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- W2362495434 abstract "The Dapingzhang Cu deposit is a multimetallic Cu deposit formed by volcanism. The main ore-body-disseminated ore-body is of a subvolcanic hydrothermal type, which is controlled by dacite volcanic arch and cryptoexplosion breccia pipe structures and occurred in the cryptoexplosion breccia-subvolcanic lithofacies of volcanic channel. The massive ore body is formed in the D 2～C 1 marine-facies volcanic eruption, broken by later structure and emplacement of volcanic-subvolcanic rock body and distribu-ted brecciatedly in the structural fracture zone. Generally speaking, it is a composite Cu deposit of submarine volcanic eruption-exhalation deposition and subvolcanic hydrothermal superimposed reformation." @default.
- W2362495434 created "2016-06-24" @default.
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- W2362495434 date "2001-01-01" @default.
- W2362495434 modified "2023-09-25" @default.
- W2362495434 title "THE GEOLOGICAL CHARACTERISTICS AND METALLOGENETIC MECHANISM OF DAPINGZHANG MULTIMETALLIC CU DEPOSIT, SIMAO" @default.
- W2362495434 hasPublicationYear "2001" @default.
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