开阳县花梨乡清水江地质特征和成矿特征分析  

Analysis of Kaiyang County Township Pear River water geological characteristics and metallogenic characteristics

作　　者：周高[1] 

机构地区：[1]贵州省地质矿产勘查开发局106地质大队,贵州遵义563000

出　　处：《世界有色金属》2017年第9期108-109,共2页World Nonferrous Metals

摘　　要：开阳是贵州三大磷矿产地之一,开阳地区磷矿成矿区受到地层、岩性、构造、沉积环境及古地理等多种因素的影响。对此,本文首先介绍了贵州省磷矿矿床成因,然后以开阳县花梨乡清水江磷矿为研究对象,对开阳县花梨乡清水江磷矿地质特征以及成矿特征进行了详细探究,以期为矿山建设及探矿工作提供借鉴。Shenyang Guizhou is one of the three major metallogenic region of phosphate rock phosphate mines affected area was Kaiyang strata, tectonic and sedimentary environment and paleogeography factors. In this regard, this paper first introduces the genesis of phosphorite in Guizhou Province, then in Kaiyang County of pear Township Qingshuijiang phosphate as the research object, the geological features of river water and phosphate Kaiyang County pear Township metallogenic characteristics are explored in detail, in order to provide the reference for the mine construction and exploration.

关 键 词：开阳县 磷矿 古地理 

分 类 号：P619.2[天文地球—矿床学]