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龙马溪组岩相类型及其对孔隙特征的影响因素
引用本文:徐传正,冯烁,田继军,蒋立伟. 龙马溪组岩相类型及其对孔隙特征的影响因素[J]. 西南石油大学学报(自然科学版), 2021, 43(1): 51-60. DOI: 10.11885/j.issn.1674-5086.2019.05.04.01
作者姓名:徐传正  冯烁  田继军  蒋立伟
作者单位:1. 新疆大学地质与矿业工程学院, 新疆 乌鲁木齐 830047;2. 新疆维吾尔自治区煤田地质局煤层气研究开发中心, 新疆 乌鲁木齐 830091;3. 中国石油浙江油田公司, 浙江 杭州 310023
基金项目:国家科技重大专项(2017ZX05063002-008)。
摘    要:以川南黔北地区下志留统龙马溪组下段页岩储层为研究对象,以全岩矿物分析为手段,结合岩芯薄片观察,划分出4种页岩岩相,其中,黏土质页岩岩相和混合页岩岩相是本研究区发育的主要岩相.基于扫描电镜、有机碳含量和低温氮气吸附实验,系统地分析了两种主要岩相孔隙结构特征.结果表明,黏土质页岩岩相储层中较大孔隙以细颈瓶状、开放型孔隙和半...

关 键 词:龙马溪组  页岩岩相  矿物含量  有机质  孔隙结构
收稿时间:2019-05-04

Lithofacies Types of Longmaxi Formation and Its Influencing Factors on Pore Characteristics
XU Chuanzheng,FENG Shuo,TIAN Jijun,JIANG Liwei. Lithofacies Types of Longmaxi Formation and Its Influencing Factors on Pore Characteristics[J]. Journal of Southwest Petroleum University(Seience & Technology Edition), 2021, 43(1): 51-60. DOI: 10.11885/j.issn.1674-5086.2019.05.04.01
Authors:XU Chuanzheng  FENG Shuo  TIAN Jijun  JIANG Liwei
Affiliation:1. School of Geology&Mineral Engineering, Xinjiang University, Urumqi, Xinjiang 830047, China;2. CBM Research and Development Center, Xinjiang Bureau of Coalfield Geology, Urumqi, Xinjiang 830091, China;3. China National Petroleum Corporatsion Zhejiang Oilfield Company, Hangzhou, Zhejiang 310023, China
Abstract:The main subjects of study for this paper are from Longmaxi Formation of Lower Silurian in northern Yunnan and Guizhou Province.Based on analysis of whole rock-mineral and observation of core slices,we divide shale lithofacies into 4 types of shale facies,in which the main developed lithofacies in the study area are the clayey shale facies and mixed shale facies.Based on scanning electron microscopy imaging and organic carbon content measurement,and the experiment of nitrogen adsorption at low temperature,we analyzed the pore structure characteristics of different shale facies.The results show that the larger pores in argillaceous shale facies reservoir are mainly flask-shaped pores,open pores and half-closed pores.The larger pore forms in mixed shale facies are mainly open pores with some half-closed pores;the smaller pores in the two facies are mostly half-closed pores.The content of TOC is favorable to the development of micropores and mesopores,while the content of argillaceous minerals is beneficial to the development of macropores.Because the clay mineral content of the clayey shale facies are higher than that of the mixed shale facies,as well as the effect of diagenesis,the macro-pore volume of the clayey shale facies is higher than that of the mixed shale facies,the pore volume of micro-pore and meso-pore is smaller than that of mixed shale facies.
Keywords:Longmaxi Formation  shale lithofacies  mineral contents  organic matter  pore structure
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