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J4 ›› 2009, Vol. 17 ›› Issue (5): 36-41.

• article • Previous Articles     Next Articles

Geological Characteristics and Prospecting Criteria of Ag-Pb Polymentallic Deposit in Highland 1017, Inner Mongolia

HUANG Zhongjun, WANG Guichun   

  1. NO.4 Gold Geological Party of CAPF, Liaoyang 111000, Liaoning, China
  • Received:2009-01-12 Revised:2009-03-19 Online:2009-10-30 Published:2011-09-29

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Abstract:

Ag-Pb polymeta llic m ining area of highland 1017 is a kind ofmagmatic hydrothermal Ag-Pb polymetallic deposit found in the northeast part of Xilinguole league, Inner Mongolia. Large-scale geological survey and comprehensive research for it are in process. The major source beds are medium-coarse and medium-finegrained biotite adamellite of late Yanshan era, the folds and faults structure provide spaces for the polymetallicm ineralization. The important indicators of finding Ag-Pb polymetallic ore include structure fracture zone and tectonic breccia inrocks, the geological body with a variety of altered andm ineralized, the polarizab ility anomaly area delineated by the geophysical IP intermediate gradient, and the low resistivity geological body delinaeated by controllable source audio-frequency magneto telluric sounding. There are the ore-controlling factors for large ormedium Ag-Pb polymetallic ore in high land 1017.

Key words: Ag-Pb polymetallic ore, Geological characteristics, Prospecting criteria, Highland 1017, Inner Mongolia

CLC Number: 

  • P618.51


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