塔北哈拉哈塘油田奥陶系岩溶储层发育模式

doi:10.7623/syxb201511007

石油学报 ›› 2015, Vol. 36 ›› Issue (11): 1380-1391.DOI: 10.7623/syxb201511007

塔北哈拉哈塘油田奥陶系岩溶储层发育模式

廖涛¹, 侯加根¹, 陈利新², 马克¹, 杨文明², 董越¹

1. 中国石油大学地球科学学院北京 102249;
2. 中国石油塔里木油田公司新疆库尔勒 841000

收稿日期:2015-04-14 修回日期:2015-08-21 出版日期:2015-11-25 发布日期:2015-12-05
通讯作者: 侯加根,男,1963年9月生,1985年获华东石油学院学士学位,1997年获石油大学(北京)博士学位,现为中国石油大学(北京)地球科学学院教授、博士生导师,主要从事油气田开发地质方面的研究和教学工作。Email:houjg63@cup.edu.cn
作者简介:廖涛,男,1966年9月生,1988年获新疆石油学院学士学位,现为中国石油大学(北京)地球科学学院博士研究生,主要从事石油地质方面的研究。Email:liaotao1967@126.com
基金资助:
国家重点基础研究发展计划(973)项目(2011CB201003)和国家重大科技专项(2011ZX05014-002)资助。

Evolutionary model of the Ordovician karst reservoir in Halahatang oilfield, northern Tarim Basin

Liao Tao¹, Hou Jiagen¹, Chen Lixin², Ma Ke¹, Yang Wenming², Dong Yue¹

1. College of Geosciences, China University of Petroleum, Beijing 102249, China;
2. PetroChina Tarim Oilfield Company, Xinjiang Korla 841000, China

Received:2015-04-14 Revised:2015-08-21 Online:2015-11-25 Published:2015-12-05

摘要/Abstract

摘要：

针对碳酸盐岩缝洞型储层发育随机性强的特点,通过对哈拉哈塘油田哈601井区进行详细解剖,在充分认识不同时期古地貌及构造运动背景的基础上,通过动、静态多类型储层预测,以塔北奥陶系古岩溶露头认知为指导,将储集体细分为暗河管道厅堂洞、断裂明河双控洞穴、断控洞穴、早期裂缝-孔洞和微裂缝-孔洞共5种成因类型;并依据储集体形态规模及发育规律,明确了研究区最重要的岩溶发育地质控制因素为良里塔格组古地貌古水系、地层岩性、加里东中期和加里东晚期-海西早期断裂。各缝洞系统先后经历了加里东中期断裂发育、良里塔格组水系下切、晚加里东期-早海西期断裂发育3个主要过程,经过后期一定程度改造形成了现今缝洞体形态。同时明确了岩溶内幕区不同缝洞系统对于油井产能的控制,为类似区块的井位部署及开发提供了地质依据。

关键词: 塔里木盆地, 哈拉哈塘油田, 岩溶储层, 控制因素, 发育模式

Abstract:

The development of fracture-vug carbonate reservoirs shows great randomness. According to this characteristic, through detailed analysis of Ha 601 well block in Halahatang oilfield, dynamic and static multi-type reservoir prediction was carried out based on a thorough understanding of paleo-geomorphology and tectonism background in different geological periods. On this basis, under the guidance of the understanding of paleo-karst outcrops in northern Tarim Basin, reservoir bodies were divided into five genetic types, i.e., underground-river tubulose hall caves, fault and river-controlled caves, fault-controlled caves, early fracture-vug and micro fracture-vug. According to morphological scale and development rule of reservoir bodies, the most important geological control factors for karst development in the study area were clarified, including paleo-geomorphology water system and formation lithology of Lianglitag Formation as well as the faults formed in the middle Caledonian and late Caledonian-early Hercynian. The fracture-vug system experienced three major processes, i.e., fault development in middle Caledonian, river incision in Lianglitag Formation, and fault development in late Caledonian-early Hercynian. Current fracture-vug morphologies were formed through a certain degree of reformation in the late period. Meanwhile, the control of various fracture-vug systems on oil well capacity in buried hill karst area was clarified, thus providing a geological basis for well location arrangement and development in similar blocks.

Key words: Tarim Basin, Halahatang oilfield, karst reservoirs, coutrol factors, evolutionary model

中图分类号:

TE122.2

廖涛, 侯加根, 陈利新, 马克, 杨文明, 董越. 塔北哈拉哈塘油田奥陶系岩溶储层发育模式[J]. 石油学报, 2015, 36(11): 1380-1391.

