高分翻译啦！@@

来源：百度知道 编辑：UC知道 时间：2024/05/10 08:40:27
Genetically, the mudstone is thought to have acted as an impermeable cap-rock to the mineralising fluids. Volcanic rocks interbedded with the limestone are generally barren, but occasionally allow the development of sub-horizontal deposits of "flats". There is a broad, cross-country, mineral zonation of fluorspar-barytes-lead veins, with fluorspar being the dominant mineral in the east, and barytes+calcite becoming progressively more abundant westward. However, the zones are poorly defined and there is considerable overlap.

这是化学方面的，关于萤石，千万别用google翻啊，我一眼就看出来的哦@！！

一般的看法是，泥岩为矿化中的岩浆形成了一层不渗水的岩盖。同石灰石成互层的火山岩通常都不含矿，然而有时也会促成次水平面上“板状矿”的积聚。此处有一条广阔的，跨国界的以萤石和方解石为主的矿物分带；其东部以萤石为主，往西部推进过程中，重晶石和方解石的含量不断增高。不过，区域上的分布并不明确，并且各区域间有相当的重叠。

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呼。。 头大 = =

基因，泥岩被认为是起到了一个不透水的上限岩向mineralising流体。火山岩互与石灰石普遍荒芜，但偶尔让发展小组的横向存款“单位” 。有广泛的，跨国家，矿产区划萤石-重晶石铅静脉，与萤石作为优势矿种在东部地区，和重晶石+方解石逐渐更丰厚的西移。然而，区不善的界定有相当多的重叠。

Genetically, the mudstone is thought to have acted as an impermeable cap-rock to the mineralising fluids. Volcanic rocks interbedded with the limestone are generally barren, but occasionally allow the development of sub-horizontal deposits of "flats". There is a broad, cross-country, mineral zonation of fluorspar-barytes-lead veins, with fluorspar being the dominant mineral in the east, and barytes+calcite becoming progressively more abundant westward. However, the zones are poorly defined and there is considerable overlap.

基因，泥岩被认为是起到了一个不透水的上限岩向mineralising流体。火山岩互与石灰石普遍荒芜，但偶尔让发展小组的横向存款“单位” 。有广泛的，跨国家，矿产区划萤石-重晶石铅静脉，