2010Mineral Resources and GeologyRequires access

The metallogenic condition and prospect analysis of porphyry copper-molybdenum deposit in Antuoling

Shen Liu-sheng

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Abstract

The Antuoling porphyry body is located between the two deep fracture zones of Shanghuangqi-Wulonggou and Lingnantai-Zijingguan. It is a hypabyssal-super hypabyssal intermediate-acid magma rock of multiple intrusions with a small scale. It is integrally inclined to the south and pitched to the southeast as elliptical-shaped. It is strongly altered with the mineralization zoning. It is controlled by flexible shear fracture zones in eastwest,flexible-brittle fracture zones in northeast and cross tension fracture zones in northwest. These feathers all can be compared with ore-bearing porphyries in domestic and abroad. So the metallogenic condition is ascendant in this distinct,it is with the prospect of large-scale porphyry copper-molybdenum deposit.

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What this paper is about

The Antuoling porphyry body is located between the two deep fracture zones of Shanghuangqi-Wulonggou and Lingnantai-Zijingguan. It is a hypabyssal-super hypabyssal intermediate-acid magma rock of multiple intrusions with a small scale. It is integrally inclined to the south and pitched to the southeast as elliptical-shaped. It is strongly altered with the mineralization zoning. It is controlled by flexible shear fracture zones in eastwest,flexible-brittle fracture zones in northeast and cross tension fracture zones in northwest. These feathers all can be compared with ore-bearing porphyries in domestic and abroad. So the metallogenic condition is ascendant in this distinct,it is with the prospect of large-scale porphyry copper-molybdenum deposit.

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Available abstract

The Antuoling porphyry body is located between the two deep fracture zones of Shanghuangqi-Wulonggou and Lingnantai-Zijingguan. It is a hypabyssal-super hypabyssal intermediate-acid magma rock of multiple intrusions with a small scale. It is integrally inclined to the south and pitched to the southeast as elliptical-shaped. It is strongly altered with the mineralization zoning. It is controlled by flexible shear fracture zones in eastwest,flexible-brittle fracture zones in northeast and cross tension fracture zones in northwest. These feathers all can be compared with ore-bearing porphyries in domestic and abroad. So the metallogenic condition is ascendant in this distinct,it is with the prospect of large-scale porphyry copper-molybdenum deposit.

Key concepts: Geology, Geochemistry, Porphyry copper deposit, Molybdenum, Mineralization (soil science), Fracture (geology), Magma, Shear (geology)

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