通过岩心资料、镜下薄片鉴定、测井资料解释等,对合川地区须二段的储层特征及其主控因素进行了深入的研究。研究区储层物性主要受沉积作用和成岩作用的双重控制。储层岩性主要以岩屑长石砂岩和长石岩屑砂岩为主,属于低孔低渗致密砂岩。须二段主要为三角洲前缘相沉积。有利储层发育的微相为水上分流河道和河口坝。有利储层发育的成岩作用主要是环边绿泥石胶结、溶蚀作用、构造破裂作用。
By analyzing core data, thin slice and logging data interpretation, this paper deeply investigated the reservoir characteristics and controlling factors of the Xu-2 member in Hechuan area. Reservoirs physical properties of study area are double controlled by sedimentation and diagenesis. The reservoir lithology mainly of the lithic arkose and the feldspathic litharenite belongs to low porosity and low permeability tight sandstone. Xu-2 member is mainly of the delta front facies deposition. The favorable sedimentary subfacies for reservoir are distributary channels and mouth bars. The favorable diagenesis for reservoir are rim chlorite cementation, denudation and tectonic disruption.