Depositional Environments in Carbonate Rocks
Depositional Environments in Carbonate Rocks
复制标题
碳酸盐岩的沉积环境
DOI：
10.2110/pec.69.03
复制
发表时间：
1969
期刊：
影响因子：
--
通讯作者：
G. Friedman
中科院分区：
文献类型：
--
作者：
G. Friedman
地质学家的主要任务之一是确定岩石沉积的沉积环境。尽管自从地层学成为地质学的一个既定分支以来，人们就已经了解了海侵和海退、海岸线运动以及大陆和海洋沉积的总体方面的区域环境解释，但沉积学直到最近才提出了对特定露头、井甚至手工样本的环境识别标准。这一观察结果对于碳酸盐岩尤其如此。本卷中的论文将为认识碳酸盐岩沉积环境这一主题提供一把钥匙。基于 1967 年 4 月在加利福尼亚州洛杉矶举行的 AAPG 和 SEPM 联席会议上的研讨会。
One of the principal tasks of the geologist is to determine the depositional environments in which rocks are deposited. Although regional environmental interpretations of transgressions and regressions, movements of shoreline, and gross aspects of continental and marine sedimentation have been understood since stratigraphy became an established branch of geology, only recently has the science of sedimentology come up with criteria for environmental recognition of specific outcrops, wells, or even hand samples. This observation is especially true of carbonate rocks. The papers in this volume will provide a key to the subject of recognition of depositional environments in carbonate rocks. Based on a symposium held in Los Angeles, California, on April 1967, at the joint meeting of AAPG and SEPM.