摘要
通过对赋存于麻山群老地层且与岩浆热液有关的老柞山金矿床的矿床地质及稳定同位素地球化学特征的研究分析，得出老柞山金矿床与岩浆岩、构造和麻山群密切相关，岩浆热液提供主要的物源和热源。
Based on the studies of geology and isotope geochemistry of Laozhuoshan
gold deposit, we can get important information about the deposit. It is concluded that magmatic
hydrothermal fluid provides ore forming material, and ore forming material has the character of
deep and single source (derived form upper mantle and lower crust). The deposit is closely
related to magmatic thermal fluid, structure and Mashan group (Ptm). This is confirmed by
regional geology and the characters of Pb, S, C and O stable isotopes.
出处
《地质找矿论丛》
CAS
CSCD
1999年第1期48-52,87,共6页
Contributions to Geology and Mineral Resources Research
