian (Missourian) stark shale member of the dennis limestone, Wabaunsee County, Kansas, U.S.A[J].Chemical Geology,1992, 99(1/3): 65-82. [100] Xiong Guoqing, Wang Jian, Hu Renfa. Trace element characteristics and sedimentary environment of the sinian system of the Fanjingshan area in Guizhou province[J]. Acta Geosicentica Sinica,2008, 29(1): 51-60.[熊国庆, 王剑, 胡仁发. 贵州梵净山地区震旦系微量元素特征及沉积环境[J]. 地球学报, 2008, 29(1): 51-60.] [101] Jones B, Manning D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in Ancient Mudrocks[J].Chemical Geology,1994, 111(1/4): 111-129. [102] Wu Chaodong, Yang Chenyun, Chen Qiying. The origin and geochemical characteristics of Upper Sinain-Lower cambrian black shales in Western Hunan[J].Acta Petrologica et Mineralogica,1999, 18(1): 26-39.[吴朝东, 杨承运, 陈其英. 湘西黑色岩系地球化学特征和成因意义[J]. 岩石矿物学杂志, 1999, 18(1): 26-39.] [103] Hallberg R O A. Geochemical method for investigation of paleoredox conditions in sediments[J].Ambio Special Report,1976,4:139-147. [104] Dypvik H. Geochemical compositions and depositional conditions of Upper jurassic and Lower Cretaceous yorkshire clays, England[J].Geological Magazine,1984,121(5):489-504. [105] Lu Yuanfa. GeoKit—A geochemical toolkit for Microsoft Excel[J].Geochimica,2004,33(5):459-464.[路远发. Geokit: 一个用VBA组建的地球化学工具软件通[J]. 地球化学,2004,33(5):459-464.] |