摘要
笔者根据四川盆地东北部长兴组沉积特点,将其分为台地边缘生物礁相、台地边缘浅滩相、开阔台地相、局限台地相、碳酸盐斜坡相、盆地相和蒸发台地相等7个基本的相带。由于期间经历了一次二级海平面的升降过程,使得长兴组广泛发育海侵生物礁滩,形成了两类最为有利的储集相带。礁滩沉积相带在纵横向上不断迁移、抬升,主要发育于台盆的两侧,呈带状分布,明显受沉积相带控制。主要沉积微相类型有生物粘结云岩微相、亮晶颗粒云岩微相、角砾云岩微相、云泥岩微相、生物粘结灰岩微相、灰泥岩微相、亮晶颗粒灰岩微相和介屑灰岩等,其中对储层最有利的微相类型是角砾云岩微相、生物粘结云岩微相和亮晶颗粒云岩微相。在详细研究分析各沉积相带沉积特点的基础上,探讨了该期沉积相带的空间展布。利用钻井、野外露头、岩心和岩石薄片等资料,对目的层进行了沉积相和沉积微相研究的基础上,建立了研究区的沉积模式以及对沉积模式的演化进行了研究,最后编制了沉积相平面分布。
Changxing Formation in northeast Sichuan basin is marine deposit which can be divided into platform margin organic reefs,platform margin shoals,open platform,limited platform,carbonate ramp,basinal facies and platform evaporite facies.Affected by second-grade sea level changes,the transgressive reef-beach bodies are well developed in Changxing Formation,forming two types of favorable reservoirs.The reef-beach facies migrated and uplifted in vertical direction and developed in zonal form on both sides of the basin,controlled by sedimentary facies.The main sedimentary microfacies comprises organisms-bearing dolomite microfacies,sparry grained dolomite microfacies,gravel dolomite microfacies,dolomite mudstone microfacies,organisms-bearing calcite microfacies,sparry grained calcite microfacies and ostrocoda limestone,of which the most favorable microfacies are gravel dolomite microfacies,organisms-bearing dolomite microfacies and sparry grained dolomite microfacies.Based on detailed research on the characteristics of sedimentary facies,drilling data,outcrops,core and thin section observation,the authors have built the sedimentary model and evolution model of the study area and compiled the sedimentary facies distribution map.
出处
《中国地质》
CAS
CSCD
北大核心
2011年第3期594-609,共16页
Geology in China
基金
国家重大专项(2008ZX05005-002-003)资助
关键词
沉积(微)相
沉积模式
古地理演化
长兴组
川东北
碳酸盐岩
sedimentary facies
sedimentary model
palaeogeographic evolution
Changxing Formation
northeast Sichuan basin
carbonate rock
