海拉尔盆地乌尔逊凹陷大磨拐河组成岩作用研究DIAGENESIS OF DAMOGUAIHE FORMATION OF WUERXUN DEPRESSION IN HAILAER BASIN
隋少强，宋丽红，张金亮
Sui Shaoqiang;
摘要(Abstract)：
本文分析了乌尔逊凹陷大磨拐河组的岩石矿物、泥岩演化，孔隙演化等特征，得出压实作用导致了早期孔隙度的降低，自生胶结物充填了粒间孔隙，溶解作用产生了次生孔隙，温度是埋藏成岩过程中的主要因素，成岩阶段分成早期、中期和晚期３个阶段。
This paper analyzes the characteristics such as rock minerals and mudstone evolution etc.of Damoguaihe formation of Wuerxun depression and nakes the following conclucsions:Compaction results in early stage porosity decrease;inte-granular pores are filled by authigenic cement;diasslution leads to secondary pores;tempernture is the major factor during the process of diagenesis and diagenesis stage is divided into early, medium and late periods.
关键词(KeyWords)：
乌尔逊凹陷，大磨拐河组，成岩作用，成岩演化，压实作用，孔隙演化，海拉尔盆地
Wuerxun depression, Damoguaihe Formation, Diagenesis, Diagenesis evolution,Campection,Pore evolution, Hailaer basin
基金项目(Foundation):
作者(Authors):
隋少强，宋丽红，张金亮
Sui Shaoqiang;
DOI: 10.19597/j.issn.1000-3754.1996.04.003