Oil & Gas Geology ›› 2018, Vol. 39 ›› Issue (2): 384-397.doi: 10.11743/ogg20180217
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Li Hua1,3, He Youbin1,3
Received:
2017-04-27
Revised:
2018-01-05
Online:
2018-04-28
Published:
2018-05-16
CLC Number:
Li Hua, He Youbin. Sedimentary characteristics and significance of reworked sands in the Ordovician Pingliang Formation,southwestern margin of Ordos Basin[J]. Oil & Gas Geology, 2018, 39(2): 384-397.
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[1] Shanmugam G.Deep-marine tidal bottom currents and their reworked sands in modern and ancient submarine canyons[J].Marine and Petroleum Geology, 2003, 20:471-491. [2] Bouma A H.Sedimentology of some flysch deposits[M].Elsevier, Amsterdam, 1962:168. [3] Rebesco M, Hernández-Molina, Rooij D V,et al.Contourites and associated sediments controlled by deep-water circulation processes:State-of-the-art and future considerations[J].Marine Geology, 2014, 352:111-154. [4] Gao Z Z, Kenneth A E, He Y B, et al.Deep-water traction current deposits-The study of internal-tide, internal-wave, and contour current deposits[M].Beijing:Science Press, 1996:77-113. [5] Mulder T, Faugères J C, Gonthier E.Mixed turbidite-contourite systems[M].Elsevier, 2008:435-456. [6] 吴嘉鹏,王英民,王海荣,等.深水重力流与底流交互作用研究进展[J].地质论评,2012,58(6):1110-1120. Wu Jiapeng, Wang Yingmin, Wang Hairong, et al.The interaction between deep-water turbidity and bottom currents:a review[J].Geological Review, 2012, 58(6):1110-1120. [7] 李华,何幼斌,王英民,等.深水交互作用沉积研究进展——以南海北部珠江口盆地为例[J].岩性油气藏,2015,27(5):218-224. Li Hua, He Youbin, Wang Yingmin, et al.Research advances in deep water interaction deposition:A case from the Pearl River Mouth Basin, northern South China Sea[J].Lithologic Reservoirs, 2015, 27(5):218-224. [8] Shanmugam, Spalding T D, Rofheart D H.Process sedimentology and reservoir quality of deep-marine bottom-current reworked sands(sandy contourites):An example from the Gulf of Mexico[J].AAPG, 1993, 77(7):1241-1259. [9] Shanmugam G, Spalding T D, Rofheart D H.Traction structures in deep-marine, bottom-current-reworded sands in the Pliocene and Pleistocene, Gulf of Mexico[J].Geology, 1993, 21:929-932. [10] Gong C L, Wang Y M, Zheng R C, et al.Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin:Processes, genesis, and implications[J].Journal of Asian Earth Sciences, 2016,128:116-129. [11] 黄银涛,姚光庆,朱红涛,等.莺歌海盆地东方区黄流组重力流砂体的底流改造作用[J].石油学报,2016,37(7):854-866. Huang Yintao, Yao Guangqing, Zhu Hongtao, et al.Reworking of gravity flow sandbody by bottom-current from Huangliu Formation in Dongfang area of Yinggehai Basin, northwestern South China Sea[J].Acta Petrolei Sinica, 2016, 37(7):854-866. [12] Moraes M A S, Maciel W B, Braga M S S, et al.Bottom-current reworked Palaeocene-Eocene deep-water reservoirs of the Campos Basin, Brazil[M].in:Viana A R and Rebesco M (eds).Economic and palaeoceanographic significance of contourite deposits.London, Geological Society, 2007, 81-94. [13] Mitchum R M.Interaction between deepwater current drifts (contourites) and canyon fill-slope valley turbidites, Cretaceous and Tertiary sediments of offshore West Africa[C].AAPG 2014 annual convention & exhibition, USA, 2014, 06983. [14] 高振中,罗顺社,何幼斌,等.鄂尔多斯盆地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. [15] 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 characteristics of Middle Ordovician contour current deposits and geological implication in Fuping region, Shaanxi Province, China[J].Geological Bulletin of China, 2010, 29(9):1304-1309. [16] 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 western Huan and eastern Guizhou[J].Mineralogy and Petrology, 1990, 10(4):43-47. [17] Stow D A V, Fargères J C.Contour faces and the facies model[M].in:Rebesco M,Camerlenghi A (eds.).Contourites.Developments in sedimentology 60, the Great Britain, 2008, 223-256. [18] 吴胜和,冯增昭.鄂尔多斯盆地西缘及南缘中奥陶统平凉组重力流沉积[J].石油与天然气地质,1994,15(3):226-234. Wu Shenghe, Feng Zengzhao.Sedimentology of gravity flow deposits of Middle Ordovician Pingliang Formation in west and south Margins of Ordos[J].Oil & Gas Geology, 1994, 15(3):226-234. [19] 何幼斌,高振中,罗顺社,等.陕西陇县地区平凉组三段发现内潮汐沉积[J].