辽宁省瓦房店市磨盘山石灰岩矿床地质特征

doi:10.13686/j.cnki.dzyzy.2009.04.009

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Abstract The Mopanshan limestone deposit, located in Wafangdian City, Liaoning Province, occurs in the second member of Cambrian Zhangxia formation. The Middle Cambrian Xuzhuang and Zhangxia formations and Upper Cambrian Gushan and Changshan formations cropped in the ore field belong to a suit of sediment sequence dominated by limestone. The ore bodies are in stratiform, with well continuity and large scale. The structures in the ore field are simple, without magmatic rock crops. According to the lithology and rock association, the deposit is of chemical or biochemical sedimentary type.

Key words： limestone geological features chemical or biochemical sedimentary deposit Liaoning Province

Received: 31 May 2009

PACS:

P619.22

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	Articles by authors
	XU Hong-bin
	LIN Shao-quan
	ZHANG Guo-gang

Cite this article:

XU Hong-bin,LIN Shao-quan,ZHANG Guo-gang. GEOLOGICAL FEATURES OF THE MOPANSHAN LIMESTONE DEPOSIT IN WAFANGDIAN CITY, LIAONING PROVINCE[J]. GEOLOGY AND RESOURCES, 2009, 18(4): 270-273.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2009.04.009 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2009/V18/I4/270

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