资阳地区震旦系古岩溶作用及其特征讨论  

Paleokarst and Its Characteristics of Dengying Formation in Ziyang Area

作　　者：向芳[1] 陈洪德[1] 张锦泉[1] 

机构地区：[1]成都理工学院沉积地质研究所,成都610059

出　　处：《沉积学报》2001年第3期421-424,共4页Acta Sedimentologica Sinica

基　　金：国家九五攻关二级专题"四川盆地加里东古隆起震旦;寒武系储层研究及横向预测"资助项目

摘　　要：在资阳地区震旦系灯影组的白云岩地层中发现了四川盆地又一含气区块 ,通过对地层资料、露头特征及构造史的分析研究 ,证实该储层为古岩溶作用的产物 ,在此基础上对古岩溶的分带性、旋回性及岩溶地貌特征进行了讨论 。In Ziyang area, another gas bearing block in Sichuan Basin has been found in Sinian Dengying Formation. Dengying Formation is a set of carbonate sediments, which includes algal granula dolostone, algal cementation dolostone, micrite dolostone and crystal powder cryptomere dolostone. To the origin of the gas bearing block, there are some different explanations: 1) the result of weathering, meteoric water leaching and later tectonic process; 2) formed by recrystallization and later burial dissolution; 3) generated by dolomitization and dissolution; 4) main control factor being paleokarst. According to the study of seven drills, regional exposure characteristic and tectonic evolution history, it can be concluded that paleokarst existed in Dengying Formation in this area and it took place during Tongwan Movement at the end of Sinian. Paleokarst profile can be divided into three zones: surface, vadose and phreatic dissolution zones. In the vadose and phreatic dissolution zones, four karst forms can be found : dissolved fissure, spelaeum, dissolved hollow and cave. In this area, two karst cycles can be identified in Dengying Formation. The layer which formed by superposition of phreatic dissolution zone in first cycle and vadose zone in second cycle is the position where karst is the most developed, and the maximum vugular pore space is 42.5%. According to study, it can be found that Cambrian silicon phosphorus sediments have the characteristics of compensation sedimentation, which lie on the relic Dengsan and Dengsi section. On the basis of thickness of silicon phosphorus sediments, the paleokarst topography can be reconstructed,i.e: in south west, it is mosor high land; in north east, it is mosor bottom; between them there is a mosor slope. All topography shows from higher in south west to lower in north east. All of these provide the necessary information for the research on reservoir characteristics and forecast prospecting targets.

关 键 词：资阳地区 灯影组 古岩溶作用 岩溶特征 震旦系 储层 旋回性 

分 类 号：P618.130.2[天文地球—矿床学] P642.25[天文地球—地质学]