叠生 meaning in Chinese

storey

Therefore , two mineralization periods ore divided , which can be called as hot - water sedimention period and telescoping period . stratiform green - rock is the direct country rock of bedded orebodies . the rock was called as skam in the past
作者将本区成矿过程划分出两个成矿期，即早志留世热水沉积成矿期和燕山期岩浆?热液叠生改造成矿期。
There are typical laminated structure , soft sedimentary - slipping deformed structure , syngenetic brecciated structure in the ore which are the mirror of syngenetic sedimentation . the other type of ore has the charactristic of epigenetic mineralization , which is called as telescoped ore . the ore occurs in vein , pocket , lensoid and bedd
矿石中发育典型的纹层状构造、软沉积滑动变形构造、同生角砾构造等反映同生沉积特征的矿石构造；另一类矿石具有明显的后生成矿特点，称之为叠生改造型矿石，矿石产于脉状、囊状、透镜状及似层状矿体中，与燕山期岩浆岩及断裂裂隙构造关系密切。