西南石油大学学报(自然科学版) ›› 2012, Vol. 34 ›› Issue (3): 47-55.

• 地质勘探 • 上一篇    下一篇

阿北区块 A 井区构造特征及油气地质条件

李小刚1,徐国强1,沈忠民1,严永新2,先 伟3   

  1. 1.“油气藏地质及开发工程”国家重点实验室 · 成都理工大学,四川 成都 6100592. 中石化河南油田分公司石油勘探开发研究院,河南 南阳 4731323. 中石化西北油田分公司石油勘探开发研究院,新疆 乌鲁木齐 830011
  • 收稿日期:1900-01-01 修回日期:1900-01-01 出版日期:2012-06-01 发布日期:2012-06-01

Study on Structural Feature and its Oil and Gas Geologic Conditions of AWell Area,North of Awati Sag,Tarim Basin

Li Xiaogang1, Xu Guoqiang1, Shen Zhongmin1, Yan Yongxin2, Xian Wei3   

  1. 1. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu,Sichuan 610059,China2. Exploration and Development Research Institute of Henan Oilfield Company,SINOPEC,Nanyang,Henan 473132,China3. Exploration and Development Research Institute of Northwest Company,SINOPEC,Urumqi,Xinjiang 830011,China
  • Received:1900-01-01 Revised:1900-01-01 Online:2012-06-01 Published:2012-06-01

摘要:
要:环阿瓦提凹陷区(环阿区)的油气勘探一直没有重大突破,近年来随着钻探技术及认识程度的提高,对环阿区
油气勘探前景,尤其是对潜在有利构造带进行重新评估显得十分迫切。基于前人研究成果,利用 A 井区已有钻探及新
旧地震资料,通过开展系统的地层、构造解释与关键层位(第三系底、中上奥陶灰岩顶)构造图编制,揭示该井区中新生
界为一完整的、轴向 NW—SE 的线状挤压背斜,古生界则为一个大型的冲断盐丘穹隆状背斜,古生界盐构造的解释与
前期认识有较大差异。在此基础之上,通过分析其油气地质条件,得出该井区具有构造圈闭规模大、毗邻中上奥陶统
闭塞海湾相烃源岩、裂缝性储层发育、盖层条件好、海西晚期(二叠纪末)形成古构造圈闭、印支—喜山期继承性隆起
且处于油气运移和充注中心等较为有利的油气地质条件。其不利因素为埋藏较深(达 6 400∼7 500 m),且可能受到东
北部大型火山侵入体的影响

关键词: 关键词:阿瓦提凹陷, A 井区, 构造特征, 油气地质条件, 塔里木盆地

Abstract: Abstract:Few large oil and gas fields have been presently discovered around the Awati Sag in western Tarim Basin. However,
in recent years,with both the improvements of drilling technology and level of understanding,it is obviously urgent to carry
out related re-evaluation upon those potential favorable structural traps or zones. In this paper,based on previous studies,
using both pre-existing and newly-obtained 2D seismic data covering the A structure together with drilling data,we firstly
conduct seismic data interpretation and delineate structural maps of key reflector layers(the bottom surface of the Tertiary and
the top surface of the mid-upper Ordovician limestones). The results show that the A structure is an integrated compressional
anticline trending NW-SE within the Mesozoic-Cenozoic interval,but within Palaeozoic interval it is a large-scale thrust-diapir
domal anticline structure,which is quietly different from previous understanding. Further analysis on oil and gas conditions
indicatethatthethrust-diapirdomalstructurepossessessomeessentialelementsforformingpotentialgiantreservoir,including:
1)a large-scale trap with an area of 260 km2and a closure height of 1 100m;2)location beside available source rocks of
the mid-upper Ordovician blocked-trough;3)fractured reservoir of the Upper Cambrian–Middle Ordovician carbonate rocks;
4)lateHercynianpaleostructuraltrapconditiontogetherwithcontinuoushydrocarbonchargingfromCretaceoustothepresent;
5)massive shale sealing condition as well as the fault sealing condition within the shale beds. The adverse factors for this
structure are its depth of burial with target layers up to 6 400∼7 500 m,and may be affected by the neighboring large-scale
volcanic intrusion to its northeast.

Key words: Key words:North Awati Sag, A Well Area, structural feature, hydrocarbon geological condition, Tarim Basin