Liao Tao, Hou Jiagen, Chen Lixin, Ma Ke, Yang Wenming, Dong Yue. Evolutionary model of the Ordovician karst reservoir in Halahatang oilfield, northern Tarim Basin[J]. Acta Petrolei Sinica, 2015, 36(11): 1380-1391.

参考文献

[1] 沈安江,潘文庆,郑兴平,等.塔里木盆地下古生界岩溶型储层类型及特征[J].海相油气地质,2010,15(2):20-29.
Shen Anjiang,Pan Wenqing,Zheng Xingping,et al.Types and characteristics of Lower Palaeozoic karst reservoirs in Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(2):20-29.
[2] 张宝民,刘静江.中国岩溶储集层分类与特征及相关的理论问题[J].石油勘探与开发,2009,36(1):12-29.
Zhang Baomin,Liu Jingjiang.Classification and characteristics of karst reservoirs in China and related theories[J].Petroleum Exploration and Development,2009,36(1):12-29.
[3] 张丽娟,范秋海,朱永峰,等.塔北哈6区块奥陶系油藏地质与成藏特征[J].石油地质,2013,2(2):7-12.
Zhang Lijuan,Fan Qiuhai,Zhu Yongfeng,et al.Geological and accumulations characteristics of Ordovician oil reservoir in Ha 6 block of Tabei[J].Petroleum Geology,2013,2(2):7-12.
[4] 倪新峰,张丽娟,沈安江,等.塔北地区奥陶系碳酸盐岩古岩溶类型、期次及叠合关系[J].中国地质,2009,36(6):1312-1321.
Ni Xinfeng,Zhang Lijuan,Shen Anjiang,et al.Paleo-karstification types,karstification periods and superimposition relationship of Ordovician Carbonates in Northern Tarim Basin[J].Geology in China,2009,36(6):1312-1321.
[5] 张学丰,李明,陈志勇,等.塔北哈拉哈塘奥陶系碳酸盐岩岩溶储层发育特征及主要岩溶期次[J].岩石学报,2012,28(3):815-826.
Zhang Xuefeng,Li Ming,Chen Zhiyong,et al.Characteristics and karstification of the Ordovician carbonate reservoir,Halahatang area,northern Tarim Basin[J].Acta Petrologica Sinica,2012,28(3):815-826.
[6] 杜金虎,王招明,李启明,等.塔里木盆地寒武-奥陶系碳酸盐岩油气勘探[M].北京:石油工业出版社,2010:1-82.
Du Jinhu,Wang Zhaoming,Li Qiming,et al.Oil and gas exploration of Cambrian-Ordovician carbonate in Tarim Basin[M].Beijing:Petroleum Industry Press,2010:1-82.
[7] 倪新峰,张丽娟,沈安江,等.塔里木盆地英买力-哈拉哈塘地区奥陶系岩溶储集层成岩作用及孔隙演化[J].古地理学报,2010,12(4):467-479.
Ni Xinfeng,Zhang Lijuan,Shen Anjiang,et al.Diagenesis and pore evolution of the Ordovician karst reservoir in Yengimahalla-Hanilcatam region of Tarim Basin[J].Journal of Palaeogeography,2010,12(4):467-479.
[8] 马晓强,侯加根,胡向阳,等.塔里木盆地塔河油田奥陶系断控型大气水岩溶储层结构研究[J].地质论评,2013,59(3):521-532.
Ma Xiaoqiang,Hou Jiagen,Hu Xiangyang,et al.Framework of fault-controlled meteoric palaeokarst Ordovician reservoirs in Tahe Oilfield,Tarim Basin[J].Geological Review,2013,59(3):521-532.
[9] 金强,田飞.塔河油田岩溶型碳酸盐岩缝洞结构研究[J].中国石油大学学报:自然科学版,2013,37(5):15-21.
Jin Qiang,Tian Fei.Investigation of fracture-cave constructions of karsted cabonate reservoirs of Ordovician in Tahe Oilfield,Tarim Basin[J].Journal of China University of Petroleum:Edition of Natural Sciences,2013,37(5):15-21.
[10] 杨鹏飞,张丽娟,郑多明,等.塔里木盆地奥陶系碳酸盐岩大型缝洞集合体定量描述[J].岩性油气藏,2013,25(6):89-94.
Yang Pengfei,Zhang Lijuan,Zheng Duoming,et al.Quantitative characterization of Ordovician carbonate fracture-cavity aggregate in Tarim Basin[J].Lithologic Reservoirs,2013,25(6):89-94.
[11] 倪新峰,张丽娟,沈安江,等.塔里木盆地英买力-哈拉哈塘地区奥陶系碳酸盐岩岩溶型储层特征及成因[J].沉积学报,2011,29(3):465-474.
