热水沉积成矿与正常沉积矿床在矿质来源和成矿机制上有很大的差异，反映在岩矿石结构构造上也有明显的差异性。
There is a great difference not only between thermal water sedimentary deposit and sedimentary deposit from original material of ore and metallogenesis, but also ore texture of them.
矿石、矽卡岩具有典型的岩浆矿床的结构构造。
Finally, skarn and ores show typical textures and structures of magmatic deposits.
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