中国煤炭地质
中國煤炭地質
중국매탄지질
Coal Geology of China
2015年
11期
14-17
,共4页
煤储层%含气潜力%比德区块%比德-三塘盆地
煤儲層%含氣潛力%比德區塊%比德-三塘盆地
매저층%함기잠력%비덕구괴%비덕-삼당분지
coal reservoir%gas-bearing potential%Bide block%Bide-Santang Basin
基于比德-三塘盆地比德区块煤炭地质勘查及煤层气井取得的地质成果,对煤储层特征及有利区进行了研究。分析认为:该区块煤层厚度总体呈西北薄、东南厚的特点,且主力煤层厚度较大,平均为7.0m;煤的宏观煤岩类型多为半暗煤,其次为半亮煤,显微组分以镜质组为主,平均为67.11%;煤储层孔喉均一性较好,渗透率较高,有利于煤层气的渗流;主力煤层VL平均为26.4 cm3/t,煤岩的吸附能力较强,煤层含气潜力较大。综合分析并根据煤层厚度和埋深初步圈定了煤层气有利勘探区。
基于比德-三塘盆地比德區塊煤炭地質勘查及煤層氣井取得的地質成果,對煤儲層特徵及有利區進行瞭研究。分析認為:該區塊煤層厚度總體呈西北薄、東南厚的特點,且主力煤層厚度較大,平均為7.0m;煤的宏觀煤巖類型多為半暗煤,其次為半亮煤,顯微組分以鏡質組為主,平均為67.11%;煤儲層孔喉均一性較好,滲透率較高,有利于煤層氣的滲流;主力煤層VL平均為26.4 cm3/t,煤巖的吸附能力較彊,煤層含氣潛力較大。綜閤分析併根據煤層厚度和埋深初步圈定瞭煤層氣有利勘探區。
기우비덕-삼당분지비덕구괴매탄지질감사급매층기정취득적지질성과,대매저층특정급유리구진행료연구。분석인위:해구괴매층후도총체정서북박、동남후적특점,차주력매층후도교대,평균위7.0m;매적굉관매암류형다위반암매,기차위반량매,현미조분이경질조위주,평균위67.11%;매저층공후균일성교호,삼투솔교고,유리우매층기적삼류;주력매층VL평균위26.4 cm3/t,매암적흡부능력교강,매층함기잠력교대。종합분석병근거매층후도화매심초보권정료매층기유리감탐구。
Based on coal geological exploration and CBM well acquired geological results in the Bide-Santang Basin, carried out stud?ies on coal reservoir features and favorable exploration area. The analysis considered that the coal thickness in the Bide block presents peculiarity of thin in northwest and thick in southeast, besides, the principal coal seam is rather thick, average 7.0m. The macroli?thotype of coal is mostly semidull coal, then semibright coal;maceral is mainly vitrinite, average 67.11%. Homogeneity of pore throat in coal reservoir is preferable with higher permeability, propitious to CBM seepage. Average VL of principal coal is 26.4 cm3/t;adsorptivity of coal and rock is rather strong, thus larger coal seam gas-bearing potential. On the bases of comprehensive analysis and coal thick?ness, buried depth, preliminarily delineated CBM favorable exploration areas.