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准噶尔盆地庄1井区下侏罗统三工河组二段砂体成因
引用本文:李德江,朱筱敏,张小静,孔祥林,黄文松.准噶尔盆地庄1井区下侏罗统三工河组二段砂体成因[J].石油勘探与开发,2006,33(3):326-329.
作者姓名:李德江  朱筱敏  张小静  孔祥林  黄文松
作者单位:1. 中国石油大学(北京)
2. 中国石化胜利油田河口采油厂
3. 中国石油吉林油田地质录井公司
4. 中国石油勘探开发研究院
摘    要:准噶尔盆地庄1井区下侏罗统三工河组二段砂体是重要的油气储集体,明确该套砂体的成因,建立该区的沉积相模式,对于该区的进一步勘探有重要指导意义。目前对此套砂体成因的认识不一。通过对庄1井区的岩心、岩相、岩相组合的细致分析,认为J1s2^1(下侏罗统三工河组二段上亚段)主要为曲流河三角洲前缘沉积,而J1s2^2(下侏罗统三工河组二段下亚段)主要为辫状河三角洲前缘沉积,且夹有滑塌浊流沉积。图8参10

关 键 词:准噶尔盆地  下侏罗统三工河组二段  曲流河三角洲前缘  辫状河三角洲前缘  滑塌浊流沉积  沉积相模式
文章编号:1000-0747(2006)03-0326-04
收稿时间:05 15 2005 12:00AM
修稿时间:2005-05-152006-02-21

Origin of Member 2 sandbodies of Lower Jurassic Sangonghe Formation in the area of Well Zhuang 1, Junggar Basin
LI De-jiang,ZHU Xiao-min,ZHANG Xiao-jing,KONG Xiang-lin,HUANG Wen-song.Origin of Member 2 sandbodies of Lower Jurassic Sangonghe Formation in the area of Well Zhuang 1, Junggar Basin[J].Petroleum Exploration and Development,2006,33(3):326-329.
Authors:LI De-jiang  ZHU Xiao-min  ZHANG Xiao-jing  KONG Xiang-lin  HUANG Wen-song
Affiliation:China University of Petroleum, Beijing 102249, China;China University of Petroleum, Beijing 102249, China;Hekou Oil Production Factory, SLOF, Sinopec, Shandong 257000, China;The Geology Logging Company, PetroChina Jilin Oilfield Company, Jilin 138000, China;Research Institute of Petroleum Exploration & Development, PetroChina, Beijing 100083, China
Abstract:Sandbodies of Member 2 of Lower Jurassic Sangonghe Formation are the important reservoirs in the Junggar Basin.At present,there are different understandings to the sandbodies.Understanding the origin of the sandbodies and establishing a sedimentary facies model of the area will shed light on the petroleum exploration and development.The analysis of the core,lithofacies and lithofacies sequence of the wells around Well Zhuang 1 indicates that J_1s_2~1(the Upper Second Member of Sangonghe Formation of the Lower Jurassic) belongs to the deposition of meandering stream deltaic front;J_1s_2~2(the Lower Second Member of Sangonghe Formation of the Lower Jurassic) belongs to the deposition of braided stream deltaic front and is with the slump turbidite facies at the front of it.
Keywords:Junggar Basin  Member 2 of Lower Jurassic Sangonghe Formation  meandering stream deltaic front  braided stream deltaic front  slump turbidite  sedimentary facies model
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