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تکتونیک و تکامل چینه ای زاگرس و مکران در مزوزوئیک و سنوزوئیک

Tectonic and Stratigraphic Evolution of Zagros and Makran during the Mesozoic-Cenozoic
(Geological Society Special Publication 330)

Tectonic and Stratigraphic Evolution of Zagros and Makran during the Mesozoic-Cenozoic

By P. Leturmy, C. Robin, 2010

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    * Publisher:   Geological Society of London
    * Number Of Pages:   376
    * Publication Date:   2010-03-15
    * ISBN-10 / ASIN:   1862392935
    * ISBN-13 / EAN:   9781862392939

Product Description:
The Zagros fold-thrust belt (ZFTB) extends from Turkey to the Hormuz Strait, resulting from the collision of the Arabian and Eurasian plates during Cenozoic times, and separates the Arabian platform from the large plateaux of central Iran. To the east a pronounced syntaxis marks the transition between the Zagros collision belt and the Makran accretionary wedge. In the ZFTB, the Proterozoic to Recent stratigraphic succession pile is involved in huge folds, and offers the opportunity to study the stratigraphic and tectonic evolution of the Palaeo-Tethyan margin.
Few recent data were widely available on the southern Tethys margin preserved in the Zagros Mountains. The Middle East Basins Evolution (MEBE) program was an excellent opportunity to go back to the field and to collect new data to better constrain the evolution of this margin. In this volume the structure of the Zagros Mountains is explored through different scales and using different methodologies.