Discovery and characteristics of coated gravels and coated conglomerates from the Ordovician karst cave and sediment in northern margin of Tarim Basin
Zhong Jianhua1, Ni Liangtian1, Cao Mengchun1, Chen Xin2, Zhang Danfeng3, Sun Ningliang1, Hao Bing1, Liu Chuang1, Shao Zhufu4, Niu Yongbin5
1 School of Geosciences,China University of Petroleum(East China),Qingdao 266580,Shandong; 2 BGP Geophysical Research Institute,CNPC,Zhuozhou 072751,Hebei; 3 Research Institute of Petroleum Exploration &Development,PetroChina, Beijing 100083; 4 Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong; 5 Institute of Resources and Environment,Henan Polytechnic University,Jiaozuo 454000,Henan;
Abstract Coated gravels and coated conglomerates, a specific type of sediment from karst caves and palaeokarsts,were found in the Ordovician in northern margin of Tarim Basin. These coated gravels and coated conglomerates,not been documented previously,are characterized by oolith- or oncolite-like textures,i.e.,a core and coat around the core. The core is divided into four types:(1)limestone gravel identical to the country rock of the karst cave;(2)core composed of sandstone;(3)composite core of conglomerates and(4)core comprised by palaeotravertine clasts. The coat is also divided into four types:(1)coat with cycles;(2)granular coat;(3)homogeneous coat and(4)composite coat comprised by granular coats and cycle-like coats. Coated gravels and coated conglomerates are typical products of karst caves and palaeokarsts, which can be served as markers of the presence of karsts and karst caves. Furthermore,the inherent storage capability in coated gravels and coated conglomerates make them effective hydrocarbon reservoirs,and thus a target for oil and gas exploration and development.
Fund:; [Co-funded by the National Natural Science Foundation of China(No.41172093),National Major Fundamental Research Program(No.2006CB202401)and National Major Projects of Oil and Gas(No.2008ZX05014-002-002HZ)
Corresponding Authors:
Zhong Jianhua,born in 1958,is a professor and Ph.D. supervisor in China University of Petroleum(East China). He is engaged in sedimentology and structural geology. E-mail: zhongjh@upc.edu.cn.
Cite this article:
Zhong Jianhua,Ni Liangtian,Cao Mengchun et al. Discovery and characteristics of coated gravels and coated conglomerates from the Ordovician karst cave and sediment in northern margin of Tarim Basin[J]. JOPC, 2016, 18(5): 721-730.
Zhong Jianhua,Ni Liangtian,Cao Mengchun et al. Discovery and characteristics of coated gravels and coated conglomerates from the Ordovician karst cave and sediment in northern margin of Tarim Basin[J]. JOPC, 2016, 18(5): 721-730.
[1] 顾家裕. 1999. 塔里木盆地轮南地区下奥陶统碳酸盐岩岩溶储集层特征及形成模式. 古地理学报,1(1):54-60. [Gu J Y. 1999. Characteristics and evolutional model of karst reservoirs of lower Ordovician carbonate rocks in Lunnan area of Tarim Basin. Journal of Palaeogeography(Chinese Edition),1(1):54-60] [2] 何治亮,陈强路,钱一雄,李慧莉. 2006. 塔里木盆地中央隆起区油气勘探方向. 石油与天然气地质,27(6):769-778. [He Z L,Chen Q L,Qian Y X,Li H L. 2006. Hydrocarbon exploration targets in central uplift area of Tarim Basin. Oil and Gas Geology,27(6):769-778] [3] 贾承造. 1999. 塔里木盆地构造特征与油气聚集规律. 新疆石油地质,20(3):177-268. [Jia C Z. 1999. Structural characteristics and oil/gas accumulative regularity in Tarim Basin. Xinjiang Petroleum Geology,20(3):177-268] [4] 金之钧. 2005. 