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- W2392816273 abstract "Ophiolitic melange exposed in the Mandula area, north-central Inner Mongolia, formed by tectonic mixing of fragments of fractured or dismembered incomplete ophiolite. The matrix is composed of serpentine and cataclastic tuffaceous slate that were sheared by structure, and the blocks are ultramafic rocks, gabbros, mafic volcanic rocks and cherts of varying size and shape. The blocks in matrix account for about 30-50%. Metaperidotite shows the characteristics of lower Cr, Ti and Ca and higher Mg, very low content of REE, enrichment of LREE, and positive anomaly of Eu, with MgO/(MgO+FeO.) = 0.86-0.89. Mafic volcanic rocks have the characteristics of MORB and their geochemical characteristics indicate that they may have formed in a small intracontinental oceanic basin. It may be determined that its age indicate that the metagabbro should be formed prior to 433.6±3.6 Ma." @default.
- W2392816273 created "2016-06-24" @default.
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- W2392816273 date "2004-01-01" @default.
- W2392816273 modified "2023-09-23" @default.
- W2392816273 title "Characteristics and tectonic significance of the Solon Mountain ophiolitic mélange in the Mandula area, Darhan Muminggan, Inner Mongolia" @default.
- W2392816273 hasPublicationYear "2004" @default.
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