石油实验地质
石油實驗地質
석유실험지질
Petroleum Geology and Experiment
2015年
5期
535-540
,共6页
郭少斌%付娟娟%高丹%李贺洋%黄家国
郭少斌%付娟娟%高丹%李賀洋%黃傢國
곽소빈%부연연%고단%리하양%황가국
海陆交互相%研究现状%页岩气%中国
海陸交互相%研究現狀%頁巖氣%中國
해륙교호상%연구현상%혈암기%중국
marine-continental facies%research status%shale gas%China
国内外对于海陆交互相页岩气的勘探开发与研究工作尚处于起步阶段。海陆交互相富有机质泥页岩在中国主要分布在北方鄂尔多斯盆地、沁水盆地、南华北盆地的石炭—二叠系本溪、太原和山西组地层中,以及南方四川盆地西南部、贵州西部和湘中—湘南坳陷的二叠系龙潭组地层中。该文总结了中国海陆交互相页岩气研究的成果,认为中国海陆交互相泥页岩干酪根类型以Ⅱ-Ⅲ型为主,除南华北盆地南部和东部外,有机质成熟度普遍较高,一般大于1.5%,处于高成熟—过成熟阶段。海陆交互相泥页岩地层岩相变化快,单层厚度薄,常与煤和致密砂岩甚至灰岩互层,单独开发这套薄层煤系页岩气在开发成本和技术上将面临很大的挑战,进行页岩气、致密气、煤层气等多目的层联合开发将是有效的新途径。
國內外對于海陸交互相頁巖氣的勘探開髮與研究工作尚處于起步階段。海陸交互相富有機質泥頁巖在中國主要分佈在北方鄂爾多斯盆地、沁水盆地、南華北盆地的石炭—二疊繫本溪、太原和山西組地層中,以及南方四川盆地西南部、貴州西部和湘中—湘南坳陷的二疊繫龍潭組地層中。該文總結瞭中國海陸交互相頁巖氣研究的成果,認為中國海陸交互相泥頁巖榦酪根類型以Ⅱ-Ⅲ型為主,除南華北盆地南部和東部外,有機質成熟度普遍較高,一般大于1.5%,處于高成熟—過成熟階段。海陸交互相泥頁巖地層巖相變化快,單層厚度薄,常與煤和緻密砂巖甚至灰巖互層,單獨開髮這套薄層煤繫頁巖氣在開髮成本和技術上將麵臨很大的挑戰,進行頁巖氣、緻密氣、煤層氣等多目的層聯閤開髮將是有效的新途徑。
국내외대우해륙교호상혈암기적감탐개발여연구공작상처우기보계단。해륙교호상부유궤질니혈암재중국주요분포재북방악이다사분지、심수분지、남화북분지적석탄—이첩계본계、태원화산서조지층중,이급남방사천분지서남부、귀주서부화상중—상남요함적이첩계룡담조지층중。해문총결료중국해륙교호상혈암기연구적성과,인위중국해륙교호상니혈암간락근류형이Ⅱ-Ⅲ형위주,제남화북분지남부화동부외,유궤질성숙도보편교고,일반대우1.5%,처우고성숙—과성숙계단。해륙교호상니혈암지층암상변화쾌,단층후도박,상여매화치밀사암심지회암호층,단독개발저투박층매계혈암기재개발성본화기술상장면림흔대적도전,진행혈암기、치밀기、매층기등다목적층연합개발장시유효적신도경。
Shale gas has become one of the hot spots of unconventional natural gas exploration. At present, domestic and overseas research for shale gases is carried out mostly on marine formations; however, research for marine?continental shale gases is still at the initial stage. In China, marine?continental shales rich in organic matter are mainly distributed in the Benxi, Taiyuan and Shanxi formations of Carboniferous and Permian age in the Ordos, Qinshui and southern North China basins in the north, and the Longtan Formation of Permian age in the southwestern Sichuan Basin, the western Guizhou province, and the central Hunan and southern Hunan depressions in the south. This paper summarizes present research results for marine?continental shale gases in China, and shows that the kerogen types of marine?continental shales are mainly II and III. Except for the south and east of the southern North China Basin, organic matter maturity is generally high, commonly greater than 1.5%Ro and is in the high mature and over?mature stages. The lithofacies of marine?continental shales change rapidly and the thickness of a single layer is typically thin, often interbedded with coals, tight sandstones, and even limestones. As a result, separately developing shale gases from such thin layers will face a great challenge in development costs and technology. The joint develop?ment of shale gases, tight gases and coal bed gases from multiple target layers will be an effective new strategy.