Petrogenesis of cogenetic silica-oversaturated and -undersaturated syenites of Abu Khruq ring complex, South Eastern Desert, Egypt
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文摘

Concluding that the magma sources of Abu Khruq Ring Complex (ARC) are not derived from normal primitive mantle.

Emphasizing that the Silica-Oversaturated and -Undersaturated Syenites in ARC have a cogenetic relationship.

First time using the microprobe analysis of amphiboles and pyroxenes of different rock units of ARC.

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