摘要
研究区处于高寒地区,地质勘查程度较低,尤其是矿体目前仅由少量地表工程控制。本文通过对研究区的区域概况、以往的地质勘查情况、区域地层及构造、岩性、地球化学特征等进行了综合性论述,为后续的地质找提供了理论据。
The study area is located in the alpine region, and the degree of geological exploration is relatively low, especially the orebody is only controlled by a small amount of surface engineering at present. In this paper, the regional general situation, geological exploration in the past, regional stratigraphy and structure, lithology and geochemical characteristics of the study area are discussed comprehensively, which provides theoretical basis for the follow-up geological prospecting.
引文
[1]王健,张向飞,卫清.四川省日绒措铜钼锑矿点地质特征及其成因[J].矿物学报,2009,29(z1).
[2]谭康华,张世全.普朗斑岩铜矿蚀变及矿化特点.云南地质,2007,26(3):271-276.