天然气工业
天然氣工業
천연기공업
NATURAL GASINDUSTRY
2009年
12期
115-118
,共4页
中国%页岩气%泥页岩%富集区%海相%海陆交互相%陆相煤系%湖相
中國%頁巖氣%泥頁巖%富集區%海相%海陸交互相%陸相煤繫%湖相
중국%혈암기%니혈암%부집구%해상%해륙교호상%륙상매계%호상
China%shale gas%mud shale%play%marine facies%transitional facies%continental coal measure strata%lacustrine facies
我国页岩气勘探才刚刚起步,目前研究主要集中在页岩气成藏条件和有利区评价方面.页岩气有利区优选还处于富含有机质泥页岩优选阶段,优选出的主要是页岩气发育远景区.受复杂地质背景和多阶段演化过程的影响,我国含油气盆地类型多、盆地结构复杂,盆地的不同演化规律直接控制着富含有机质泥页岩的发育与分布.为此,依据形成环境将富含有机质泥页岩划分为海相厚层富含有机质泥页岩、海陆交互相及陆相煤系地层富含有机质泥页岩、湖相富含有机质泥页岩这3种类型,并分别探讨了其页岩气勘探开发前景.结论认为:①海相厚层富含有机质页岩是我国近期页岩气勘探的首选;②海陆交互相及陆相煤系地层富含有机质泥页岩单层厚度较薄,但与致密砂岩气和煤层气有共生条件,发展页岩气与致密砂岩气等多类型天然气资源多层合采技术具有十分现实的意义;③湖相富含有机质泥页岩成岩程度普遍不高,需要进一步优选岩石强度较大、具备裸眼完井条件的层位进行勘探开发.
我國頁巖氣勘探纔剛剛起步,目前研究主要集中在頁巖氣成藏條件和有利區評價方麵.頁巖氣有利區優選還處于富含有機質泥頁巖優選階段,優選齣的主要是頁巖氣髮育遠景區.受複雜地質揹景和多階段縯化過程的影響,我國含油氣盆地類型多、盆地結構複雜,盆地的不同縯化規律直接控製著富含有機質泥頁巖的髮育與分佈.為此,依據形成環境將富含有機質泥頁巖劃分為海相厚層富含有機質泥頁巖、海陸交互相及陸相煤繫地層富含有機質泥頁巖、湖相富含有機質泥頁巖這3種類型,併分彆探討瞭其頁巖氣勘探開髮前景.結論認為:①海相厚層富含有機質頁巖是我國近期頁巖氣勘探的首選;②海陸交互相及陸相煤繫地層富含有機質泥頁巖單層厚度較薄,但與緻密砂巖氣和煤層氣有共生條件,髮展頁巖氣與緻密砂巖氣等多類型天然氣資源多層閤採技術具有十分現實的意義;③湖相富含有機質泥頁巖成巖程度普遍不高,需要進一步優選巖石彊度較大、具備裸眼完井條件的層位進行勘探開髮.
아국혈암기감탐재강강기보,목전연구주요집중재혈암기성장조건화유리구평개방면.혈암기유리구우선환처우부함유궤질니혈암우선계단,우선출적주요시혈암기발육원경구.수복잡지질배경화다계단연화과정적영향,아국함유기분지류형다、분지결구복잡,분지적불동연화규률직접공제착부함유궤질니혈암적발육여분포.위차,의거형성배경장부함유궤질니혈암화분위해상후층부함유궤질니혈암、해륙교호상급륙상매계지층부함유궤질니혈암、호상부함유궤질니혈암저3충류형,병분별탐토료기혈암기감탐개발전경.결론인위:①해상후층부함유궤질혈암시아국근기혈암기감탐적수선;②해륙교호상급륙상매계지층부함유궤질니혈암단층후도교박,단여치밀사암기화매층기유공생조건,발전혈암기여치밀사암기등다류형천연기자원다층합채기술구유십분현실적의의;③호상부함유궤질니혈암성암정도보편불고,수요진일보우선암석강도교대、구비라안완정조건적층위진행감탐개발.
Shale gas, as a new type of unconventional natural gas resources, its exploration and development have got great success in the U.S.A., and fast progress in Canada, Australia and other countries. Shale gas exploration in China has just started and its study is still focused on shale gas reservoir conditions and favorable area evaluation. China's preferred shale gas favorable area is mainly related with organic-rich clay and shale, and the major optimization is a prospective area for shale gas. Complicated geological background and multi-stage evolution lead to many types of China's petroleum basins whose structures are complex. Different evolution history of each basin directly controls the development and distribution of organic-rich shale. By the different formation environment, organic-rich shale can be divided into marine thick layer organic-rich shale, continent-sea intercrossing organic-rich shale, coal-bearing strata organic-rich shale, and lacustrine organic-rich shale. Among them, the thick layer marine organic-rich shale is of first priority in China's near future shale gas exploration; continent-sea intercrossing organic-rich shale and coal-bearing strata organic-rich shale are thin in single-layer, but they have symbiotic conditions with tight sandstone gas and coal-bed gas, so the multi-layer co-mining technology of shale gas, tight sandstone gas and many other types of natural gas resources has great practical significance; the lacustrine organic-rich shale's diagenesis degree is generally low, and needs further optimization of a horizon with high-strength rock and the conditions of open hole completion for exploration and development.