油气勘探

细粒相沉积地质特征与致密油勘探——以渤海湾盆地沧东凹陷孔店组二段为例

展开
  • 1. 中国石油大港油田公司;
    2. 中国石油大学(华东)
蒲秀刚(1968-),男,四川阆中人,博士,中国石油大港油田公司高级工程师,主要从事沉积学、储集层地质学综合研究和油气勘探方面的工作。地址:天津市滨海新区大港油田幸福路1278号,大港油田公司勘探开发研究院实验中心S709,邮政编码:300280。E-mail: puxgang@petrochina.com.cn

网络出版日期: 2017-01-01

基金资助

中国石油科技重大专项“大港油区大油气田勘探开发关键技术研究”(2014E-06)

Geologic features of fine-grained facies sedimentation and tight oil exploration: A case from the second Member of Paleogene Kongdian Formation of Cangdong sag, Bohai Bay Basin

Expand
  • 1. PetroChina Dagang Oilfield Company, Tianjin 300280, China;
    2. China University of Petroleum (East China), Qingdao 266580, China

Online published: 2017-01-01

摘要

以渤海湾盆地沧东凹陷古近系孔店组二段湖盆中部细粒相区600多米连续整体取心、上万块次系统分析联测及配套测录井资料为基础,运用传统石油地质学、沉积岩石学及致密油气形成新理论新方法,对孔二段细粒相区沉积特征进行了研究。结果表明,沧东凹陷孔二段是孔店组最大湖泛期的沉积,半深湖—深湖亚相细粒沉积分布较广,主要发育细粒长英沉积岩类、细粒混合沉积岩类及白云岩类,而黏土岩类不发育,细粒岩类具有“岩石成分多,优势矿物少;碎屑矿物多,黏土矿物少;方沸石多,黄铁矿少;脆性矿物多,石英含量少;岩石类型多,油页岩少;致密储集层多,无裂缝的少;优质烃源岩多,非烃源岩少;高频旋回多,单一沉积少”等特点。这些认识更新了以往关于陆相闭塞湖盆中部仅以“泥页岩”烃源岩沉积为主的观点。在地质认识指导及配套工程工艺技术的支撑下多口探井获工业油流,展示了陆相湖盆细粒相区致密油勘探的良好前景。图9参19

本文引用格式

蒲秀刚, 周立宏, 韩文中, 周建生, 王文革, 张伟, 陈世悦, 时战楠, 柳飒 . 细粒相沉积地质特征与致密油勘探——以渤海湾盆地沧东凹陷孔店组二段为例[J]. 石油勘探与开发, 2016 , 43(1) : 24 -33 . DOI: 10.11698/PED.2016.01.03

Abstract

Based on analysis of successive and whole cores over six hundred meters from the second Member of Kongdian Formation (Kong 2 Member) of fine-grained facies zone in central lake basin of Cangdong sag, ten thousands of systematic and joint analysis data, and the matching logging data, the sedimentary characteristics in the fine-grained facies zone is examined by means of traditional petroleum geology, sedimentology, and new theory and method of tight oil and gas generation. The Kong 2 Member is the sedimentation during the maximum lake flooding in the Kongdian Formation. Fine-grained sedimentation of half-deep lake to deep lake are widely distributed, the fine-grained feldspar-quartz contained sedimentary rock, fine-grained mixed sedimentary rock, and dolomite are developed, and the clay rock is poorly developed. The fine-grained rocks have these features as follows: more rock compositions, less advantageous minerals; more debris minerals, less clay minerals; more analcites, less pyrites; more brittle minerals, less quartz; more rock types, less oil shale; more tight reservoirs with less non-cracked reservoirs; more high-quality source rocks, less non-source rocks; more high-frequency cycle sediments, less single sediments. These understandings updated the former view that only mud shale source rock was dominantly developed in the closed continental lake. With the help of geologic research and matched engineering technologies, several exploration wells have produced industrial oil flows, showing a good prospect of tight oil exploration in fine-grained facies zones of continental lacustrine basins.

