世界上大部分的汞储量和汞产量是来自石英-迪开石型汞矿床。石英-迪开石型汞矿床的特点是:围岩常为厚层陆源沉积岩(呈复合互层状或含有均匀的砂岩层);实际上完全没有喷出岩(辉绿玢岩岩脉除外);控矿构造是被断裂所复杂化的背斜褶皱;矿体为趋于产在褶曲穹部的钟状体、与褶皱弯曲部位破碎带有关的网脉状体以及柱状体、透镜体和细脉等;成矿溶 Most of the world’s mercury reserves and mercury production come from quartz-dickite-type mercury deposits. Quartz-dickite-type mercury deposits are characterized by the fact that the surrounding rock is often a thick terrigenous sedimentary rock (in the form of a composite interbedded layer or a homogeneous sandstone bed); virtually no extritiated rock (except for the diabase dyke veins) ; The ore-controlling structure is an anticline fold complicated by faults; the ore body is a bell-shaped body that tends to be produced in the foramen magnum, a reticulate body that is related to the crushed zone of the folded bend, and a columnar body, a lens body, and a thin Pulse, etc .; mineralization