石油天然气学报,2007,29(4):28-33. He Youbin, Gao Zhenzhong, Luo Shunshe, et al.Discovery of Internal-tide deposits from the Third Member of Pingliang Formation in Longxian area, Shaanxi province[J].Journal of Oil and Gas Technology, 2007, 29(4):28-33. [20] 李华,何幼斌,黄伟,等.鄂尔多斯盆地南缘奥陶系平凉组等深流沉积[J].古地理学报,2016,18(4):631-642. Li Hua, He Youbin, Huang Wei, et al.Contourites of the Ordovician Pingliang Formation in southern margin of Ordos Basin[J].Journal of Palaeogeography, 2016, 18(4):631-642. [21] 郭彦如,赵振宇,徐旺林,等.鄂尔多斯盆地奥陶系层序地层格架[J].沉积学报,2014,32(1):44-60. Guo Yanru, Zgao Zhenyu, Xu Wanglin, et al.Sequence Stratigraphy of the Ordovician system in the Ordos Basin[J].Acta sedimentologica Sinica, 2014, 32(1):44-60. [22] Song S G, Niu Y L, Su L, et al.Tectonics of the North Qilian orogen, NW China[J].Gondwana Research, 2013, 23:1378-1401. [23] 王振涛,周洪瑞,王训练,等.鄂尔多斯盆地西、南缘奥陶纪地质事件群耦合作用[J].地质学报,2015,89(11):1990-2004. Wang Zhentao, Zhou Hongrui, Wang Xunlian, et al.Ordovician geological events group in the west and south Ordos Basin[J].Acta Geologica Sinica, 2015, 89(11):1990-2004. [24] 陈小烩,牟传龙,周恳恳,等.鄂尔多斯西缘中晚奥陶世大坪阶-艾家阶岩相古地理[J].中国地质,2014,41(6):2028-2038. Chen Xiaowei, Mou Chuanlong, Zhou Kenken, et al.Lithofacies-paleogeography of middle-late Ordovician Daping stage-Aijiashan stage on the western margin of the Ordos Basin[J].Geology in China, 2014, 41(6):2028-2038. [25] 冯益民,何世平.祁连山及其邻区大地构造基本特征——兼论早古生代海相火山岩的成因环境[J].西北地质科学,1995,16(1):92-103. Feng Yimin, He Shiping.Basic characteristics of tectonics in the Qlian Mountains and its neighbourings-On genetic environment of Early Paleozoic margin volcanics[J].Northwest Geoscience, 1995, 16(1):92-103. [26] 鲍志东,朱井泉,江茂生,等.海平面升降中的元素地球化学响应——以塔中地区奥陶纪为例[J].沉积学报,1998,16(4):32-36. Bao Zhidong, Zhu Jingquan, Jiang Maosheng, et al.Isotope and trace element evolution:Responding to seal-level flucturation-An example of Ordovician in Middle Tarim Basin[J].Acta sedimentologica Sinica, 1998, 16(4):32-46. [27] Akarish A I M, El-Gohary A M.Petrography and geochemistry of lower Paleozoic sandstones, East Sinai, Egypt:implications for provenance and tectonic setting[J].Journal of African Earth Sciences, 2008, 52:43-54. [28] 田洋,赵小明,王令占,等.重庆石柱二叠纪栖霞组地球化学特征及其环境意义[J].沉积学报,2014,32(6):1035-1045. Tian Yang, Zhao Xiaoming, Wang Lingzhan, et al.Geochemical characteristics and its paleoenvironmental implication of Permian Qixia formation in Shizhu, Chongqing[J].Acta Sedimentologica Sinica, 2014, 32(6):1035-1045. [29] Couch E L.Calculation of paleosalinities from boron and clay mineral data[J].AAPG Bulletin, 1971, 55(10):1829-1837. [30] 柏道远,周亮,王先辉,等.湘东南南华系-寒武系砂岩地球化学特征及对华南新元古代-早古生代构造背景的制约[J].地质学报,2007,81(6):755-771. Bai Daoyuan, Zhou Liang, Wang Xianhui, et al.Geochemistry of Nanhuan-Cambrian sandstones in southeastern Hunan, and its constraints on Neoproterozoic-Early Paleozoic tectonic setting of South China[J].Acta Geologica Sinica, 2007, 81(6):755-771. [31] Heezen B, Hollister C.Deep sea current evidence from abyssal sediment[J].Marine Geology, 1964, 1:141-174. [32] 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 [33] 席胜利,李振宏,王欣,等.鄂尔多斯盆地奥陶系储层展布及勘探潜力[J].石油与天然气地质,2006,27(3):405-412. Xi Shengli, Li Zhenghong, Wang Xin, et al.Distribution and exploration potential of Ordovician reservoir in Ordos basin[J].Oil & Gas Geology, 2006, 27(3):405-412. [34] 李华,何幼斌,刘朱睿鸷,等.鄂尔多斯盆地西南缘奥陶系平凉组重力流沉积特征[J].中国科技论文,2017,12(15):1774-1779. Li Hua, He Youbin, Liu Zhuruizhi, et al.Characteristic of gravity flow deposit in Pingliang Formation of Ordovician in the southwest magrin of the Ordos Basin[J].China Sciencepaper, 2017, 12(15):1774-1779. [35] 徐焕华,杨忠芳,丁海军.贺兰拗拉谷北段奥陶系等深流烃源岩[J].西部探矿工程,2008,(3):88-90. Xu Huanhua, Yang Zhongfang, Ding Haijun.Contourite source rocks of Ordovician in north part of Helan Aulacogen[J].West Exploration Engineering, 2008, (3):88-90. [36] 丁海军,孟祥华,葛铭,等.贺兰拗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 of Helan Aulacogen[J].Journal of Earth Sciences and Environment, 2009, 31(1):58-64. [37] 张月巧,郭彦如,侯伟,等.鄂尔多斯盆地西南缘中上奥陶统烃源岩特征及勘探潜力[J].天然气地球科学,2013,24(5):894-904. Zhang Yueqiao, Guo Yanru, Hou Wei, et al.Geochemical characteri-stics and exploration potential of the Middle-Upper Ordovician source rocks on the western and southern margin of Ordos Basin[J].Natural Gas Geoscience, 2013, 24(5):894-904. |
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