山东科技大学学报:自然科学版
山東科技大學學報:自然科學版
산동과기대학학보:자연과학판
Journal of Shandong Univ of Sci and Technol: Nat Sci
2011年
6期
65-72
,共8页
张超%李旭平%钟建华%张涛锋
張超%李旭平%鐘建華%張濤鋒
장초%리욱평%종건화%장도봉
巴喀%致密砂岩%沉积作用%成岩作用%构造
巴喀%緻密砂巖%沉積作用%成巖作用%構造
파객%치밀사암%침적작용%성암작용%구조
Baka%compact sandstone%sedimentation%diagenesis%structure
运用层序地层手段,结合主要探井、地震资料,确定对比标志层;通过钻井,测井资料,划分基准面旋回,建立地层格架。通过关键井单井相、岩心观察和描述,编制综合井柱状图。经薄片鉴定、扫描电镜及X-衍射粘土矿物分析,认为储层颗粒整体较粗,胶结物含量低、成分成熟度和结构成熟度高,普遍含塑性岩屑、发育亩电利石等多因素共同导致了储层的致密化。储集空间主要为粒闽孔和粒内溶蚀孔。
運用層序地層手段,結閤主要探井、地震資料,確定對比標誌層;通過鑽井,測井資料,劃分基準麵鏇迴,建立地層格架。通過關鍵井單井相、巖心觀察和描述,編製綜閤井柱狀圖。經薄片鑒定、掃描電鏡及X-衍射粘土礦物分析,認為儲層顆粒整體較粗,膠結物含量低、成分成熟度和結構成熟度高,普遍含塑性巖屑、髮育畝電利石等多因素共同導緻瞭儲層的緻密化。儲集空間主要為粒閩孔和粒內溶蝕孔。
운용층서지층수단,결합주요탐정、지진자료,학정대비표지층;통과찬정,측정자료,화분기준면선회,건입지층격가。통과관건정단정상、암심관찰화묘술,편제종합정주상도。경박편감정、소묘전경급X-연사점토광물분석,인위저층과립정체교조,효결물함량저、성분성숙도화결구성숙도고,보편함소성암설、발육무전리석등다인소공동도치료저층적치밀화。저집공간주요위립민공화립내용식공。
By means of the sequence stratigraphy and combining with main exploratory wells and seismic data the comparative key bed was determined. The sedimentary base cycles was divided and the stratigraphic framework was established with the drilling and logging data. The columnar section of comprehensive well was made through the study of single-well phase of key wells, the observation and description of cores. By thin section authentication, electron microscopy scanning and X-ray diffraction of clay mineral analysis,the grain size of particles composed the reservoirs was quite coarse as a whole,and the low cement content,low compositional maturity and high textural maturity,generally with plastic debris,and the development of illite and many other factors led to the reservoir compaction. Accumulation capacity of the reservoirs mainly displays intergranular pores and intragranular dissolution pores.