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塔里木盆地奥陶系古潜山碳酸盐岩岩溶储层评价与预测——以轮古7井区以东为例

张庆玉 梁彬 秦凤蕊 曹建文 淡永 李景瑞

中国岩溶2017,Vol.36Issue(1):32-41,10.
中国岩溶2017,Vol.36Issue(1):32-41,10.DOI:10.11932/karst20170104

塔里木盆地奥陶系古潜山碳酸盐岩岩溶储层评价与预测——以轮古7井区以东为例

Evaluation and prediction of carbonate karst reservoirs in the Ordovician buried hills beneath the Tarim basin: An example east of the Lungu7 well block

张庆玉 1梁彬 2秦凤蕊 2曹建文 2淡永 1李景瑞2

作者信息

  • 1. 中国地质大学(武汉)环境学院,武汉430074
  • 2. 中国地质科学院岩溶地质研究所/国土资源部、广西岩溶动力学重点实验室,广西桂林541004
  • 折叠

摘要

Abstract

The Ordovician carbonate karst reservoirs are characterized by deep burial and strong heterogeneity in Tarim basin.The karst reservoir space is primarily the later dissolution pores,karst caves and solution fissures.The study on paleogeomorphology restoration and karst vertical zonation,combined with the reservoir production performance permits to evaluate and predict the Ordovician carbonate karst reservoirs east of the Lungu7 well block.The research suggests that high-production and high-efficiency wells are mainly located in karst graves,karst crests,and karst slopes of peak-hill depressions,hill-peak depressions and karst peak cluster valleys.In the vertical direction,surface karst belts and the upper part of vertical infiltration belts are localities with good exploitation effects,where developed crack-hole reservoirs and karst cave reservoirs.In the runoff karst belts and undercurrent karst belts developed weak karst,where small-scale karst caves and karst pipelines are present,and the karst reservoirs are of the fractured-or hole-type.At last,the research predicts five high-efficient oil and gas reservoir areas,which provide the evidence for planning exploration and development of oil and gas in this area.

关键词

储层评价/碳酸盐岩/岩溶古潜山/塔里木盆地

Key words

reservoir evaluation/reservoir prediction/carbonate/buried hill/Tarim basin

分类

天文与地球科学

引用本文复制引用

张庆玉,梁彬,秦凤蕊,曹建文,淡永,李景瑞..塔里木盆地奥陶系古潜山碳酸盐岩岩溶储层评价与预测——以轮古7井区以东为例[J].中国岩溶,2017,36(1):32-41,10.

基金项目

国家自然基金青年基金项目(41302122) (41302122)

国家重点基础研究发展计划(973计划)项目(2011CB201001) (973计划)

国土资源部公益性行业科研专项(201211082)共同资助 (201211082)

中国地质调查局地调项目(DD20160300) (DD20160300)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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