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《Geology and Resources》 2013-05
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GEOLOGICAL CHARACTERISTICS AND PROSPECTING TARGETS OF THE QAGAN OBO Fe-Zn POLYMETALLIC DEPOSIT IN INNER MONGOLIA

CHANG Chun-jiao;CONG Run-xiang;LIU Gui-ge;QI Li-hua;WANG Zhi-hua;WANG Liang;ZHANG Hui-yu;KONG Yuan-yuan;Institute of Gold Geology,CAPF;  
The Qagan Obo Fe-Zn polymetallic deposit tectonically lies in the eastern part of the Early Paleozoic Qagan Obo-Aoyoute-Chaobuleng tectonomagmatic belt. The Middle Ordovician Duobaoshan Formation, serving as the main host,is closely related to the metallogenesis. The skarn zones with Fe-Zn and Mn layers commonly occur at the contact between Qagan Obo quartz diorite stock and the neritic facies sedimentary rocks of Duobaoshan Formation. The Fe-Zn orebodies are mainly hosted by the skarn in stratiform, banded or lenticular shapes. The Qagan Obo quartz diorite stock supplies not only the ore materials, but also the ore-forming fluid and dynamic. The regional NE-striking Qagan Obo-Dongwuqi deep fault controls the occurrences of rock bodies and polymetallic deposits. The secondary NE- and NW-trending fractures control the distribution Fe-Zn orebodies. The favorable areas for seeking Fe-Zn polymetallic deposits are the contact zones between the multi-staged acid-intermediate magmatic intrusions and the neritic facies sedimentary rocks of Middle Ordovician Duobaoshan Formation and the concentrated fissure belts in the wallrocks.
【Fund】: 中国地质调查局矿产资源远景调查评价项目(编号1212011085263)资助
【CateGory Index】: P618.2
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