滇东南地区岩子脚锰矿床矿物学特征及其指示意义

	滇东南地区岩子脚锰矿床矿物学特征及其指示意义
	段建兵; 符亚洲; 肖加飞; 张正伟
	2015
Source Publication	矿物学报
Issue	S1
Abstract	滇东南地区是我国典型的中三叠世锰成矿域和主要的优质富锰矿产区,具有地域小而矿床分布集中的特点。目前该区已发现斗南、老乌、岩子脚、大箐、汤得、倘甸等矿床、矿点30余处,其中以斗南最为著名,有斗南锰矿带之称。前人对斗南锰矿带进行了许多矿床地质和岩相古地理等方面的研究(牟传龙等,1991;罗崇迅等,1992),但由于该区锰矿床矿物组成较为复杂且矿物结晶程度差、多为隐晶质或显微隐晶质,因此,系统的矿物学工作开展较少,总体认识程度偏低。
Keyword	锰矿床斗南锰矿滇东南隐晶质倘甸褐锰矿矿床分布岩相古地理同沉积作用矿物学特征
Subject Area	矿床地球化学
Indexed By	CSCD
Language	中文
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/5749
Collection	矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation GB/T 7714	段建兵,符亚洲,肖加飞,等. 滇东南地区岩子脚锰矿床矿物学特征及其指示意义[J]. 矿物学报,2015(S1).
APA	段建兵,符亚洲,肖加飞,&张正伟.(2015).滇东南地区岩子脚锰矿床矿物学特征及其指示意义.矿物学报(S1).
MLA	段建兵,et al."滇东南地区岩子脚锰矿床矿物学特征及其指示意义".矿物学报 .S1(2015).

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