Scientific Quarterly Journal of Geosciences

Scientific Quarterly Journal of Geosciences

Southern borderland of Triassic Laurasia in north-east Iran

Document Type : Original Research Paper

Author
A. W. Ruttner
Geologische Bundesanstalt, Rasumovskygasse 23, PO Box 127, A- 1031 Wien, Austria
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 Permian 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 intermittent sedimentation in a pull- apart basin along sinistral strike-slip faults. The Triassic of Aghdarband has much in common with other deposits of the Triassic Tethys; however, it shows a few unique features, e.g., the Early 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 conglomerates 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. These 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-slip 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.
Subjects
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Scientific Quarterly Journal of Geosciences
Volume 3, Issue 12
Summer 1994, Vol. 3, No. 12
Autumn 1994
Pages 64-79