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首页|期刊导航|古地理学报|鄂尔多斯盆地姬塬地区上三叠统延长组长8油层组有利储集层分布及控制因素

鄂尔多斯盆地姬塬地区上三叠统延长组长8油层组有利储集层分布及控制因素

刘昊伟 王键 刘群明 赵昕

古地理学报2012,Vol.14Issue(3):285-294,10.
古地理学报2012,Vol.14Issue(3):285-294,10.

鄂尔多斯盆地姬塬地区上三叠统延长组长8油层组有利储集层分布及控制因素

Favorable reservoir distribution and its controlling factors of the Chang 8 interval of Upper Triassic Yanchang Formation in Jiyuan area, Ordos Basin

刘昊伟 1王键 1刘群明 1赵昕1

作者信息

  • 1. 中国石油勘探开发研究院,北京100083
  • 折叠

摘要

Abstract

The Chang 8 interval of the Upper Triassic Yanchang Formation is a typical low-porosity and low-permeability reservoir in Jiyuan area of the Ordos Basin. Researches of the main controlling factors, the formation conditions of high quality reservoirs and forecast of the favorable target have great significance for the exploration of potential oil and gas resources. Comprehensive analyses have been made on the sedimentary characteristics, property characteristics, rock thin sections, casting thin sections and so on. This paper discusses the distribution of favorable reservoir, the petrology characteristics, the pore texture and pore types, the physical property and the diagenesis types, which finally makes a comprehensive prediction of the distribution characteristics of favorable reservoir area. The results reflect that the lithic arkose is developed well and the cement, especially the ferrocalcite, is general in the Chang 8 interval of the study area. It is poor of the physical properties of the whole reservoir which is characterized by strong heterogeneity. The pore types mainly include residual intergranular pore and dissolution pore. The reservoir is controlled by the sedimentation, diagenisis and tectonism. Based on the above analyses, we forecasted the favorable reservoir in the Jiyuan area.

关键词

鄂尔多斯盆地/姬塬地区/延长组/有利储集层

Key words

Ordos Basin/ Jiyuan area/ Yanchang Formation/ favorable reservoir

分类

能源科技

引用本文复制引用

刘昊伟,王键,刘群明,赵昕..鄂尔多斯盆地姬塬地区上三叠统延长组长8油层组有利储集层分布及控制因素[J].古地理学报,2012,14(3):285-294,10.

基金项目

国家科技重大专项(编号:2008ZX05004)资助 (编号:2008ZX05004)

古地理学报

OA北大核心CSCDCSTPCD

1671-1505

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