Ni Xinfeng,Zhang Lijuan,Shen Anjiang,et al.Characteristics and genesis of Ordovician carbonate karst reservoir in Yingmaili-Halahatang Area,Tarim Basin[J].Acta Sedimentologica Sinica,2011,29(3):465-474.
[12] 高计县,唐俊伟,张学丰,等.塔北哈拉哈塘地区奥陶系一间房组碳酸盐岩岩心裂缝类型及期次[J].石油学报,2012,33(1):64-73.
Gao Jixian,Tang Junwei,Zhang Xuefeng,et al.Types and episodes of fractures in carbonate cores from the Ordovician Yijianfang Formation in the Halahatang area,northern Tarim Basin[J].Acta Petrolei Sinica,2012,33(1):64-73.
[13] 姜华,张艳秋,潘文庆,等.塔北隆起英买2井区碳酸盐岩储层特征及岩溶模式[J].石油学报,2013,34(2):232-238.
Jiang Hua,Zhang Yanqiu,Pan Wenqing,et al.Carbonate reservoir features and karst mode in the Yingmai-2 well field of Tabei uplift[J].Acta Petrolei Sinica,2012,34(2):232-238.
[14] 苏劲,张水昌,杨海军,等.断裂系统对碳酸盐岩有效储层的控制及其成藏规律[J].石油学报,2010,31(2):196-203.
Su Jin,Zhang Shuichang,Yang Haijun,et al.Control of fault system to formation of effective carbonate reservoir and the rules of petroleum accumulation[J].Acta Petrolei Sinica,2010,31(2):196-203.
[15] 邬光辉,陈志勇,曲泰来,等.塔里木盆地走滑带碳酸盐岩断裂相特征及其与油气关系[J].地质学报,2012,86(2):219-227.
Wu Guanghui,Chen Zhiyong,Qu Tailai,et al.Characteristics of the strik-slip fault facies in Ordovician carbonate in the Tarim Basin,and its relations to hydrocarbon[J].Acta Geologica Sinica,2012,86(2):219-227.
[16] 朱光有,杨海军,朱永峰,等.塔里木盆地哈拉哈塘地区碳酸盐岩油气地质特征与富集成藏研究[J].岩石学报,2011,27(3):827-844.
Zhu Guangyou,Yang Haijun,Zhu Yongfeng,et al.Study on petroleum geological characteristics and accumulation of carbonate reservoirs in Hanilcatam area,Tarim Basin[J].Acta Petrologica Sinica,2011,27(3):827-844.
[17] 崔海峰,郑多明,滕团余.塔北隆起哈拉哈塘凹陷石油地质特征与油气勘探方向[J].岩性油气藏,2009,21(2):54-58.
Cui Haifeng,Zheng Duoming,Teng Tuanyu.Petroleum geologic characteristics and exploration orientation in Halahatang depression of Tabei uplift[J].Lithologic Reservoirs,2009,21(2):54-58.
[18] 任美锷,刘振中,王飞燕.岩溶学概论[M].北京:商务印书馆,1983:3-33.
Ren Mei'e,Liu Zhenzhong,Wang Feiyan.Overview of karst study[M].Beijing:The Commercial Press,1983:3-33.
[19] Loucks R G.Paleocave carbonate reservoirs; origins,burial-depth modifications,spatial complexity,and reservoir implications[J].AAPG Bulletin,1999,83(11):1795-1834.
[20] 李阳,范智慧.塔河奥陶系碳酸盐岩油藏缝洞系统发育模式与分布规律[J].石油学报,2011,32(1):101-106.
Li Yang,Fan Zhihui.Developmental pattern and distribution rule of the fracture-cavity system of Ordovician carbonate reservoirs in the Tahe oilfield[J].Acta Petrolei Sinica,2011,32(1):101-106.
[21] 吴东胜,张玉清,刘少华,等.塔里木盆地轮古西潜山油气运聚及分布机理[J].石油学报,2006,27(5):41-45.
Wu Dongsheng,Zhang Yuqing,Liu Shaohua,et al.Oil-gas migration and distribution mechanism of Lunguxi buried hill in Tarim Basin[J].Acta Petrolei Sinica,2006,27(5):41-45.
[22] Mylroie J E,Carew J L.Karst development on Carbonate Islands[M]//Budd D A,Saller A H,Harris P M.Unconformities and porosity in carbonate strata.American Association of Petroleum Geologists,Memoir,1995:55-76.
[23] 赵宗举.全球海平面变化指标及海相构造层序研究方法:以塔里木盆地奥陶系为例[J].石油学报,2015,36(3):262-273.
Zhao Zongju.Indicators of global sea-level change and research methods of marine tectonic sequences:take Ordovician of Tarim Basin as an example[J].Acta Petrolei Sinica,2015,36(3):262-273.
