摘要
古利库金（银）矿床的形成与早白垩世中晚期火山喷发活动及其所形成的火山穹隆构造有关，矿体定位于火山活动波及范围内，平均成矿温度220℃，平均成矿压力135×10^5Pa，成矿深度约500～600m，属冰长石—绢云母型浅成低温热液矿床，与国内外同类型矿床具有可比性。
Formation of Guliku Gold （Silver） deposit is related with volcanic eruption and dome -shaped volcanic structure formed in the middle - late period of early cretaceous. The deposit is located in the volcano - affected area. Average mineralizing temperature is 220℃, average pressure is 135 × 10^5Pa, and forming depth is about 500～600m. The deposit belongs to adularia- sericite type epithermal one, which can be compared to the same types from China and other areas.
出处
《地质与勘探》
CAS
CSCD
北大核心
2006年第5期23-27,共5页
Geology and Exploration
基金
地科定96-08项目资助
