天然气地球科学 ›› 2012, Vol. 23 ›› Issue (2): 279–283.doi: 10.11764/j.issn.1672-1926.2012.02.279

• 天然气地质学 • 上一篇    下一篇

东营南坡新生界与中古生界不整合面特征及对油气成藏的影响

王东旭   

  1. 胜利油田分公司地质科学研究院,山东 东营 257015
  • 收稿日期:2011-11-14 修回日期:2011-12-27 出版日期:2012-04-10 发布日期:2012-04-10
  • 通讯作者: 王东旭wangdongxu.slyt@sinopec.com. E-mail:wangdongxu.slyt@sinopec.com.
  • 作者简介:王东旭(1979-),男,辽宁营口人,工程师,主要从事石油地质综合研究.E-mail:wangdongxu.slyt@sinopec.com.
  • 基金资助:

    国家重大科技专项“渤海湾盆地东营凹陷勘探成熟区精细评价示范工程”(编号:2008ZX05051)资助.

Features of Unconformity between Cenozoic and Mesozoic-Paleozoic and Its Effect on Hydrocarbon Accumulation in South of Dongying Sag

Wang Dong-xu   

  1. Geological Scientific Research Institute,Shengli Oilfield Company,SINOPEC,Dongying 257015,China
  • Received:2011-11-14 Revised:2011-12-27 Online:2012-04-10 Published:2012-04-10

摘要:

受多期构造运动影响,东营凹陷形成多期不整合面。其中新生界与中古生界不整合广泛分布于凹陷之中,其上覆地层与下伏地层的接触关系多为削超样式。不整合结构层中的风化粘土层,经过成岩压实作用,极易固结,形成非渗透层,具有很好的封堵效应。由于风化淋滤作用,不整合面下的风化砂砾岩、碳酸盐岩等的渗透性均得到不同程度的改善,成为输导油气甚至储集油气的有利场所。油气在不整合中运移主要通过2种方式:不整合结构层侧向输导和不整合“天窗”式垂向输导。受不整合削超或平超式、砂/泥型或泥/砂型等多种岩性组合的控制,东营凹陷南斜坡多发育地层超覆、不整合削截油藏。

关键词: 东营凹陷, 不整合, 新生界, 中古生界, 油气成藏

Abstract:

Under multiphase tectonic activity,many unconformities were formed in the Dongying sag.Among them,the unconformities between Tertiary and pre-Tertiary exist widely.The main contact between overlying and underlying formations is truncation-overlap.The weathered layer in the unconformity structure went through the diagenetic compression,and is easily solidified to form the impermeability layer with good sealing.Under the weathering and leaching action,the permeability of glutenite and carbonate under the unconformity is improved,and becomes a favorable area of oil and gas migration or accumulation.Two pathways of oil and gas migration in the unconformity are lateral and vertical.Since the multi-contact styles constrain the petroleum accumulation,such as truncation-overlap or parallelism-overlap and sand/mud or mud/sand,stratigraphic overlap and unconformity truncation,the stratigraphic overlap and unconformity truncation oil reservoirs occur generally in the south slope of Dongying sag.

Key words: Dongying sag, Unconformity, Cenozoic, Mesozoic-Paleozoic, Hydrocarbon accumulation.

中图分类号: 

