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(英文)  

Evaluation of Tectonic Setting of the Proto-tethyan Remnants in Central Iran:A Geochemical Study

作　　者：Monireh POSHTKOOHI 

机构地区：[1]Geological Survey of Iran

出　　处：《地球学报》2012年第S1期55-57,共3页Acta Geoscientica Sinica

摘　　要：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).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).

关 键 词：GNEISSES ultra-mafic ROCKS Central Iran Saghand Posht-e-Badam 

分 类 号：P5[天文地球—地质学]