山西阳城—沁水地区太原组碳酸盐岩的沉积特征及成因类型 |
| |
引用本文: | 刘善印,黄操明,徐萱,杨学成.山西阳城—沁水地区太原组碳酸盐岩的沉积特征及成因类型[J].山西矿业学院学报,1995(3). |
| |
作者姓名: | 刘善印 黄操明 徐萱 杨学成 |
| |
作者单位: | 中科院地质所
(刘善印),山西矿业学院地测系
(黄操明),山西省电力勘测设计院
(徐萱),山西矿业学院总务处(杨学成) |
| |
摘 要: | 本文详细阐述了阳城—沁水地区太原组碳酸盐岩的矿物成分、结构构造、生物组合和氧碳同位素等沉积特征,进而将碳酸盐岩划分为泻湖灰岩、潮间带灰岩、潮下浅水灰岩和风暴灰岩等四种成因类型,并对太原组沉积环境的演化进行了探讨。
|
关 键 词: | 碳酸盐岩 沉积特征 成因类型 沉积环境 |
Depositional characters and genetic types of carbonate rocks of the Taiyuan formation in Yangcheng-Qinshui region, Shanxi |
| |
Authors: | Liu Shanyin Huang Caoming |
| |
Abstract: | On the basis of the analysis of depositional characters of carbonate rocks of the Taiyuan Formation in Yangcheng-Qinshui region,four types of carbonate rocks may be distinguished: lagoon, intertital, subtital and storm deposits. Their sedimentary environments are discussed. |
| |
Keywords: | carbonate rocks depositional characters genetic types sedimentary environments |
本文献已被 CNKI 等数据库收录! |