Microfacies and depositional environments of the Asmari Formation, at Dehdez area (a correlation across central Zagros basin)

被引：0
作者：
Ali Seyrafian
机构：
[1] University of Esfahan,Geology Department, Faculty of Sciences
来源：
Carbonates and Evaporites | 2000年 / 15卷
关键词：
Foraminifera; Depositional Environment; Microfacies; Grainstone; Wackestone;
D O I：
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摘要：
The predominant microfacies of the Asmari Formation at Dehdez area are: (1) globigerinid bioclastic wackestone to packstone, (2) globigerinid laminated wackestone, (3) coral and coralline algal boundstone, (4) bioclastic-lithoclastic wackestone to packstone, (5) foraminifera bioclastic wackestone to packstone, (6) foraminifera grainstone, (7) peloid wackestone to packstone, and (8) peloid bioclastic grainstone.
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页码：121 / 129
页数：8
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