论文部分内容阅读
穆家庄铜矿床矿体呈层状、似层状沿构造破碎带产出 ,矿物组构显示了同生沉积和改造特征 ,流体包裹体为高盐度的热卤水 ,矿石及围岩氧、碳同位素具同一来源 ,矿床成因属变质和构造改造的热水喷流沉积类型。
The ore bodies of the Mujiazhuang copper deposit are stratified and appear to be stratified along the structural crustal belt. The mineral assemblages show syngenetic sedimentary and remodeling characteristics. The fluid inclusions are high-salinity hot brine, ore and surrounding rock oxygen , Carbon isotopes with the same source, the deposit belongs to a metamorphic and tectonic transformation of the hot water jet deposition type.