[24] 鲍志东,金之钧,孙龙德,等.塔里木地区早古生代海平面波动特征:来自地球化学及岩溶的证据[J].地质学报,2006,80(3):366-373.
Bao Zhidong,Jin Zhijun,Sun Longde,et al.Sea-level fluctuation of the Tarim area in the early paleozoic:respondence from geochemistry and karst[J].Acta Geologica Sinica,2006,80(3):366-373.
[25] 俞仁连,闫相宾,金晓辉,等.塔里木盆地研究进展与勘探方向[J].石油与天然气地质,2005,26(5):598-604.
Yu Renlian,Yan Xiangbin,Jin Xiaohui,et al.Research achievements and exploration direction in Tarim Basin[J].Oil & Gas Geology,2005,26(5):598-604.
[26] 徐国强,刘树根,李国蓉,等.塔中、塔北古隆起形成演化及油气地质条件对比[J].石油与天然气地质,2005,26(1):114-119.
Xu Guoqiang,Li Shugen,Li Guorong,et al.Comparison of tectonic evolutions and petroleum geological conditions in Tazhong and Tabei palaeohighs in Tarim Basin[J].Oil & Gas Geology,2005,26(1):114-119.
[27] 张一伟,金之钧,刘国臣,等.塔里木盆地环满加尔地区主要不整合形成过程及剥蚀量研究[J].地学前缘,2000,7(4):449-457.
Zhang Yiwei,Jin Zhijun,Liu Guochen,et al.Study on the formation of unconformaties and the amount of eroded sedimentation in Tarim Basin[J].Earth Science Frontiers,2000,7(4):449-457.
[28] 孙龙德.塔里木含油气盆地沉积学研究进展[J].沉积学报,2004,22(3):408-416.
Sun Longde.Progress of sedimentological research in Tarim Basin[J].Acta Sedimentologica Sinica,2004,22(3):408-416.
[29] 康玉柱.塔里木盆地塔河大油田形成的地质条件及前景展望[J].中国地质,2003,30(3):315-319.
Kang Yuzhu.Geological characteristics of the formation of the large Tahe oilfield in the Tarim Basin and its prospects[J].Geology in China,2003,30(3):315-319.
[30] 乔占峰,沈安江,邹伟宏,等.断裂控制的非暴露型大气水岩溶作用模式:以塔北英买2构造奥陶系碳酸盐岩储层为例[J].地质学报,2011,85(12):2070-2083.
Qiao Zhanfeng,Shen Anjiang,Zou Weihong,et al.A fault-controlled non-exposed meteoric karstification:a case study of Ordovician carbonate reservoir at Structure YM2 in northern Tarim Basin,northwestern China[J].Acta Geologica Sinica,2011,85(12):2070-2083.
[31] 汤良杰,漆立新,邱海峻,等.塔里木盆地断裂构造分期差异活动及其变形机理[J].岩石学报,2012,28(8):2569-2583.
Tang Liangjie,Qi Lixin,Qiu Haijun,et al.Poly-phase differential fault movement and hydrocarbon accumulation of the Tarim Basin,NW China[J].Acta Petrologica Sinica, 2012,28(8):2569-2583.
[32] 刘学锋,彭德堂,刘绍平,等.塔北隆起构造格架及其成因[J].江汉石油学院学报,1996,18(4):26-30.
Liu Xuefeng,Peng Detang,Liu Shaoping,et al.Structural frame-work and origin of the northern Tarim uplift[J].Journal of Jianghan Petroleum Institute,1996,18(4):26-30.
[33] 周文,李秀华,金文辉,等.塔河奥陶系油藏断裂对古岩溶的控制作用[J].岩石学报,2011,27(8):2339-2348.
Zhou Wen,Li Xiuhua,Jin Wenhui,et al.The control action of fault to paleokarst in view of Ordovician reservoir in Tahe area[J].Acta Petrologica Sinica,2011,27(8):2339-2348.
[34] Loucks R G,Mescher P K,McMechan G A.Three-dimensional architecture of a coalesced,collapsed-paleocave system in the Lower Ordovician Ellenburger Group,central Texas[J].AAPG Bulletin,2004,88(5):545-564.
[35] 张光亚,赵文智,王红军,等.塔里木盆地多旋回构造演化与复合含油气系统[J].石油与天然气地质,2007,28(5):653-663.
Zhang Guangya,Zhao Wenzhi,Wang Hongjun,et al.Multicycle tectonic evolution and composite petroleum systems in the Tarim Basin[J].Oil & Gas Geology,2007,28(5):653-663.

