摘要
达县—宣汉长兴组礁滩白云岩主要成岩作用类型有压实作用、压溶作用、胶结作用、白云石化作用、新生变形作用、溶蚀作用、破裂作用和充填胶结作用等,对研究区储层贡献最大的成岩作用主要是溶蚀作用、新生变形作用和破裂作用。根据岩石中所形成的大量溶蚀孔隙、晶间溶孔和晶间孔以及裂缝的特征,该套礁滩白云岩储层的良好物性主要形成于中—深埋藏环境。
The diagenesis of the reef shoal dolostones from the Changxing Formation in the Daxian-Xuanhan region includes compression, pressure solution, cementation, dolomitization, neomorphism, dissolution, fracturing and infilling-cementation, of which dissolution, neomorphlsm and fracturing serve as most important ones in the study area. Judged from abundant solution openings, intercrystal solution openings, intercrystal pores and fissures and cracks in the reservoir rocks, the good physical properties of the reef shoal dolostone reservoirs should be formed in the moderately and deeply buried environments.
出处
《沉积与特提斯地质》
CAS
CSCD
2006年第1期30-36,共7页
Sedimentary Geology and Tethyan Geology
基金
中石化南方勘探分公司"川东北宣汉-达县地区长兴组-飞仙关组高精度沉积相
层序地层与储层特征研究"
关键词
达县-宣汉
上二叠统
长兴组
礁滩白云岩
成岩作用
川东北
Daxian-Xuanhan region
Upper Permian
Changxing Formation
reef shoal dolostone
diagenesis
northeastern Sichuan
