摘要
本文据最新的物探资料及样品测试结果认为：吴伯浩金、银、铜、铅、锌多金属矿化类型为浅成中低温热液充填型，成矿流体物化环境为低盐度、低密度、弱酸性一近中性贫硫低氧的弱还原环境，其热液来源于深部次火山岩浆活动；中深部可能赋存有铅锌矿床和浸染状斑岩型铜矿床。
According to the lateast geophysical prospecting data and sample testing results, it is advanced that the polymetallic mineralization including An, Ag, Cu, Pb and Zn belongs to the type of shallow-seated low-to-moderate temperature hydrothermal infilling, the deep-seated subvolcanic magmatic activity is the source of the hydrothermal solution and the ore-forming fluid is in the physical-chemical environment of weak reductant characterized by low-density, low -salinity, weak acidic-approaching nautral, poor sulphur and low oxygen. Lastly, it is prognosticated that there may be medium-deep seated lead-zine deposit and porphyry copper deposit occurenced in Wubohao area.
出处
《资源环境与工程》
1998年第1期22-27,共6页
Resources Environment & Engineering
关键词
吴伯浩
矿化类型
热液来源
中深部
铅锌
铜
Wubohao mineralization type source of the hydrothermal solution medium-deep seated lead-zine copper
