厄尔士山脉变质沉积物的地球化学识别和对比表明在变质逆冲单元中重现了早古生代变质沉积层序。
Geochemical discrimination and correlation from the metasediments of the Erzgebirge suggest repetition of an early Palaeozoic metasedimentary sequence in metamorphic thrust units.
在造山的过程中，一些非常古老的沉积物已被转化为火成岩和变质岩，已经无法辨认了。
Some very ancient sediments were no longer recognizable, having been converted to igneous and metamorphic rocks in the course of mountain building.
古流向和物源恢复结果证明，盆地沉积物主体来自北部和西部变质岩基底。
Sediments were demonstrated to have mainly come from metamorphic basements on the north and west.
古流向和物源恢复结果证明，盆地沉积物主体来自北部和西部变质岩基底。
Sediments were demonstrated to have mainly come from metamorphic basements on the north and west.
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