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Permo-Triassic magmatism and metallogeny of Northern Vietnam in relation to the Emeishan plume

机译:越南北部与峨眉山羽流的二叠系-三叠纪岩浆作用和成矿作用

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摘要

We have shown that the occurrences of Permo-Triassic magmatism in northern Vietnam compose the southwestern and southeastern flanks of the Emeishan large igneous province, shifted along the large-amplitude Ailao Shan-Red River shear zone. Based on new geochronological (U-Pb and Ar/Ar) data, two stages of magmatism related to the Emeishan plume have been recognized. At the first, Permian, stage (260 Ma), abundant picritoids of the Song Da and Song Hien zones formed, and at the second, gabbro-syenite and gabbro-monzodiorite associations of the Lo Gam zone, layered peridotite-gabbro massifs of the Nui Chua complex, high-alumina granites of the Phia Bioc complex, and basalt-rhyolite association of the Song Hien zone were produced. The metallogenic specialization of the Permo-Triassic magmatism of northern Vietnam is considered.
机译:我们已经表明,越南北部的Permo-Triassic岩浆作用的发生构成了峨眉山大火成岩省的西南和东南侧面,沿着大幅度的哀牢山-红河剪切带移动。根据新的年代学数据(U-Pb和Ar / Ar),已经认识到与峨眉山羽流有关的两个岩浆作用阶段。在第一个二叠纪阶段(260 Ma),形成了Song Da和Song Hien带丰富的类阿片类动物,第二个则是Lo Gam带的辉长岩-辉长岩和辉长岩-辉闪石结合,形成了该岩层的橄榄岩-闪闪长隆地块。产生了Nui Chua复合物,Phia Bioc复合物的高铝花岗岩以及Song Hien带的玄武岩-流纹岩结合体。考虑了越南北部二叠系-三叠纪岩浆作用的成矿作用。

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