2012Unpublished venueRequires access

Old Road Channel Copper Polymetallic Ore Deposit Geology Geochemistry Investigation

Yao De

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Abstract

Laodaogou copper-polymetallic deposit is located at east part of Wulanhaote-Huanggangliang metallogenic belt.On the basis of 1:10000 soil geochemical and 1∶ 10000 IP induced-current middle-gradient surveys and surface geological engineering,several copper-polymetallic ore bodies were outlied.The ore deposit is formed by fracture filling and metasometism and controlled by tectonomagamatism.All regional and metallogenic features show that the Laodaogou area have good exploration prospects.

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Laodaogou copper-polymetallic deposit is located at east part of Wulanhaote-Huanggangliang metallogenic belt.On the basis of 1:10000 soil geochemical and 1∶ 10000 IP induced-current middle-gradient surveys and surface geological engineering,several copper-polymetallic ore bodies were outlied.The ore deposit is formed by fracture filling and metasometism and controlled by tectonomagamatism.All regional and metallogenic features show that the Laodaogou area have good exploration prospects.

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Available abstract

Laodaogou copper-polymetallic deposit is located at east part of Wulanhaote-Huanggangliang metallogenic belt.On the basis of 1:10000 soil geochemical and 1∶ 10000 IP induced-current middle-gradient surveys and surface geological engineering,several copper-polymetallic ore bodies were outlied.The ore deposit is formed by fracture filling and metasometism and controlled by tectonomagamatism.All regional and metallogenic features show that the Laodaogou area have good exploration prospects.

Key concepts: Geology, Geochemistry, Polymetallic replacement deposit, Copper ore, Copper, Channel (broadcasting), Mining engineering, Porphyry copper deposit

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