参考文献

[1] MACQUAKER J H S, ADAMS A E. Maximizing information from fine-grained sedimentary rocks: An inclusive nomenclature for mudstones[J]. Journal of Sedimentary Research, 2003, 73(3): 735-744.
[2] APLIN C A, MACQUAKER H S I. Mudstone diversity: Origin and implications for source, seal, and reservoir properties in petroleum systems[J]. AAPG Bulletin, 2011, 95(12): 2031-2059.
[3] OTTER E P, MAYNARD J B, DEPETRIS J P. Mud and mudstones: Introduction and overview[M]. Berlin: Springer, 2005.
[4] 赵政璋, 杜金虎. 致密油气[M]. 北京: 石油工业出版社, 2012.
ZHAO Zhengzhang, DU Jinhu. Tight oil and gas[M]. Beijing: Petroleum Industry Press, 2012.
[5] 贾承造, 邹才能, 李建忠, 等. 中国致密油评价标准、主要类型、基本特征及资源前景[J]. 石油学报, 2012, 33(3): 343-350.
JIA Chengzao, ZOU Caineng, LI Jianzhong, et al. Assessment criteria, main types, basic features and resource prospects of the tight oil in China[J]. Acta Petrolei Sinica, 2012, 33(3): 343-350.
[6] 袁选俊, 林森虎, 刘群, 等. 湖盆细粒沉积特征与富有机质页岩分布模式: 以鄂尔多斯盆地延长组长7油层组为例[J]. 石油勘探与开发, 2015, 42(1): 1-10.
YUAN Xuanjun, LIN Senhu, LIU Qun, et al. Lacustrine fine-grained sedimentary features and organic-rich shale distribution pattern: A case study of Chang 7 Member of Triassic Yanchang Formation in Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2015, 42(1): 1-10.
[7] 杜金虎, 刘合, 马德胜, 等. 试论中国陆相致密油有效开发技术[J]. 石油勘探与开发, 2014, 41(2): 198-205.
DU Jinhu, LIU He, MA Desheng, et al. Discussion on effective development techniques for continental tight oil in China[J]. Petroleum Exploration and Development, 2014, 41(2): 198-205.
[8] 贾承造, 郑民, 张永峰. 中国非常规油气资源与勘探开发前景[J]. 石油勘探与开发, 2012, 39(2): 129-136.
JIA Chengzao, ZHENG Min, ZHANG Yongfeng. Unconventional hydrocarbon resources in China and the prospect of exploration and development[J]. Petroleum Exploration and Development, 2012, 39(2): 129-136.
[9] 李三中, 索艳慧, 周立宏, 等. 华北克拉通内部的拉分盆地: 渤海湾盆地黄骅坳陷结构构造与演化[J]. 吉林大学学报(地球科学版), 2011, 41(5): 1362-1379.
LI Sanzhong, SUO Yanhui, ZHOU Lihong, et al. Pull-apart basins within the north China craton: Structural pattern and evolution of Huanghua Depression in Bohai Bay Basin[J]. Journal of Jilin University(Earth Science Edition), 2011, 41(5): 1362-1379.
[10] 任建业, 廖前进, 卢刚臣, 等. 黄骅坳陷构造变形格局与演化过程分析[J]. 大地构造与成矿学, 2010, 34(4): 461-472.
REN Jianye, LIAO Qianjin, LU Gangchen, et al. Deformation framework and evolution of Huanghua Depression, Bohai Gulf[J]. Geotectonica et Metallogenia, 2010, 34(4): 461-472.
[11] 李明刚, 杨桥, 张健. 黄骅拗陷新生代构造样式及其演化[J]. 西南石油大学学报(自然科学版), 2011, 33(1): 71-78.
LI Minggang, YANG Qiao, ZHANG Jian. The Cenozoic structural style and its evolution in Huanghua Depression[J]. Journal of Southwest Petroleum University(Science & Technology Edition), 2011, 33(1): 71-78.
[12] 鄢继华, 蒲秀刚, 周立宏, 等. 基于X射线衍射数据的细粒沉积岩岩石定名方法与应用[J]. 中国石油勘探, 2015, 20(1): 48-54.
YAN Jihua, PU Xiugang, ZHOU Lihong, et al. The naming methods of fine-grained sedimentary rocks based on the data of X-ray diffraction[J]. China Petroleum Exploration, 2015, 20(1): 48-54.
[13] 刘招君, 杨虎林, 董清水, 等. 中国油页岩[M]. 北京: 石油工业出版社, 2009.
LIU Zhaojun, YANG Hulin, DONG Qingshui, et al. Oil shale in China[M]. Beijing: Petroleum Industry Press, 2009.
[14] 于兴河. 碎屑岩系油气储层沉积学[M]. 北京: 石油工业出版社, 2008.
YU Xinghe. Clastic rock series of oil and gas reservoir sedimentology[M]. Beijing: Petroleum Industry Press, 2008.
[15] 姜在兴. 沉积学[M]. 北京: 石油工业出版社, 2003.
JIANG Zaixing. Sedimentology[M]. Beijing: Petroleum Industry Press, 2003.
[16] 邹才能, 赵政璋, 杨华, 等. 陆相湖盆深水砂质碎屑流成因机制与分布特征: 以鄂尔多斯盆地为例[J]. 沉积学报, 2009, 27(6): 1065-1075.
ZOU Caineng, ZHAO Zhengzhang, YANG Hua, et al. Genetic mechanism and distribution of sandy debris flows in terrestrial lacustrine basin[J]. Acta Sedimentologica Sinica, 2009, 27(6): 1065-1075.
[17] 蒲秀刚, 周立宏, 韩文中, 等. 歧口凹陷沙一下亚段斜坡区重力流沉积与致密油勘探[J]. 石油勘探与开发, 2014, 41(2): 138-150.
PU Xiugang, ZHOU Lihong, HAN Wenzhong, et al. Gravity flow sedimentation and tight oil exploration in lower first member of Shahejie Formation in slope area of Qikou Sag, Bohai Bay Basin[J]. Petroleum Exploration and Development, 2014, 41(2): 138-150.
[18] SHANMUGAM G. 深水砂体成因研究新进展[J]. 石油勘探与开发, 2013, 40(3): 294-301.
SHANMUGAM G. New perspectives on deep-water sandstones: Implications[J]. Petroleum Exploration and Development, 2013, 40(3): 294-301.
[19] 王冠民. 古气候变化对湖相高频旋回泥岩和页岩的沉积控制: 以济阳坳陷古近系为例[D]. 广州: 中国科学院广州地球化学研究所, 2005.
WANG Guanmin. The sedimentary control to mudstone and shale in lacustrine high-frequency cycle by paleoclimate change: Taking the Ecogene in Jiyang Depression as an example[D]. Guangzhou: Guangzhou Institute of Geochemistry of Chinese Academy of Sciences, 2005.
文章导航

/