[1]李 玲,德勒恰提,陈春勇,等.北三台凸起东南缘梧桐沟组储集层成岩演化特征[J].新疆石油地质,2015,36(04):409.[doi:10.7657/XJPG20150406]
 LI Ling,Delaqiati,CHEN Chunyong,et al.Diagenetic Evolution of Wutonggou Reservoir in Southeastern Margin of Beisantai Swell, Junggar Basin[J].Xinjiang Petroleum Geology,2015,36(04):409.[doi:10.7657/XJPG20150406]
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北三台凸起东南缘梧桐沟组储集层成岩演化特征()
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《新疆石油地质》[ISSN:1001-3873/CN:65-1107/TE]

卷:
36
期数:
2015年04期
页码:
409
栏目:
出版日期:
2015-08-30

文章信息/Info

Title:
Diagenetic Evolution of Wutonggou Reservoir in Southeastern Margin of Beisantai Swell, Junggar Basin
文章编号:
1001-3873(2015)04-0409-06
作者:
李 玲1德勒恰提1陈春勇2谭 强2冯 伟1
(1.新疆大学 地质与矿业工程学院,乌鲁木齐 830047; 2.中国石油 新疆油田分公司 准东采油厂,新疆 阜康 831500)
Author(s):
LI Ling1 Delaqiati1 CHEN Chunyong2 TAN Qiang2 FENG Wei1
(1. College of Geology and Mining Engineering, Xinjiang University, Urumqi, Xinjiang830047, China;2.Zhundong Production Plant, Xinjiang Oilfield Company, PetroChina, Fukang, Xinjiang831500, China)
关键词:
准噶尔盆地北三台凸起梧桐沟组成岩演化储集层黏土矿物
Keywords:
Junggar basin Beisantai swell Wutonggou formation diagenetic evolution reservoir clay mineral
分类号:
TE112.221
DOI:
10.7657/XJPG20150406
文献标志码:
A
摘要:
二叠系梧桐沟组是准噶尔盆地北三台凸起重要的勘探目的层,已发现典型的岩性-地层油藏。综合铸体薄片、扫描电镜、电子探针及X射线衍射等资料,对梧桐沟组的成岩作用进行了系统研究。二叠系梧桐沟组储集层主要经历了压实、胶结、溶蚀作用,目前正处于早成岩阶段B期和中成岩阶段A期。研究区黏土矿物以自生高岭石和伊蒙混层为主,酸性水介质及有机质在成岩过程中产生大量酸和CO2,为长石碎屑高岭石化创造了有利条件。富含火山碎屑和地温梯度低、蒙皂石伊利石化速度慢是研究区黏土矿物富含伊蒙混层的重要原因。
Abstract:
The Permian Wutonggou formation is an important target zone for petroleum exploration in Beisantai swell of Junggar basin, andtypical litho?stratigraphic reservoir has been found in it. Based on the analyses of core and sedimentary facies, combined with cast thin section, SEM, electron micro?probe and X?ray diffraction data, a systematic study of the diagenesis of the Wutonggou formation is presented in this paper. The Wutonggou reservoir underwent compaction, cementation and dissolution, and is in stage between early diagenetic period B and mid?diagenetic period A. The clay minerals in the study area are dominated by authigenic kaolinite and illite/smectite, and the acidic aqueous media and organic matter produce large amount of acid and CO2 during diagenesis, which create favorable conditions for detrital feldspar kaolinization. The rich volcanic debris and low geothermal gradient as well as low speed of smectite illitization are the major reasons for rich illite/smectite in the clay minerals

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更新日期/Last Update: 2015-09-21