摘要
通过对红山铜矿普查区角砾岩产出的地质环境、火成角砾岩体形态产状规模和角砾岩的岩石学、蚀变与矿化特征的研究 ,运用作者十多年来摸索、完善的“古水热活动区成矿”和“三阶成矿”理论 ,大胆提出该区成矿活动规模有限的结论。
Based on research of geological settings, form, occurrence, scale, petrological and alteration features of igneous breccia and with the prospecting theory of “mineralization in paleo-hydrothermal active area” and “mineralization related to three-stage granitoids”, the authors conclude that the scale of mineralization in the studied area is quite limited.
出处
《华南地质与矿产》
CAS
2001年第1期9-16,共8页
Geology and Mineral Resources of South China
基金
地质矿产部定向研究基金项目"武夷山地区火成角砾岩与成矿关系及找矿标志研究"(直科定 91- 2 3)的部分成果
