内蒙古地区锑矿床特征及成矿规律

doi:10.13686/j.cnki.dzyzy.2023.03.003

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Abstract Based on the study of geological characteristics of antimony deposits in Inner Mongolia and typical antimony deposits, with comparison of the ore-controlling factors between typical antimony deposits in China, the paper discusses the metallogenic regularity of antimony deposits in Inner Mongolia from the aspects of metallogenic tectonic background, ore-bearing rock series and ore-controlling structure. It is considered that the antimony deposits in Inner Mongolia can be classified into hydrothermal type in clastic strata and volcanic hydrothermal type. The ore-bearing rock series in these deposits were mostly formed in Late Paleozoic Devonian-Permian, with the characteristics of nearly E-W linear distribution. The ore/mineralized bodies are mainly controlled by the nearly E-W-trending fault belt, and the mineralization may be related to the subduction-accretion orogeny during plate collision. The dark fine clastic rock series formed in the reduction conditions of littoral facies, neritic facies, bathyal facies or interactive marine-terrestrial sedimentary environment are the favorable horizon for ore-hosting rocks. The formation of antimony hydrothermal solution may be related to the deep mantle-mantle source tectonic magmatic activity.

Key words： antimony deposit typical deposit genetic type metallogenic regularity Inner Mongolia

Received: 10 January 2022

PACS:

P618.6

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	Articles by authors
	BAO De-jun
	LI Rui-rui
	XIE Yuan-hong
	CHEN Fang-pu
	CUI Long-sheng

Cite this article:

BAO De-jun,LI Rui-rui,XIE Yuan-hong等. CHARACTERISTICS AND METALLOGENIC REGULARITY OF ANTIMONY DEPOSITS IN INNER MONGOLIA[J]. GEOLOGY AND RESOURCES, 2023, 32(3): 268-280.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2023.03.003 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2023/V32/I3/268

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