2002Unpublished venueRequires access

METALLOGENIC REGULARITY OF NORTHERN WEST TIENSHAN:A PRELIMINARY DISCUSSION

Peng Shen

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Abstract

Seven metallogenic belts can be divided in northern west Tienshan: Alato W、Sn、Cu、Fe、Au metallogenic belt; Wenquan Bianzhentao Cu、Nb、Ta metallogenic belt; Hanjigan Pb、Zn metallogenic belt; Sailimu Cu polymetal metallogenic belt; Keguqin Cu polymetal metallogenic belt; Boluohuoluo Au metallogenic belt; Aletan Au metallogenic belt. The ore deposits display paragenesis superpositon and heterogeneity for distribution on account of complexity for mineralization and control of minerogenic evolution.

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What this paper is about

Seven metallogenic belts can be divided in northern west Tienshan: Alato W、Sn、Cu、Fe、Au metallogenic belt; Wenquan Bianzhentao Cu、Nb、Ta metallogenic belt; Hanjigan Pb、Zn metallogenic belt; Sailimu Cu polymetal metallogenic belt; Keguqin Cu polymetal metallogenic belt; Boluohuoluo Au metallogenic belt; Aletan Au metallogenic belt. The ore deposits display paragenesis superpositon and heterogeneity for distribution on account of complexity for mineralization and control of minerogenic evolution.

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Available abstract

Seven metallogenic belts can be divided in northern west Tienshan: Alato W、Sn、Cu、Fe、Au metallogenic belt; Wenquan Bianzhentao Cu、Nb、Ta metallogenic belt; Hanjigan Pb、Zn metallogenic belt; Sailimu Cu polymetal metallogenic belt; Keguqin Cu polymetal metallogenic belt; Boluohuoluo Au metallogenic belt; Aletan Au metallogenic belt. The ore deposits display paragenesis superpositon and heterogeneity for distribution on account of complexity for mineralization and control of minerogenic evolution.

Key concepts: Geology, Paragenesis, Geochemistry, Mineralization (soil science), Mining engineering, Metamorphic rock, Soil science, Soil water

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