Faugères J-C, Stow D A V. Bottom-current-controlled sedimentation: a synthesis of the contourite problem[J]. Sedimentary Geology, 1993, 82(1/4): 287-297.
[2]
郭依群,王嘹亮,匡增桂,等. 等深流沉积特征[J]. 海洋地质前沿,2012,28(6):1-9. [Guo Yiqun, Wang Liaoliang, Kuang Zenggui, et al. Depositional features of contourites and research progress[J]. Marine Geology Frontiers, 2012, 28(6): 1-9.]
[3]
方念乔,陈萍,吴琳,等. 孟加拉湾深海记录中的等深流活动特征及其环境意义初探[J]. 地球科学,2002,27(5):570-575. [Fang Nianqiao, Chen Ping, Wu Lin, et al. Contour currents in deep-water records from bay of Bengal and its environmental implication[J]. Earth Science, 2002, 27(5): 570-575.]
[4]
王玉柱,王海荣,高红芳,等. 等深流作用机制和沉积的研究进展[J]. 古地理学报,2010,12(2):141-150. [Wang Yuzhu, Wang Hairong, Gao Hongfang, et al. Contour current dynamics process and deposits: A review[J]. Journal of Palaeogeography, 2010, 12(2): 141-150.]
[5]
李发科,汪德雯,林小云,等. 湘西北下寒武统等深流沉积[J]. 江汉石油学院学报,2001,23(增刊):7-9.[Li Fake, Wang Dewen, Lin Xiaoyun, et al. Lower Cambrian contour current deposits in the Northwestern Hunan[J]. Journal of Jianghan Petroleum Institute, 2001, 23(Suppl.): 7-9.]
[6]
韩小锋,陈世悦,刘宝鸿,等. 深水沉积特征研究现状及展望[J]. 特种油气藏,2008,15(2):1-6. [Han Xiaofeng, Chen Shiyue, Liu Baohong, et al. Present research status and forecast about deep-water deposition[J]. Special Oil & Gas Reservoirs, 2008, 15(2): 1-6.]
[7]
Bein A, Weiler Y. The Cretaceous Talme Yafe Formation: a contour current shaped sedimentary prism of calcareous detritus at the continental margin of the Arabian Craton[J]. Sedimentology, 1976, 23(4): 511-532.
[8]
刘宝珺,许效松,梁仁枝. 湘西黔东寒武纪等深流沉积[J]. 矿物岩石,1990,10(4):43-47.[Liu Baojun, Xu Xiaosong, Liang Renzhi. Contourites of Cambrian in weatern Hunan and eastern Guizhou[J]. Mineralogy and Petrology, 1990, 10(4): 43-47.]
[9]
屈红军,梅志超,李文厚,等. 陕西富平地区中奥陶统等深流沉积的特征及其地质意义[J]. 地质通报,2010,29(9):1304-1309. [Qu Hongjun, Mei Zhichao, Li Wenhou, et al. The Middle Ordovician contour current deposits and its geological implication in Fuping region, Shanxi province, China[J]. Geological Bulletin of China, 2010, 29(9): 1304-1309.]
[10]
丁海军,孟祥化,葛铭,等. 贺兰坳拉谷北段奥陶系等深流沉积[J]. 地球科学与环境学报,2009,31(1):58-64.[Ding Haijun, Meng Xianghua, Ge Ming, et al. Ordovician contourite of the north part of Helan Aulacogen [J]. Journal of Earth Sciences and Environment, 2009, 31(1): 58-64.]
[11]
姜在兴,赵徽林,熊继辉. 皖中下志留统的等深积岩及其地质意义[J]. 科学通报,1989,34(20):1575-1576. [Jiang Zaixing, Zhao Huilin, Xiong Jihui. The Middle and Lower Silurian contourites and their geological significance in Anhui[J]. Chinese Science Bulletin, 1989, 34(20): 1575-1576.]