  • TE122

[1]Qiu Yigang,Cheng Rihui,Lin Changsong.Unconformity types of the lower Tertiary and their geological significance in Zhanhua trough[J].Journal of Jilin University:Earth Science Edition,2002,32(2):146-150.[邱以钢,程日辉,林畅松.沾化凹陷下第三系不整合类型及其地质意义[J].吉林大学学报:地球科学版,2002,32(2):146-150.]
[2]Wu Zhiping,Shi Buqing,Zhou Yaoqi,et al.A study on hiatus surface of Neogene Eogene in Jiyang depression[J].Oil and Gas Geology,1998,19(4):313-317.[吴智平,史卜庆,周瑶琪,等.济阳坳陷新老第三纪地层间断面研究[J].石油与天然气地质,1998,19(4):313-317.]
[3]He Dengfa.Structure of unconformity and its control on hydrocarbon accumulation[J].Petroleum Exploration and Development,2007,34(2):142-149.[何登发.不整合面的结构与油气聚集[J].石油勘探与开发,2007,34(2):142-149.]
[4]Sui Fenggui,Zhao Leqiang.The unconformity configuration type and its reservoir forming control in  Jiyang depression[J].Geotectonica et Metallogenia,2006,30(2):161-167.[隋风贵,赵乐强.济阳坳陷不整合结构类型及控藏作用[J].大地构造与成矿学,2006,30(2):161-167.]
[5]Jin Bo,Liu Zhen,Li Xushen.The study on transfers system of natural gas of Yingdong slope[J].Natural Gas Geoscience,2004,15(5):498-502.[金博,刘震,李绪深.莺东斜坡带上第三系天然气输导系统研究[J].天然气地球科学,2004,15(5):498-502.]
[JP]
[6]Yang Ning,Lv Xiuxiang,Chen Meitao,et al.Accumulation models of paleoweathering crust reservoir in carbonate Yingmaili area[J].Natural Gas Geoscience,2005,16(1):35-39.[杨宁,吕修祥,陈梅涛,等.英买力地区碳酸盐岩古风化壳油气聚集模式探讨[J].天然气地球科学,2005,16(1):35-39.]
[7]Cheng Yongsheng,Chen Songling.Hydrocarbon accumulation of Paleozoic strata in peripheral areas of Nanpu sag[J].Natural Gas Geoscience,2009,20(1):108-112.[成永生,陈松岭.南堡凹陷外围地区古生界地层油气成藏分析[J].天然气地球科学,2009,20(1):108-112.]
[8]Yin Wei,Chen Zhaonian,Xu Hao,et al.Unconformity type and its significance in petroleum geology[J].Xinjiang Petroleum Geology,2006,27(2):239-241.[尹微,陈昭年,许浩,等.不整合类型及其油气地质意义[J].新疆石油地质,2006,27(2):239-241.]
[9]Fu Guang,Xu Zejian,Han Dongling,et al.Role of surface of unconformity in formation of oil or gas reservoirs[J].Journal of Daqing Petroleum Geology,2001,25(1): 1-4.[付广,许泽剑,韩冬玲,等.不整合面在油气藏形成中的作用[J].大庆石油学院学报,2001,25(1):1-4.]
[10]Fu Guang,Duan Haifeng,Meng Qingfen.Unconformity and transport hydrocarbon characteristic[J].Petroleum Geology and Oilfield Development in Daqing,2005,24(1):13-16.[付广,段海凤,孟庆芬.不整合及输导油气特征[J].大庆石油地质与开发,2005,24(1):13-16.]
[11]Wang Yanzhong,Cao Yingchang,Wang Shuping,et al.Advances in research of spatial strucrures of unconformity[J].Geotectonica et Metallogenia,2006,30(3):326-330.[王艳忠,操应长,王淑萍,等.不整合空间结构与油气成藏综述[J].大地构造与成矿学,2006,30(3):326-330.]
[12]Chen Tao,Jiang Youlu,Song Guoqi,et al.Geological features and hydrocarbon reservoir of unconformity structures in Jiyang depression[J].Acta Petrolei Sinica,2008,29(4):499-503.[陈涛,蒋有录,宋国奇,等.济阳坳陷不整合结构地质特征及油气成藏条件[J].石油学报,2008,29(4):499-503.]
[13]Pan Zhongxiang.Significance of unconformity to oil and gas migration and accumulation[J].Acta Petrolei Sinica,1983,4(4):1-10.[潘钟祥.不整合对于油气运移聚集的重要性[J].石油学报,1983,4(4):1-10.]
[14]Hu Jianyi,Xu Shubao,Liu Shuxuan,et al.Unstructure Reservior[M].Beijing:Peroleum Industry Press,1986.[胡见义,徐树宝,刘淑萱,等.非构造油气藏[M].北京:石油工业出版社,1986.]
[15]Zhang Houfu,Fang Chaoliang,Gao Xianzhi,et al.Petroleum Geology[M].Beijing:Peroleum Industry Press,1999.[张厚福,方朝亮,高先志,等.石油地质学[M].北京:石油工业出版社,1999.]

