中国矿业
中國礦業
중국광업
CHINA MINING MAGAZINE
2014年
7期
66-69,95
,共5页
侯海海%邵龙义%唐跃%王帅%王学天%刘双
侯海海%邵龍義%唐躍%王帥%王學天%劉雙
후해해%소룡의%당약%왕수%왕학천%류쌍
低煤阶%煤层气%成因类型%成藏模式%动态%优势相带
低煤階%煤層氣%成因類型%成藏模式%動態%優勢相帶
저매계%매층기%성인류형%성장모식%동태%우세상대
low rank%coal-bed methane%genetic types%formation modes%dynamic model%advantage coal facies
基于国内外低煤阶煤层气的富集特点和成藏理论的追踪,对我国低煤阶煤层气的成因类型和成藏模式展开了研究。结果表明,我国低煤阶煤层气藏成因类型有热成因、生物成因和混合成因;煤储层特征包括埋藏浅、含气量低、厚度大、渗透率高且易改造及与其它油气共生等特点;前人从岩性、构造条件及煤储层所处位置、水文地质条件等对低煤阶煤层气的成藏模式进行了划分。基于以上研究,认为应以动态的观点来认识和探讨以有利成煤相带为煤层气富集的物质基础、以构造体为煤层气运移压差和以水动力条件为气源补给和封盖的条件的低煤阶煤层气成藏模式。以东北依兰盆地为例,结合我国低煤阶煤层气盆地的地质特征和前人研究成果,建立了我国低煤阶煤层气的成藏富集模式,即原生成因和次生成因叠合下的斜坡区成煤优势相带高富水区的煤层气富集模式。
基于國內外低煤階煤層氣的富集特點和成藏理論的追蹤,對我國低煤階煤層氣的成因類型和成藏模式展開瞭研究。結果錶明,我國低煤階煤層氣藏成因類型有熱成因、生物成因和混閤成因;煤儲層特徵包括埋藏淺、含氣量低、厚度大、滲透率高且易改造及與其它油氣共生等特點;前人從巖性、構造條件及煤儲層所處位置、水文地質條件等對低煤階煤層氣的成藏模式進行瞭劃分。基于以上研究,認為應以動態的觀點來認識和探討以有利成煤相帶為煤層氣富集的物質基礎、以構造體為煤層氣運移壓差和以水動力條件為氣源補給和封蓋的條件的低煤階煤層氣成藏模式。以東北依蘭盆地為例,結閤我國低煤階煤層氣盆地的地質特徵和前人研究成果,建立瞭我國低煤階煤層氣的成藏富集模式,即原生成因和次生成因疊閤下的斜坡區成煤優勢相帶高富水區的煤層氣富集模式。
기우국내외저매계매층기적부집특점화성장이론적추종,대아국저매계매층기적성인류형화성장모식전개료연구。결과표명,아국저매계매층기장성인류형유열성인、생물성인화혼합성인;매저층특정포괄매장천、함기량저、후도대、삼투솔고차역개조급여기타유기공생등특점;전인종암성、구조조건급매저층소처위치、수문지질조건등대저매계매층기적성장모식진행료화분。기우이상연구,인위응이동태적관점래인식화탐토이유리성매상대위매층기부집적물질기출、이구조체위매층기운이압차화이수동력조건위기원보급화봉개적조건적저매계매층기성장모식。이동북의란분지위례,결합아국저매계매층기분지적지질특정화전인연구성과,건립료아국저매계매층기적성장부집모식,즉원생성인화차생성인첩합하적사파구성매우세상대고부수구적매층기부집모식。
Based on enrichment characteristics and formation theory about low rank coal bed methane (LCBM ) at home and abroad ,national LCBM genetic types and formation models have been studied .The results show that genetic types of LCBM include thermogenic methane ,biogenic methane and mixed methane .The characteristics of low rank coal reservoir include shallow bury ,low contents ,large thickness , high permeability and transformed easily ,coexisting with other oil gas .Based on the previous research results of formation models dividing through lithology ,structure conditions ,locations and hydrogeololgy conditions ,synthesize dynamic formation model has been proposed in this paper ,including material base of favorable sedimental environment ,migration pressure difference of constructs ,methane supply and preserve of hydrogeololgy conditions ,discussing new thought of selecting area of LCBM .Taking Yilan coal-bearing basin for an example ,combined previous research results and geological conditions ,reservoir forming and accumulation model of LCBM in China is proposed ,which is advantage coal faces rich water area accumulation model in slope with coupling between primary and secondary origin .