首页> 外文期刊>Transactions of the Institutions of Mining and Metallurgy, Section B. Applied Earth Science >Favourable tectonic setting and fracture network environment for the formation of the giant Kadjaran porphyry Cu-Mo deposit in Armenia, Lesser Caucasus
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Favourable tectonic setting and fracture network environment for the formation of the giant Kadjaran porphyry Cu-Mo deposit in Armenia, Lesser Caucasus

机译:亚美尼亚巨大的kadjaran斑岩矿床形成的有利构造和骨折网络环境,较小的高加索

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摘要

The giant Kadjaran porphyry Cu-Mo deposit is situated in the southernmost Lesser Caucasus in Armenia and belongs to the Central segment of the Tethyan metallogenic belt. Cenozoic evolution of this segment was dominated by oblique convergence and final collision of the Arabian plate with the Eurasian margin. The composite Meghri-Ordubad pluton of the southernmost Lesser Caucasus was emplaced during this evolution. It hosts major porphyry Cu-Mo and epither-mal Au deposits and prospects, including the giant Oli-gocene Kadjaran porphyry Cu-Mo deposit.
机译:巨大的Kadjaran斑岩铜钼矿床位于亚美尼亚最南端的小高加索地区,属于特提斯成矿带的中段。该段新生代的演化主要是阿拉伯板块与欧亚大陆边缘的斜向会聚和最终碰撞。小高加索最南端的Meghri-Ordubad复合深成岩体是在这一演化过程中侵位的。它拥有主要的斑岩铜钼和浅层金矿床和前景,包括巨大的Oli gocene Kadjaran斑岩铜钼矿床。

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