[1] 吴靖,姜在兴,王欣. 湖相细粒沉积岩三—四级层序地层划分方法与特征——以渤海湾盆地东营凹陷古近系沙四上亚段为例[J]. 天然气地球科学, 2018, 29(2): 199-210.
[2] 肖敦清, 姜文亚, 蒲秀刚, 王娜, 岳云福, 孙超囡, 代昆, 滑双君. 渤海湾盆地歧口凹陷中深层天然气成藏条件与资源潜力[J]. 天然气地球科学, 2018, 29(10): 1409-1421.
[3] 张超,张立强,陈家乐,罗红梅,刘书会. 渤海湾盆地东营凹陷古近系细粒沉积岩岩相类型及判别[J]. 天然气地球科学, 2017, 28(5): 713-723.
[4] 韩宝,王昌伟,盛世锋,庞燕青. 准噶尔盆地中拐—五区二叠系不整合面对油气成藏控制作用[J]. 天然气地球科学, 2017, 28(12): 1821-1828.
[5] 王琳,赵孟军,孟庆洋,王鹏,王科,袁海莉,申磊军,雷刚. 柴达木盆地英西地区中深层油气成藏过程分析[J]. 天然气地球科学, 2017, 28(12): 1846-1854.
[6] 焦伟伟,汪生秀,程礼军,罗情勇,方光建. 渝东南地区下寒武统页岩气高氮低烃成因[J]. 天然气地球科学, 2017, 28(12): 1882-1890.
[7] 王龙,谢晓军,刘世翔,宋双,王一博,唐武,郭佳,孙瑞. 南海南部主要盆地油气分布规律及主控因素[J]. 天然气地球科学, 2017, 28(10): 1546-1554.
[8] 高长海,查明,陈力,赵贤正,金凤鸣. 渤海湾盆地冀中坳陷大柳泉构造不整合输导油气能力的定量表征[J]. 天然气地球科学, 2016, 27(4): 619-627.
[9] 史基安,郭晖,吴剑锋,姚爱国,邹妞妞,吴志雄. 准噶尔盆地滴西地区石炭系火山岩油气成藏主控因素[J]. 天然气地球科学, 2015, 26(S2): 1-11.
[10] 刘炜博,鞠治学,韩剑发,祁燕飞,汤明刚. 塔里木盆地塔中Ⅲ区奥陶系碳酸盐岩各层系油气成藏特征及富集规律[J]. 天然气地球科学, 2015, 26(S2): 125-137.
[11] 张存,胡有福,陈军,于金星,齐凤林,蒋其君. WEFOX叠前成像技术及其在塔里木盆地塔中地区岩溶缝洞储层中的应用[J]. 天然气地球科学, 2015, 26(S2): 158-164.
[12] 王宏斌,张虎权,杨丽莎,郑多明,姚清洲,代冬冬. 塔里木盆地哈拉哈塘地区潜山岩溶带油气成藏关键因素[J]. 天然气地球科学, 2015, 26(S1): 72-79.
[13] 刘军,崔海峰,陈永权,田雷,张年春. 膏岩层在油气成藏中的作用及勘探意义——以塔西南麦盖提斜坡区奥陶系为例[J]. 天然气地球科学, 2015, 26(S1): 139-147.
[14] 房倩,徐怀民,尹楠鑫,江同文,周新平,昌伦杰,胡泽云,张建良. 塔中地区东河砂岩段层序界面再认识及不整合对油气成藏的作用[J]. 天然气地球科学, 2015, 26(6): 1035-1046.
[15] 吴斌,何登发,孙方源. 塔里木盆地古城低凸起下古生界的断裂特征及成因机制[J]. 天然气地球科学, 2015, 26(5): 871-879.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!