Writers : Rotner,A.
Refference : Geoscinces Scientific Quarterly Journal,No.12
Publishing Year : 1373

Abstract :

Results obtained by Iranian and European geoscientists in the critical area to the north-east of the North Iran Suture east of Mashhad are described and discussed. A slightly metamorphosed ophiolite belt outcropping as the south easterly continuation of the previously known ophiolites of Mashhad along the north eastern perimeter of the Fariman_ Torbat_e_Jam depression, proved to be either the remnant of a Permiar ocean floor or more likely the remnant of a narrow ocean trough. There is as yet no proof of a Triassic age for this ophiolitic belt. To the north of this ophiolitic belt an epicontinental Triassic sequence is exposed at the southern edge of Laurasia in the erosional Window of Aghdarband. This is the result of intermitteni sedimentation in a pull- apart basin along sinistral strike- slip faults. The Triassic of Aghdarband has much ir common with other deposits of the Triassic Tethys; however, it shows a few unique features, e.g. the Earls Anisian Nicomedites fauna of a palaeobiogeographic North Tethyan Subprovince, or volcanogenic sedimentation during the late Anisian and the entire Ladinian
Permian ophiolites outcropping at the south- west corner of the Aghdarband erosional Window� are� transgressively overlain by basal conglomerats of this Triassic sequence. Hence the existence of a Triassic ocean south of Laurasia is very unlikely. This is an agreement with paleomagnetic data which suggest that the Central Iranian microcontinent was in direct contact with Laurasia during Triassic times. Thes palaeomagnetic data also suggest a clockwise rotation of the Central East Iran microplate during Triassic times (contrary to the anticlockwise rotation of this microplate in post- Triassic times). The sinistral strike- slid faulting and compression from the south- west which controls the structure of the Triassic may be derivative sequels to this clockwise rotation. All eo_ Cimmerian deformations of the Triassic rocks (e. g. folding, thrust faulting, strike- slip faulting) had stopped by Rhaetian times.

Subject List : age