埃及东部沙漠Wadi Heimur地区的密西西比有孔矿物大理石

Abd-Elmohsen A. Ahmed
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引用次数: 1

摘要

在纳赛尔湖以东的Wadi Heimur地区,暴露出一层厚度为3 m的软质有孔岩石墨大理岩带,其上覆为厚度达40 m的灰色层状大理岩带,并与低级的古地槽变质沉积物和变质火山相互交错。它以前被认为是前寒武纪(El Shazly et al. 1973,1977 and Hunting 1967)。石墨大理石含有稀有的砂质密西西比有孔虫,包括Ammobaculites, Lituotubella等。,古ospiroplectammina cf. mellina, Trochammina和Endothyra。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mississippian foraminiferal marble from Wadi Heimur Area, Eastern Desert, Egypt

A soft foraminiferal graphitic marble band of 3 m thickness overlying and grading into a grey laminated marble band up to 40 m in thickness interbanded with low grade eugeosynclinal metasediments and metavolcanics is exposed in the Wadi Heimur Area to the east of Lake Nasser. It has been considered previously as Pre-Cambrian (El Shazly et al. 1973, 1977 and Hunting 1967). The graphitic marble contains rare arenaceous Mississippian foraminifera comprising Ammobaculites, Lituotubella cl., Palaeospiroplectammina cf. mellina, Trochammina and Endothyra.

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