Rezvaneh Jamali Ashtiani- Doctor of Philosophy
- PostDoc Position at Heidelberg University
Rezvaneh Jamali Ashtiani
- Doctor of Philosophy
- PostDoc Position at Heidelberg University
About
9
Publications
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15
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Introduction
Skills and Expertise
Current institution
Education
September 2011 - February 2017
Publications
Publications (9)
Late Neoproterozoic-Early Cambrian calc-alkaline granitoids are ubiquitous in the continental basement of Iran and indicate formation within a Cadomian arc system at the northern margin of Gondwana. A basement complex comprising mainly mica schist, paragneisses, and metagranite along with metabasite and rare pegmatite is exposed in the Zayanderud r...
The Zayandehrud metamorphic complex consists of various schists, amphibolites, marbles and minor eclogites associated with intruding mylonitized gneissic granitoids, exposed over an area exceeding 800 km2 in in Esfahan and Shahrekord quadrangles in Central Sanandaj-Sirjan belt. Lack of comprehensive data on the age and chemical compositions of thes...
The Zayanderud metamorphic complex has received two different age attributes of Precambrian and Jurassic in the Najafabad and Chadegan maps, respectively. This disagreement has made these two maps to be the most incompatible adjacent maps. The metamorphic complex is nonconformably covered by fossiliferous Permian limestones suggesting a Pre-Permian...
The Sanandaj-Sirjan zone is a NW-SE-trending orogenic belt immediately north of the Zagros suture, which represents the former position of the Neotethys Ocean. The zone includes a Pan-African basement similar to the various terranes to the north in Central Iran. The crystalline basement is nonconformably overlain by the Paleozoic-Triassic platform...
The existing reconstructions of Gondwana suffer from uncertainties about its northern extensions due to the episodic separation of rifted blocks and their accretion to the Alpine-Himalayan orogenic belt during the Phanero-zoic times. Using new data and the published information we synthesize an Ediacaran (630-542 Ma) thickened continental belt whos...
The existing reconstructions of Gondwana suffer from uncertainties about its northern extensions due to the episodic separation of rifted blocks and their accretion to the Alpine-Himalayan orogenic belt during the Phanero-zoic times. Using new data and the published information we synthesize an Ediacaran (630-542 Ma) thickened continental belt whos...
