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Occurrence of the Pholopite-Spinel-Corundum-Sapphirine Assemblages in the Contact Between Granulites and Peridotites Massif at the Beni Bousera(Morocco)
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作者 barich amel M.L.Bouybaouène 《地学前缘》 EI CAS CSCD 北大核心 2009年第S1期218-218,共1页
The Beni Bousera peridotite massif(Internal Rif, Morocco),5 km in width and 15 km in length,is formed in a major part of spinel-bearing lherzolite rimed by a layer of garnet-bearing peridotite(100 m thick)which is in ... The Beni Bousera peridotite massif(Internal Rif, Morocco),5 km in width and 15 km in length,is formed in a major part of spinel-bearing lherzolite rimed by a layer of garnet-bearing peridotite(100 m thick)which is in direct contact with HP-HT granulite metamorphic rocks(16 kbar,860℃).According to recent detailed study,the shearing contact between these two formations shows the presence of serpentinite and 展开更多
关键词 PHLOGOPITE CORUNDUM saphirine METASOMATISM PERIDOTITES Rif Morocco
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