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- W153394080 abstract "The igneous complex of the Al-Hadah escarpment (ca. 600 Ma) consists of a diorite (with gabbroic inclusions)-monzogranite-granodiorite complex intruded by many dikes of essentially the same composition as the plutonic rocks. The plutonic rocks intruding the earlier basement trend from older dioritic rocks to younger granites. Chemical data indicate two magma sources which we interpret as coming from mantle and crust. The timing of dikes indicates that both magma sources operated at the same time which implies that more basic magmas were trapped beneath partially molten crust." @default.
- W153394080 created "2016-06-24" @default.
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- W153394080 date "1979-01-01" @default.
- W153394080 modified "2023-09-27" @default.
- W153394080 title "THE AL-HADAH IGNEOUS COMPLEX: PRODUCT OF PAN-AFRICAN SUBDUCTION" @default.
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- W153394080 doi "https://doi.org/10.1016/b978-0-08-024467-9.50014-9" @default.
- W153394080 hasPublicationYear "1979" @default.
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