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美国矿床地质学家爱孟司在1937年对于个别矿床矿区,以及火成岩岩基和岩钟作过关于热液矿床带状分布的研究。根据他的研究从火成岩体向外,比较高温的造矿矿物成分渐渐向比较低温的矿物过渡。同样在矿脉中,由浅到深矿物也是由低温渐向高温方向过渡。爱孟司把这个此较复杂的成矿情况简单地分成十六个带,由地表到地下为:(1)无矿带,(2)汞带,(3)锑带,(4)金银带,(5)无矿带,(6)银带,(7)铅带,(8)锌带,(9)铜带,(10)铜带,(11)金带,(12)鉮带,(13)铋带,(14)锑带,(15)锡带,(16)无矿带,(石英)。爱孟司分为这十六带主要是根据地热分带如下:
In 1937, Amengsi, a US deposit geologist, studied the banded distribution of hydrothermal deposits for individual ore deposits and for igneous and rock bells. According to his research, from the igneous rock body, the relatively high temperature ore-forming mineral components gradually transition to the relatively low-temperature minerals. Also in the veins, from shallow to deep mineral is also a gradual transition from low to high temperature direction. Monsanto divides this more complex metallogeny into sixteen zones from the surface to the ground: (1) mineralized zone, (2) mercury zone, (3) antimony zone, (4) silver zone (6) Silver Belt (7) Lead Belt (8) Zinc Belt (9) Copper Belt (10) Copper Belt (11) Gold Belt (12) (13) bismuth, (14) antimony, (15) tin, (16) non-ore belt, and (quartz). Love Meng Division divided for the sixteen belt is mainly based on geothermal zoning as follows: