白云石大理岩

吉林荒沟山铅锌矿床赋存于中元古界老岭群珍珠门组白云石大理岩中，层控特征明显。

The Huanggoushan Pb Zn deposit , occurring in the dolomite marble of Mesoproterozoic Zhenzhumen formation , is obviously controlled by strata .

主要容矿岩石为金云母石英白云石大理岩和矿化角砾岩，其它岩石次之。

Ore metals are hosted mainly in phlogopite quartz dolomitic marble and breccias .

之所以不将这些类型列在不同的标题下面，是因为它们全都具有白云石大理岩类型的特征。

These aren 't listed under different headings because they all share the characteristic of being a type of dolomitic marble .

新生代以来，山体上升，在构造节理的主导下，配合物理风化及部分地表流水作用，逐步发展成为白云石大理岩构造峰林。

Since the Cenozoic this mountain has risen and owing to structural jointing , combined with mechanical weathering and surface water erosion , it has gradually become a dolomitic marble " peak forest " .