中国典型叠合盆地及其油气成藏研究新进展(之一):叠合盆地划分与研究方法. 石油与天然气地质,26(5):553-562. [Jin Z J. 2005. New advancement in research of China’s typical superimposed basins and reservoiring(Part Ⅰ):Classification and research method of superimposed basins. Oil and Gas Geology,26(5):553-562] [5] 康玉柱. 2000. 塔里木盆地油气藏(田)特征. 石油实验地质,22(2):115-120. [Kang Y Z. 2000. Some characteristics of oil fields in the Tarim Basin. Petroleum Geology & Experiment,22(2):115-120] [6] 李华举,廖长君,姜殿强,姜光辉. 2006. 钙华沉积机制的研究现状及展望. 中国岩溶,25(1):57-62. [Li H J,Liao C J,Jiang D Q,Jiang G H. 2006. The status quo and prospect of research on travertine precipitation menchanism. Carsologica Sinica,25(1):57-62] [7] 刘再华. 2014. 表生和内生钙华的气候环境指代意义研究进展. 科学通报,59(23):2229-2239. [Liu Z H. 2014. Research progress in paleoclimatic interpretations of tufa and travertine. Chinese Science Bulletin,59(23):2229-2239] [8] 刘再华,袁道先,Dreybrodt W,Svesson U. 1993. 四川黄龙钙华的形成. 中国岩溶,12(3):185-191. [Liu Z H,Yuan D X,Dreybrodt W,Svesson U. 1993. The formation of tufa in Huanglong,Sichuan. Carsologica Sinica,12(3):185-191] [9] 刘再华,袁道先,何师意,曹建华,游省易. 2003. 四川黄龙沟景区钙华的起源和形成机理研究. 地球化学,32(1):1-10. [Liu Z H,Yuan D X,He S Y,Cao J H,You S Y. 2003. Origin and forming mechanisms of travertine at Huanglong Ravine of Sichuan. Geochimica,32(1):1-10] [10] 孙龙德,周新源,王国林. 2005. 塔里木盆地石油地质研究新进展和油气勘探主攻方向. 地质科学,40(2):167-178. [Sun L D,Zhou X Y,Wang G L. 2005. Contributions of petroleum geology and main directions of oil-gas exploration in the Tarim Basin. Chinese Journal of Geology,40(2):115-120] [11] 田在艺,柴桂林,林梁怜. 1985. 塔里木盆地地质构造演化与含油气展望. 石油与天然气地质,6(3):250-259. [Tian Z Y,Chai G L,Lin L L. 1985. Tectonic evolution of Tarim Basin and its hydrocarbon potential. Oil and Gas Geology,6(3):250-259] [12] 张英骏,莫仲达. 1982. 黄果树瀑布成因初探. 地理学报,37(3):304-316. [Zhang Y J,Mo Z D. 1982. The origin and evolution of Huangguoshu rainfall. Acta Geographica Sinca,37(3):304-316] [13] 钟建华,毛毳,李阳,袁向春,王书宝,牛永斌. 2014. 塔里木盆地奥陶系碳酸盐岩储集空间的研究. 北京:石油工业出版社. [Zhong J H,Mao C,Li Y,Yuan X C,Wang S B,Niu Y B. 2014. Characteristics of the Ordovician Carbonate Reservoir Space in Tarim Basin. Beijing:Petroleum Industry Press] [14] 钟建华,毛毳,李勇,李阳,袁向春,牛永斌,陈鑫,黄知娟,邵珠福,王培俊,李佳,张丹峰. 2012. 塔北硫磺沟奥陶系含油古溶洞的发现及意义. 中国科学:地球科学,42(11):1660-1680. [Zhong J H,Mao C,Li Y,Li Y,Yuan X C,Niu Y B,Chen X,Hang Z J,Shao Z F,Wang P J,Li J,Zhang D F. 2012. Discovery of the ancient Ordovician oil-bearing karst cave in Liuhuanggou,North Tarim Basin,and its significance. Scientia Sinica Terrae,42(11):1660-1680] [15] 朱学稳,周绪伦. 1990. 岷山岩溶区的灰华沉积. 中国岩溶,9(3):250-264. [Zhu X W,Zhou X L. 1990. Deposition of travertines in karst area of Minshan Mt.. Carsologica Sinica,9(3):250-264] [16] Du J H,Zhou X Y,Li Q M,Wu G H,Pan W Q,Yang T. 2011. Characteristics and controlling factors of the large carbonate petroleum province in the Tarim Basin,NW China. Petroleum Exploration and Development,38(6):652-661. [17] Liu Z H,Svesson U,Dreybrodt W,Yuan D X,Buhmann D. 1995. Hydrodynamic control of inorganic calcite precipitation in Huanglong Ravine,China:Field measurements and theoretical prediction of deposition rates. Geochimica et Cosmochimica Acta,59:3087-3097. [18] Liu Z H,Dreybrodt W. 1997. Dissolution kinetics of calcium carbonate minerals in H 2 O-CO 2 solutions in turbulent flow:The role of the diffusion boundary layer and the slow reaction H 2 O+CO 2 H + +HC O 3 - . Geochimica et Cosmochimica Acta,61:2879-2889.