伊朗中部原特提斯残余的评价及构造环境:据地球化学研究     

Monireh POSHTKOOHI 《地球学报》2012,33(S1):55-57

The Iranian plateau comprises several continental blocks, which are clearly bounded by major faults. The sedimentary, stratigraphic, magmatic and metamorphic features of these blocks vary from one to the other. The continental crust of subject area in Central Iran was investigated in the past by several authors. It was concluded that this zone was metamorphosed, intruded by granites and faulted during late Precambrian Pan-African Orogeny (Ramezani and Tucker, 2003).  相似文献