埃及贝尼苏埃夫东部贝尼苏埃夫-El Zaafarana 新路沿线中上更新世露头的构造环境、岩相特征和地球化学方面的问题

Alaa Amin
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引用次数: 0

摘要

始新世的特点是形成了覆盖埃及大片地区的碳酸盐平台。这些始新世碳酸盐岩广泛分布于埃及东部的贝尼苏埃夫地区。在本研究中,我们将从岩石地层学、构造背景、岩相学、地球化学和地质学等方面对这些碳酸盐岩进行研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Structural setting, facies characteristics, and geochemical aspects of the Middle-Upper Eocene outcrops along Beni Suef-El Zaafarana New Road, east of Beni Suef, Egypt
he Eocene epoch is distinguished by the development of a carbonate platform covering a large area of Egypt. These Eocene carbonates are widespread in the eastern Beni Suef region of Egypt. In the present work, the lithostratigraphy, structural setting, petrography, geochemistry
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