石油实验地质
石油實驗地質
석유실험지질
EXPERIMENTAL PETROLEUM GEOLOGY
2014年
2期
176-181
,共6页
张永东%邵志兵%乔桂林%韩彧
張永東%邵誌兵%喬桂林%韓彧
장영동%소지병%교계림%한욱
成岩作用%储集特征%东河塘组%巴麦地区%塔里木盆地
成巖作用%儲集特徵%東河塘組%巴麥地區%塔裏木盆地
성암작용%저집특정%동하당조%파맥지구%탑리목분지
diagenesis%reservoir property%Donghetang Formation%Bachu-Maigaiti area%Tarim Basin
通过普通薄片、铸体薄片、扫描电镜以及测井等分析手段,对巴麦地区东河塘组上砂岩段和下砂岩段的沉积特征、岩石学特征、成岩作用进行了详细分析。东河塘组沉积环境为滨岸相,具有较高的成分成熟度和结构成熟度,且上砂岩段的成分成熟度和结构成熟度都要高于下砂岩段。储集空间类型主要为溶蚀孔隙,其分布主要受粒度和粒间胶结物的影响,粒度较粗和钙质胶结的砂岩段溶蚀孔隙发育。主要的成岩作用为压实、胶结、胶结物溶蚀、石英颗粒碱性溶蚀、交代、重结晶以及构造破裂。根据成岩阶段划分标准,东河塘组处在中成岩阶段的B期。
通過普通薄片、鑄體薄片、掃描電鏡以及測井等分析手段,對巴麥地區東河塘組上砂巖段和下砂巖段的沉積特徵、巖石學特徵、成巖作用進行瞭詳細分析。東河塘組沉積環境為濱岸相,具有較高的成分成熟度和結構成熟度,且上砂巖段的成分成熟度和結構成熟度都要高于下砂巖段。儲集空間類型主要為溶蝕孔隙,其分佈主要受粒度和粒間膠結物的影響,粒度較粗和鈣質膠結的砂巖段溶蝕孔隙髮育。主要的成巖作用為壓實、膠結、膠結物溶蝕、石英顆粒堿性溶蝕、交代、重結晶以及構造破裂。根據成巖階段劃分標準,東河塘組處在中成巖階段的B期。
통과보통박편、주체박편、소묘전경이급측정등분석수단,대파맥지구동하당조상사암단화하사암단적침적특정、암석학특정、성암작용진행료상세분석。동하당조침적배경위빈안상,구유교고적성분성숙도화결구성숙도,차상사암단적성분성숙도화결구성숙도도요고우하사암단。저집공간류형주요위용식공극,기분포주요수립도화립간효결물적영향,립도교조화개질효결적사암단용식공극발육。주요적성암작용위압실、효결、효결물용식、석영과립감성용식、교대、중결정이급구조파렬。근거성암계단화분표준,동하당조처재중성암계단적B기。
According to the analyses of rock slice, cast slice, SEM and well logging data, the sedimentary, petrologic characteristics and diagenesis of the upper and the lower sandstone segments of the Donghetang Formation in the Bachu-Maigaiti area were studied. Deposited in littoral environment, the Donghetang Formation was featured by higher compositional maturity and textural maturity, and both of the 2 maturities were higher in the upper sandstone segment than in the lower one. Dissolution pores served as the main reservoir space, and their distribution was determined by grain size and intergranular material. For example, the dissolution pores were well developed in the sandstone segment with bigger grain size and calcareous cementation. The most important diagenesis effects included compaction, cementation, cement dissolution, quartz alkali dissolution, metasomasis, recrystallization and structure cataclasis. According to the division standard of diagenetic phase, the Donghetang Formation was in the B stage of middle phase.