[12]
李华,王英民,徐强,等. 南海北部第四系深层等深流沉积特征及类型[J]. 古地理学报,2013,15(5):741-750. [Li Hua, Wang Yingmin, Xu Qiang, et al. Sedimentary characteristics and types of the Quaternary deep water contourites in northern South China Sea[J]. Journal of Palaeogeography, 2013, 15(5): 741-750.]
[13]
李华,王英民,徐强,等. 南海北部珠江口盆地重力流与等深流交互作用沉积特征、过程及沉积模式[J]. 地质学报,2014,88(6):1120-1129.[Li Hua, Wang Yingmin, Xu Qiang, et al. Interactions between down-slope and along-slope processes on the northern slope of South China Sea: products, processes, and depositional model[J]. Acta Geologica Sinica, 2014, 88(6): 1120-1129.]
[14]
段太忠,郭建华,高振中,等. 华南古大陆边缘湘北九溪下奥陶统碳酸盐等深岩丘[J]. 地质学报,1990(2):131-143. [Duan Taizhong, Guo Jianhua, Gao Zhenzhong, et al. A Lower Ordovician carbonate contourite drift on the margin of the South China palaeocontinent in Jiuxi, northern Hunan[J]. Acta Geologica Sinica, 1990(2): 131-143.]
[15]
Stow D A V, Pudsey C J, Howe J A, et al. Deep-Water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics[M]. London: Geological Society, 2002: 409-442.
[16]
Duan T Z, Gao Z Z, Zeng Y F, et al. A fossil carbonate contourite drift on the Lower Ordovician palaeocontinental margin of the middle Yangtze Terrane, Jiuxi, northern Hunan, southern China[J]. Sedimentary Geology, 1993, 82(1/2/3/4): 271-284.
[17]
王剑,段太忠,谢渊,等. 扬子地块东南缘大地构造演化及其油气地质意义[J]. 地质通报,2012,31(11):1739-1749. [Wang Jian, Duan Taizhong, Xie Yuan, et al. The tectonic evolution and its oil and gas prospect of southeast margin of Yangtze Block[J]. Geological Bulletin of China, 2012, 31(11): 1739-1749.]
[18]
段太忠,曾允孚,高振中. 根据沉积历史分析华南古大陆边缘的构造演化[J]. 石油与天然气地质,1988,9(4):410-420. [Duan Taizhong, Zeng Yunfu, Gao Zhenzhong. Analysis of tectonic evolution of paleo-continental margin in South China based on sedimentary history[J]. Oil & Gas Geology, 1988, 9(4): 410-420.]
[19]
冯增昭,彭勇民,金振奎,等. 中国南方寒武纪岩相古地理[J]. 古地理学报,2001,3(1):1-14. [Feng Zengzhao, Peng Yongmin, Jin Zhenkui, et al. Lithofacies palaeogeography of the Cambrian in South China[J]. Journal of Palaeogeography, 2001, 3(1): 1-14.]
[20]
葛祥英,牟传龙,周恳恳,等. 湖南奥陶纪沉积演化特征[J]. 中国地质,2013,40(6):1829-1841.[Ge Xiangying, Mou Chuanlong, Zhou Kenken, et al. Characteristics of Ordovician sedimentary evolution in Hunan province[J]. Geology in China, 2013, 40(6): 1829-1841.]
[21]
左景勋,彭善池,朱学剑. 扬子地台寒武系碳酸盐岩的碳同位素组成及地质意义[J]. 地球化学,2008,37(2):118-128.[Zuo Jingxun, Peng Shanchi, Zhu Xuejian. Carbon isotope composition of Cambrian carbonate rocks in Yangtze Platform, South China and its geological implications[J]. Geochimica, 2008, 37(2): 118-128.]
