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作 者:郑莲慧[1] 高倩[2] 曹超[3] 尹帅[1] 王倩倩[1] 刘嫣[1]
机构地区:[1]成都理工大学能源学院,四川成都610059 [2]辽河油田特种油开发公司,辽宁盘锦124010 [3]中联煤层气有限责任公司,山西长治046000
出 处:《四川文理学院学报》2013年第5期54-56,共3页Sichuan University of Arts and Science Journal
摘 要:煤层显微组分与微裂隙二元关系研究对煤层气开采具有潜在价值.通过对沁东北太原组15号煤宏观、电镜、物性等方面资料进行综合分析,对煤储层显微组分和微裂隙之间二元机理进行阐述,结果表明,基质有机显微组分可以产生张性裂隙和压性裂隙,而镜质组中的张性裂隙对煤层气扩散作用较大,惰质组中内生裂隙不太发育.该区渗透率呈现低渗——特低渗的原因主要是割理被脉状方解石填充以及粘土矿物的充填.The microscopic constituent of coal- bed and the micro -fissure's binary relation study has a potential value to the coal- bed methane's mine. Through the comprehensive analysis of microscopy, electron microscopy, physical property~ data of the northeast Qin of Taiyuan Group No. 15 coal and the elaborating of the binary mechanism between the microscopic constituent of coal - bed and micro - fissure which show that matrix organic microscopic constituent can produce tensional fissures and pres- sure fissures, tensional fissures in the vitreous component has bigger effect on the diffusion of coal - bed methane, endogenous fis- sures in the inertinite component are undeveloped. Permeability of the area presented hypotonie - ultra - low permeability, its main reasons are that the cleats are filled up by the vein calcite and clay minerals.
分 类 号:TE122[石油与天然气工程—油气勘探]
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