贵州青岩中三叠统垄头组台地边缘滩相储层特征分析

作    者:淡永,陈洪德,林良彪,隆轲,范昱,邹灏
单    位:成都理工大学野油气藏地质及开发工程冶国家重点实验室;成都理工大学沉积地质研究院
基金项目:全国油气资源战略选区调查与评价项目(XQ-2007-01)部分成果
摘    要:
贵州贵阳青岩地区中三叠统垄头组发育于台地边缘浅滩沉积环境中,主要为 一套藻屑、砾屑灰岩。青岩实测剖面的分析表明,垄头组储层岩石类型主要为生物碎屑灰岩、核形石灰岩、砂砾屑灰岩、藻团块灰岩及泥微晶灰岩。铸体薄片及扫描电镜鉴定分析发现,垄头组储集空间类型主要有微孔、晶间孔、粒内溶孔、铸模孔及构造微裂缝;对野外样品的物性特征研究表明,垄头组仅有4.5%的样品属好储层。认为沉积作用对储层发育具有一定的控制作用,胶结作用、重结晶作用尽管使得垄头组储层整体物性较差,但是溶蚀作用、白云石化作用及构造作用却局部改善了储层。指出了藻屑滩亚相内的裂缝发育带为有利储层发育区。
关键词:贵州;中三叠统;垄头组;碳酸盐岩储集层;储集层特征;成岩作用;控制因素

Reservoir Characteristics of Middle Triassic Longtou Shoal Facies of Platform Margin at Qingyan in Guiyang, Guizhou

Author's Name: Dan Yong, Chen Hongde, Lin Liangbiao, Long Ke, Fan Yu, Zou Hao
Institution: Institute of Sedimentary Geology, Chengdu University of Technology
Abstract:
The measured profile rock of Middle Triassic Longtou Formation that is cropped out at Qingyan in the south part of Guiyang,Guizhou is the shoal sediments of platform margin. The Longtou reservoir mainly consists of bioclastic limestone,oncolitic limestone, algal limestone and micritic limestone. By analysis of cast thin sections and SEM, it is identified that micropores, intercrystalline pores, intragranular dissolved pores, molded pores and structural microfissures. Analysis of reservoir physical property for 44 field samples has shown that only 4.5% of samples can be sorted well with good reservoirs. it is deemed that sedimentation is of a certain control to the reservoir. Cementation, recrystallization made the whole Longtou reservoir poor physical property but the dissolution,dolomitization and tectonism partly improve the reservoir. It is indicated that the fracture zone in algae subfacies is the favorable area of reservoir development with hydrocarbon potential.
Keywords: Middle Triassic; Longtou Formation, Carbonate reservoir; Reservoir characteristics; Diagenesis; Controlling Factor; Guizhou
投稿时间: 2010-01-25  
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