[22]
裴羽,罗顺社,冯洁,等. 深水泥晶灰岩中大型交错层理成因探讨——以湘北九溪地区下奥陶统为例[J]. 石油天然气学报(江汉石油学院学报),2013,35(6):32-35.[Pei Yu, Luo Shunshe, Feng Jie, et al. Discussions of large-scale cross beddings in deepwater micrite—A case study of Lower Ordovician in Jiuxi area of northern Hunan province[J]. Journal of Oil and Gas Technology, 2013, 35(6): 32-35.]
[23]
Faugèers J -C, Gonthier E, Stow D A V. Contourite drift molded by deep Mediterranean outflow[J]. Geology, 1984, 12(5): 296-300.
[24]
何幼斌,高振中,罗顺社,等. 等深流沉积的特征及其鉴别标志[J]. 江汉石油学院学报,1998,20(4):1-6. [He Youbin, Gao Zhenzhong, Luo Shunshe, et al. Features of contourites and their discrimination[J]. Journal of Jianghan Petroleum Institute, 1998, 20(4): 1-6.]
[25]
郑秀才,郭成贤,高振中,等. 湘西下寒武统清虚洞组碳酸盐缓坡沉积相特征[J]. 江汉石油学院学报,1992,14(3):15-20. [Zheng Xiucai, Guo Chengxian, Gao Zhenzhong, et al. A carbonate ramp of Lower Cambrian Qingxudong Formation in West Hunan[J]. Journal of Jianghan Petroleum Institute, 1992, 14(3): 15-20.]
[26]
郑秀才,郭成贤. 中扬子地区下寒武统清虚洞组斜坡带沉积特征及其含油气性[J]. 湖南地质,1995,14(3):140-144,158. [Zheng Xiucai, Guo Chengxian. Sedimentary and hydrocarbon-bearing features of the slope zone of Qingxudong Formation of Lower Cambrian system in central Yangtze region[J]. Hunan Geology, 1995, 14(3): 140-144, 158.]
[27]
虞子冶,施央申,郭令智. 广西钦州盆地志留纪—中泥盆世等深流沉积及其大地构造意义[J]. 沉积学报,1989,7(3):21-29. [Yu Ziye, Shi Yangshen, Guo Lingzhi. The paleocontourite and its tectonic significance in Qinzhou Basin, Guangxi, China[J]. Acta Sedimentologica Sinica, 1989, 7(3): 21-29.]
[28]
罗顺社,汪凯明. 河北宽城地区中元古代高于庄组碳酸盐岩碳氧同位素特征[J]. 地质学报,2010,84(4):492-499. [Luo Shunshe, Wang Kaiming. Carbon and oxygen isotope composition of carbonate rock from the Mesoproterozoic Gaoyuzhuang Formation in the Kuancheng area, Hebei province[J]. Acta Geologica Sinica, 2010, 84(4): 492-499.]
[29]
李日辉,张光威,李维群. 等深岩识别标志研究[J]. 海洋地质与第四纪地质,1997,17(3):63-70.[Li Rihui, Zhang Guangwei, Li Weiqun. Criteria for recognition of ancient contourites[J]. Marine Geology & Quaternary Geology, 1997, 17(3): 63-70.]
[30]
罗顺社,何幼斌. 深水等深积岩丘及其含油气潜能[J]. 海相油气地质,2002,7(4):8-12.[Luo Shunshe, He Youbin. Deep-water contourite drifts and their hydrocarbon potential[J]. Marine Origin Petroleum Geology, 2002, 7(4): 8-12.]
[31]
Stow D A V. Distinguishing between fine-grained turbidites and contourites on the Nova Scotian Deep Water Margin[J]. Sedimentology, 2006, 26(3): 371-387.
[32]
高振中,罗顺社,何幼斌,等. 鄂尔多斯地区西缘中奥陶世等深流沉积[J]. 沉积学报,1995,13(4):16-26. [Gao Zhenzhong, Luo Shunshe, He Youbin, et al. The Middle Ordovician contourite on the west margin of Ordos[J]. Acta Sedimentologica Sinica, 1995, 13(4): 16-26.]
