新疆地质
新疆地質
신강지질
XINJIANG GEOLOGY
2013年
2期
223-227
,共5页
李永红%吉丛伟%邵龙义%张少林%郭晋宁%李猛%文怀军
李永紅%吉叢偉%邵龍義%張少林%郭晉寧%李猛%文懷軍
리영홍%길총위%소룡의%장소림%곽진저%리맹%문부군
青海%木里煤田%天然气水合物%特征%成藏模式
青海%木裏煤田%天然氣水閤物%特徵%成藏模式
청해%목리매전%천연기수합물%특정%성장모식
Qinghai%Muli coalfield%Gas hydrates%Characteristic%Accumulating model
青海木里煤田发现的天然气水合物,主要产自下部煤层和页岩层,为典型煤成气及页岩气.青藏高原永冻层为天然气水合物形成提供盖层圈闭条件,断层、裂隙、砂体及不整合面为天然气水合物形成提供输导系统,砂体为其形成提供储层.天然气水合物在测井曲线上表现为低密度值、高电阻率、高声速、高天然伽马及井径变大或基本不变,化学组成以CH4、N2为主,含少量O2、C2H6及CO2.在对天然气水合物形成条件及特征研究基础上,提出天然气水合物形成模式:断层为疏导系统,不整合面为疏导系统,渗透性好的砂体为疏导系统.
青海木裏煤田髮現的天然氣水閤物,主要產自下部煤層和頁巖層,為典型煤成氣及頁巖氣.青藏高原永凍層為天然氣水閤物形成提供蓋層圈閉條件,斷層、裂隙、砂體及不整閤麵為天然氣水閤物形成提供輸導繫統,砂體為其形成提供儲層.天然氣水閤物在測井麯線上錶現為低密度值、高電阻率、高聲速、高天然伽馬及井徑變大或基本不變,化學組成以CH4、N2為主,含少量O2、C2H6及CO2.在對天然氣水閤物形成條件及特徵研究基礎上,提齣天然氣水閤物形成模式:斷層為疏導繫統,不整閤麵為疏導繫統,滲透性好的砂體為疏導繫統.
청해목리매전발현적천연기수합물,주요산자하부매층화혈암층,위전형매성기급혈암기.청장고원영동층위천연기수합물형성제공개층권폐조건,단층、렬극、사체급불정합면위천연기수합물형성제공수도계통,사체위기형성제공저층.천연기수합물재측정곡선상표현위저밀도치、고전조솔、고성속、고천연가마급정경변대혹기본불변,화학조성이CH4、N2위주,함소량O2、C2H6급CO2.재대천연기수합물형성조건급특정연구기출상,제출천연기수합물형성모식:단층위소도계통,불정합면위소도계통,삼투성호적사체위소도계통.
The gas hydrates was discovered in the coal and shale of the Jurassic coal measures in the Muli coalfield, and the gas sources were coal and shale. The Permafrost in Tibetan plateau provides cap-rock for gas hydrate. The Fault, fracture, sand body and unconformity supply conducting system for gas, and the sand body also offers as reservoir. The gas hydrates has a low density value, high resistivity, high velocity, high natural gamma and increasing well diameter of logging curve. Chemical compositions are mainly CH4, N2 , with a small amount of O2, C2H6 and CO2. Based on the study of forming condition and characteristics of gas hydrates, we have proposed a model of gas hydrates accumulation;fault plays a role of migration system, disconformity acts as migration system, well-permeable sandstones act as migra-tion and reservoir system.