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作 者:冯学仕
机构地区:[1]贵州地矿局103地质大队
出 处:《贵州地质》1995年第3期204-207,共4页Guizhou Geology
摘 要:基于湘黔汞矿带中客观上存在(铅)锌矿的事实,近年来常有当地群众在汞矿区内明采(铅)锌矿石,又鉴于汞、(铅)锌元素地球化学习性近似,二者在矿田内共消共长,密切伴生,产出特征类同,是同一控制因素,同一地质作用条件下元素分异差异就位的产物,最后,提出了在湘黔汞矿带(大硐喇等矿田)开展(铅)锌矿的普查评价工作。In the Dadongla mercury field of eastern Guizhou, there have recently been a few of local activities of open mining Pb-Zn ores-a hint of the occurence of lead-zinc deposits in the well-known mercury belt between eastern Guizhou and western Hunan. For this reason, the author, on the basis of the similarities in geochemical behavior of elements Hg,Pb-Zn and in their characteristic of occurence, with combination of their spatial relation within epithermal ore-forming belts,believed that it is quite possible to find Pb-Zn deposits within the mercury orefield and made a proposal that it be highly necessary to mount the exploration program and futher evaluation for lead-zinc deposits in these areas.
分 类 号:P618.680.8[天文地球—矿床学]
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