渤中凹陷古生界碳酸盐岩潜山气藏储层特征及主控因素CHARACTERISTICS AND MAIN CONTROLLING FACTORS OF PALEOZOIC CARBONATE BURIED-HILL GAS RESERVOIRS IN BOZHONG SAG
邓吉锋,史浩,王保全,王改卫,陈国童
DENG Jifeng,SHI Hao,WANG Baoquan,WANG Gaiwei,CHEN Guotong
摘要(Abstract):
渤海盆地渤中凹陷BZ21构造区发现了一个10×10~8m~3方级别的古生界碳酸盐岩潜山气藏。根据岩心观察、岩石薄片、铸体薄片、成像测井、常规测井、分析化验及地震等资料,对潜山气藏的储集层演化特征、储集空间类型及形成主控因素进行了分析。研究认为:加里东运动使华北地台整体抬升,形成大型古潜山并长期遭受风化剥蚀,在大气淡水淋滤作用下,形成大量溶蚀孔、洞,水沿着早期岩溶作用所形成的孔隙层渗滤,形成顺层岩溶,改善了储层的横向连通性;碳酸盐岩储层的储集层空间类型主要为溶孔、溶洞及裂缝,成岩作用和构造裂缝是储层的主控因素;碳酸盐岩潜山纵向上可划分为垂直渗流带、水平潜流带及深度缓流带。
One-billion-cubic-meter Paleozoic carbonate buried-hill gas reservoirs are discovered in Structural Area BZ21 of Bozhong Sag of Bohai Bay.According to the following data such as the core observation,rock slices,cast thin sections,imaging logging,conventional loggings,analysis-test,and seismic survey and so on,the reservoir evolutional characteristics,AS types and their main controlling factors are analyzed.The studies show that Caledonian orogeny makes the whole uplift of North China Platform and formation of large-size paleo-buried hill and sufferance of long-period weathering and erosion;under the conditions of the air and fresh water leaches,a great number of dissolved pores and caves are induced,and moreover the karsts along the formations are resulted from the leach of the water along the stimulated porous zones by the early diagenesis,thus the horizontal connectivity of the reservoirs is improved;the AS types of the carbonate reservoirs are mainly dissolved pores,caves and various cracks,the diagenesis and structural fractures are the principal controlling factors of the reservoirs;the buried hill can be vertically divided into vertical seepage belts,horizontal undercurrent belts and deep slow-flow belts.
关键词(KeyWords):
渤中凹陷;碳酸盐岩;潜山气藏;储集空间类型;成岩作用;构造裂缝
Bozhong Sag;carbonate rock;buried-hill gas reservoir;accumulation space(AS) type;diagenesis;structural fracture
基金项目(Foundation): 国家科技重大专项“近海大中型油气田形成条件及勘探技术”(2011ZX05023-002)
作者(Author):
邓吉锋,史浩,王保全,王改卫,陈国童
DENG Jifeng,SHI Hao,WANG Baoquan,WANG Gaiwei,CHEN Guotong
参考文献(References):
- [1]王学军.碳酸盐岩潜山有利储集层预测[M].北京:石油工业出版社,2008.
- [2]吕坐彬,赵春明,张迎春,等.裂缝性潜山油藏裂缝发育规律及其对井位部署的指导[J].大庆石油地质与开发,201 1,23(6):75-79.
- [3]吴李泉,郑玉梅,曹代勇,等.千米桥潜山构造特征及其在油气成藏中的作用[J].石油勘探与开发,2002,29(4):38-40.
- [4]隋少强,曹思远,王允诚,等.潜山灰岩溶蚀和裂缝的特征参数应用[J].大庆石油地质与开发,2003,22(6):5-7.
- [5]官大勇,王应斌,王永利,等.渤海海域PL花岗岩潜山油藏储集层特征[J].大庆石油地质与开发,2012,31(2):48-51.
- [6]付崇清.辽河油田变质岩潜山测井综合评价[J].大庆石油地质与开发,2007,26(5):138-142.
- [7]王占忠.中央凸起变质岩古潜山内幕油气成藏条件[J].大庆石油地质与开发,2011,30(4):9-13.
- [8]刘宏,蔡正期,谭秀成,等.川东高陡构造薄层碳酸盐岩裂缝性储集层预测[J].石油勘探与开发,2008,35(4):431-436.
- [9]王光付.碳酸盐岩溶洞型储层综合识别及预测方法[J].石油学报,2008,29(1):47-50.
- [10]肖淑蓉,张跃明.辽河盆地基岩潜山油藏裂缝型储集层特征[J].中国海上油气,2000,14(2):108-111.
- [11]周心怀,项华.渤海锦州南变质岩潜山油藏储集层特征与发育控制因素[J].石油勘探与开发,2002,29(4):38-40.
- [12]陈恭洋,何鲜,陶自强,等,千米桥潜山碳酸盐岩古岩溶特征及储层评价[J].天然气地球科学,2003,14(5):375-379.
- [13]吴兴宁,李国军,田继强,等.冀中坳陷碳酸盐岩潜山内幕储层特征及其形成主控因素[J].特种油气藏,2011,18(2):22-25.
- [14]赵贤正,金风鸣,王余泉,等.冀中坳陷长洋淀地区“古储古堵”潜山成藏模式[J].石油学报,2008,29(4):489-493.
- [15]赵明,樊太亮,于炳松,等.塔中地区奥陶系碳酸盐岩储层裂缝发育特征及主控因素[J].现代地质,2009,23(4):709-718.
- [16]董平川,徐衍彬,李飞,等.储层裂缝识别和预测方法[J].大庆石油地质与开发,2010,29(2):5-12.
- [17]刘小平,孙冬胜.古岩溶地貌及其对岩溶储层的控制——以塔里木盆地轮古西地区奥陶系为例[J].石油实验地质,2007,29(3):265-268.
- [18]李丕龙,张善文,王永诗,等.断陷盆地多样性潜山成因——以济阳坳陷为例[J].石油学报,2004,25(3):28-31.
- [19]林会喜.济阳坳陷桩西—埕岛地区下古生界白云岩储集空间形成机理[J].油气与地质采收率,2012,13(3):5-11.
- 渤中凹陷
- 碳酸盐岩
- 潜山气藏
- 储集空间类型
- 成岩作用
- 构造裂缝
Bozhong Sag - carbonate rock
- buried-hill gas reservoir
- accumulation space(AS) type
- diagenesis
- structural fracture