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湘黔汞矿是我国产汞最富和开采最早的地区。其地質情况早经許多地質学者加以研究,一般論述較为詳尽,但对汞矿床的構造控制,論述的尚感不足。众所周知,一般具有工业价值的汞矿床,都是低温热液矿床,矿物成份簡单,所以划分汞矿床工业类型的主要基础是構造关系和矿床形态。而矿床形态主要又受構造控制,其关系甚为密切。因而笔者拟根据兩年来在湘黔汞矿工作中的体会,分为以下五个部份加以简单的說明。錯誤之处,希同志們多加指正。
Xiang Qian mercury mine is the richest and the earliest mining area in our country. Its geological conditions have been studied by many geologists as early as possible, and the general discussion is more exhaustive. However, the structural control of mercury deposits is not yet discussed. It is well-known that mercury deposits, which are generally of industrial value, are low-temperature hydrothermal deposits and have a simple mineral composition. Therefore, the main basis for the division of the mercury-bearing industrial type is the tectonic relationship and the morphology of the deposit. The deposit morphology is dominated by the structure, the relationship is very close. Therefore, according to two years of my work in Hunan and Guizhou mercury mine experience, divided into the following five parts to be a simple description. Wrong place, Greek comrades more correct.