埃及西南部和苏丹西北部三叠纪和第三纪火山岩的岩石学、地球化学和年龄关系

G. Franz , H. Puchelt , P. Pasteels
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引用次数: 43

摘要

本文介绍了埃及西南部和苏丹北部Gebel Kamil-Lake Nasser-Laqia Arbain-Nile地区火山岩的岩石学、地球化学和K/Ar辐射全岩年龄资料。这些岩石是(i)粗质-声母岩和(ii)碱橄榄玄武岩,主要形成火山塞。它们的岩相和主微量元素模式是典型的大陆板块内火山活动。确定了两组年龄:以硅质岩浆为主的三叠纪(240 ~ 233 Ma)和以玄武质岩浆为主的第三纪(60 ~ 20 Ma)。玄武岩主要元素丰度与岩石年龄无关,呈现由西向东、由低到高的区域分选趋势。它们的出现与两条东西向隆起带有关,这两条隆起带对利比亚沙漠大型沉积盆地的构造发育具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Petrology, geochemistry and age relations of Triassic and Tertiary volcanic rocks from SW Egypt and NW Sudan

Petrological, geochemical and K/Ar radiometrical whole rock age data of volcanic rocks from SW Egypt and N Sudan in the area of Gebel Kamil-Lake Nasser-Laqia Arbain-Nile are presented. These rocks are (i) trachytic-phonolitic rocks and (ii) alkali olivine basalts occurring mostly as volcanic plugs. Their petrographic and their major and trace element patterns are typical for continental within-plate volcanism. Two groups of ages were determined: Triassic (240, 233 Ma) with predominantly silicic, differentiated magmas, and Tertiary (60-20 Ma) with predominantly basaltic magmas. Major element abundances of the basalts show a regional trend from west to east from low to high fractionation irrespective of the age of the rock. Their occurrence can be correlated with two W-E uplift zones which are important for the structural development of the large sedimentary basins of the Libyan desert.

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