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THE GEOLOGICAL FEATURES AND METALLOGENIC CONDITIONS OF THE COPPER-NICKEL-BEARING BASIC-ULTRABASIC INTRUSIVE IN XINGDI, XINJIANG

Cags Xi

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Abstract

The paper discusses the geological features and metallogenic conditions of the Cu-Nibearing basic-ultrabasic rock body in Xingdi, Xinjiang Autonomous Region. The main conclusions are as follows: (1) The rock body was formed by multiple intrusion of olivine tholeiite magma from the mantle. The diagenetic epoch was Mesoproterozoic, t= 1 209±37 Ma. (2) This intrusive had favourable assemblage of rock and tectonic setting, metallogenic specialization and ore-forming process for formation of Cu-Ni sulfide deposit.

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What this paper is about

The paper discusses the geological features and metallogenic conditions of the Cu-Nibearing basic-ultrabasic rock body in Xingdi, Xinjiang Autonomous Region. The main conclusions are as follows: (1) The rock body was formed by multiple intrusion of olivine tholeiite magma from the mantle. The diagenetic epoch was Mesoproterozoic, t= 1 209±37 Ma. (2) This intrusive had favourable assemblage of rock and tectonic setting, metallogenic specialization and ore-forming process for formation of Cu-Ni sulfide deposit.

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Available abstract

The paper discusses the geological features and metallogenic conditions of the Cu-Nibearing basic-ultrabasic rock body in Xingdi, Xinjiang Autonomous Region. The main conclusions are as follows: (1) The rock body was formed by multiple intrusion of olivine tholeiite magma from the mantle. The diagenetic epoch was Mesoproterozoic, t= 1 209±37 Ma. (2) This intrusive had favourable assemblage of rock and tectonic setting, metallogenic specialization and ore-forming process for formation of Cu-Ni sulfide deposit.

Key concepts: Ultramafic rock, Geology, Geochemistry, Mantle (geology), Tectonics, Intrusion, Olivine, Diagenesis

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