塔北哈拉哈塘油田奥陶系岩溶储层发育模式

Evolutionary model of the Ordovician karst reservoir in Halahatang oilfield, northern Tarim Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	黄亚浩, 汪如军, 文志刚, 张银涛, 崔仕提, 李梦勤, 王彭, 何涛华. 塔里木盆地富满油田深层—超深层油气成藏过程[J]. 石油学报, 2024, 45(6): 947-960.
[2]	杨德彬, 何新明, 张恒, 汪彦, 刘遥, 王明. 塔河油田主体区奥陶系表层岩溶带智能识别及缝洞发育规律[J]. 石油学报, 2024, 45(2): 374-389,411.
[3]	王清华, 徐振平, 张荣虎, 杨海军, 杨宪彰. 塔里木盆地油气勘探新领域、新类型及资源潜力[J]. 石油学报, 2024, 45(1): 15-32.
[4]	郭秋麟, 黄少英, 卢玉红, 王建, 吴晓智, 陈宁生. 塔里木盆地台盆区下古生界油气系统模拟及资源分布预测[J]. 石油学报, 2023, 44(9): 1459-1471.
[5]	陈利新, 贾承造, 姜振学, 苏洲, 杨美纯, 杨博, 邱晨. 塔里木盆地哈拉哈塘地区碳酸盐岩富油模式与主控因素[J]. 石油学报, 2023, 44(6): 948-961.
[6]	蔡国富, 彭光荣, 吴静, 白海军, 李振升, 汪晓萌, 杜晓东, 熊万林. 珠江口盆地阳江凹陷始新统古湖泊环境与优质烃源岩发育模式[J]. 石油学报, 2023, 44(5): 809-825.
[7]	孔悦, 高晓鹏, 石开波, 刘波, 姜伟民, 于进鑫, 何卿, 吴淳. 塔北地区奥陶系鹰山组斑状白云岩成因及储层意义[J]. 石油学报, 2023, 44(4): 598-611.
[8]	申威, 唐军, 信毅, 曹磊, 陈文迪, 唐保勇, 何泽, 齐戈为. 塔里木盆地北部潜山岩溶相带定量表征与储层评价[J]. 石油学报, 2023, 44(3): 471-484.
[9]	杨焦生, 冯鹏, 唐淑玲, 汤达祯, 王玫珠, 李松, 赵洋, 李站伟. 大宁—吉县区块深部煤层气相态控制因素及含量预测模型[J]. 石油学报, 2023, 44(11): 1879-1891.
[10]	云露, 邓尚. 塔里木盆地深层走滑断裂差异变形与控储控藏特征——以顺北油气田为例[J]. 石油学报, 2022, 43(6): 770-787.
[11]	马安来, 林会喜, 云露, 邱楠生, 朱秀香, 吴鲜. 塔里木盆地顺托果勒地区奥陶系原油中乙基桥键金刚烷系列的检出及意义[J]. 石油学报, 2022, 43(6): 788-803.
[12]	李斌, 张欣, 郭强, 吕海涛, 杨素举, 徐勤琪, 彭军. 塔里木盆地寒武系超深层含油气系统盆地模拟[J]. 石油学报, 2022, 43(6): 804-815.
[13]	黄渊, 段太忠, 樊太亮, 刘彦锋, 沈禄银, 张文彪, 李蒙, 张德民. 塔河地区寒武纪碳酸盐岩台地沉积演化史与成因机制——来自地层沉积正演模拟的启示[J]. 石油学报, 2022, 43(5): 617-636.
[14]	吴鲜, 李丹, 韩俊, 朱秀香, 黄诚, 曹自成, 常健, 刘雨晨. 塔里木盆地顺托果勒北部地区超深层现今地温场特征[J]. 石油学报, 2022, 43(1): 29-40.
[15]	白莹, 李建忠, 刘伟, 徐兆辉, 徐旺林, 李欣, Abitkazy Taskyn. 塔里木盆地西北部下寒武统白云岩特征及多重白云石化模式[J]. 石油学报, 2021, 42(9): 1174-1191.