尕林格矽卡岩型铁多金属矿床地质-地球物理模型

收稿日期: 2009-06-12

修回日期: 2010-03-09

刊出日期: 2010-06-15

Geologic-Geophysical Model of Skarn Iron-Polymetallic Deposit in Galinge Region

Received Date: 12 June 2009

Revised Date: 09 March 2010

Publish Date: 15 June 2010

摘要: 尕林格矽卡岩型铁多金属矿床是1976-1980年青海省物探队检查航磁M512异常时发现的。通过1:5万、1:5000地面磁法、电法、重力测量和钻探验证、勘探,目前查明矿床规模已达中型以上。鉴于尕林格矿床资料相对齐全,以尕林格矽卡岩型铁多金属矿床为例,建立尕林格矽卡岩型铁多金属矿床地质-地球物理模型,为在该区乃至全省范围内寻找类似矿床奠定基础。
- 矽卡岩型 /
- 铁多金属矿床 /
- 地质-地球物理模型
Abstract: Skarn iron-polymetallic deposit in Galinge region was discovered by Qinghai geophysical prospecting teamduring investigating aeromagnetic anomalies M512 in 1976-1980.After re-exploration and careful analysis by ways of 1:50 000-1:5000 ground magnetic method,electrical method,gravity measurement,and drilling examination,we find that the deposit has reached medium-sized scale.Inview that data of Galinge deposit are relatively complete,geologic-geophysical model of skarn type iron-poly-metallic deposit in Galinge region has been established by taking Galinge Skarn iron-poly metallic deposit as an example.This is of vital significance in looking for similar deposits in Galinge and even the whole Qinghai province.
- Skarn /
- iron-poly metallic deposit /
- geologic-geophysical model