摘要
马庄山金矿产于下石炭统白山组的一套浅海—滨海相火山碎屑沉积岩、火山碎屑岩和碳酸盐岩建造中 ,是一个典型的与火山 次火山活动有关的中型金矿床 ,在空间和成因上受控于次火山侵入岩体。从矿床地质、流体包裹体、稳定同位素等角度详细论述了金矿的地质特征 ,并进一步探讨了矿床成因。
Mazhuangshan gold deposit is occured in the formation of lower Carboniferous of Baishan Group which composed by neritic littoral facies pyroclastic sedimentary rocks, pyroclastic rocks and carbonate rocks. Its a typical middle sized gold deposit related to volcanic and subvolcanic activity and controlled by subvolcanic intrusive rocks in space and origin. By research mineral deposit geology, fluid inclusion and stable isotope data in detail, the geological features and the genesis of deposit were discussed. Mazhuangshan gold deposit is a meso epithermal deposit which related with acidic intermediate acidic subvolcanic rock in middle Hercynain.
出处
《黄金地质》
2002年第1期21-25,共5页
Gold Geology
