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- W2059724196 abstract "In the Precambrian Zenaga inlier (boutonniere) in the Anti-Atlas of Morocco, many quartz veins crosscut the Ebournian (Precambrian) basement. The quartz veins predate the deposition of the overlying Precambrian III units, and were probably the feeding channels for the overlying jasperoid formation. The fluid inclusion microthermometry and textural studies show the evolution in a single crystal, from intensely recrystallized inclusions to almost untouched ones recording the uplift of the Ebournian basement. The uplift provoked the over-pressure of the inner fluid inclusions and their explosion, giving rise to hook-like or decrepitation cluster textures, while the fluid inclusions located in the outer zones only show necking-down phenomena. q 2000 Elsevier Science B.V. All rights reserved." @default.
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- W2059724196 date "2000-06-01" @default.
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- W2059724196 title "Geotectonic significance of the textural evolution of fluid inclusions in Precambrian quartz veins from the “Boutonnière de Zenaga” (Anti-Atlas, Morocco)" @default.
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- W2059724196 doi "https://doi.org/10.1016/s0375-6742(00)00028-5" @default.
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