|本期目录/Table of Contents|

[1]武春英,韩会平,康锐,等.鄂尔多斯盆地苏里格南部地区盒8段沉积相特征及其意义[J].地球科学与环境学报,2014,36(04):77-86.
 WU Chun-ying,HAN Hui-ping,KANG Rui,et al.Characteristics and Significance of Sedimentary Facies in He-8Member in the Southern Sulige Area of Ordos Basin[J].Journal of Earth Sciences and Environment,2014,36(04):77-86.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第36卷
期数:
2014年第04期
页码:
77-86
栏目:
基础地质与矿产地质
出版日期:
2014-12-15

文章信息/Info

Title:
Characteristics and Significance of Sedimentary Facies in He-8Member in the Southern Sulige Area of Ordos Basin
文章编号:
1672-6561(2014)04-0077-10
作者:
武春英韩会平康锐尹弘
1. 中国石油长庆油田公司,陕西 西安 710018; 2. 西安科技大学管理学院,陕西 西安 710054
Author(s):
WU Chun-yingHAN Hui-pingKANG RuiYIN Hong
1. Changqing Oilfield Company, PetroChina, Xi’an 710018, Shaanxi, China; 2. School of Management, Xi’an University of Science and Technology, Xi’an 710054, Shaanxi, China
关键词:
沉积相辫状河三角洲滨浅湖分流河道石盒子组上古生界鄂尔多斯盆地
Keywords:
sedimentary facies braided river delta shore-shallow lake distributary channel Shihezi Formation Upper Paleozoic Ordos Basin
分类号:
P531;TE122
DOI:
-
文献标志码:
A
摘要:
依据野外露头、岩芯、测井及相关测试资料,对鄂尔多斯盆地苏里格南部地区上古生界中二叠统石盒子组盒8沉积期的沉积类型、沉积微相特征及沉积相对天然气成藏富集的影响进行了分析。结果表明:鄂尔多斯盆地苏里格南部地区盒8沉积期自北向南依次发育缓坡浅水辫状河三角洲和滨浅湖沉积相,亚相主要为三角洲平原、三角洲前缘、滨湖和浅湖,微相包括分流河道、分流间洼地、水下分流河道、水下天然堤、分流间湾、滨湖砂坝、滨湖泥湾和浅湖泥湾;各微相在空间上相互叠置,复合加积;各微相水动力条件的差异造成微相在沉积物成分和组构上各异,导致其成岩作用不同;分流河道和水下分流河道微相发育处密集形成相互叠置的大面积骨架砂体,构成区内主砂带,成为天然气优质储集层,是有利勘探相带;沉积相明显控制优质储集层的分布,进而影响着天然气的富集成藏。总之,水下分流河道和分流河道微相是砂岩优质储集层分布和发育的最有利相带,也是今后勘探开发的方向。
Abstract:
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参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2014-06-20
基金项目:国家科技重大专项项目(2011ZX05044);中国石油重大科技专项项目(2011E-1301)
作者简介:武春英(1980-),女,山西偏关人,工程师,E-mail:wucy_cq@petrochina.com.cn。
更新日期/Last Update: 2014-12-16