Revised version of the Cenozoic Collision along the Zagros Orogen, Insights from Cr-spinel and Sandstone Modal Analyses-Reference-Cited by-同舟云学术

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Revised version of the Cenozoic Collision along the Zagros Orogen, Insights from Cr-spinel and Sandstone Modal Analyses

Published:2017-09-07 Issue:1 Volume:7 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Gholami Zadeh Parisa,Adabi Mohammad Hossein,Hisada Ken-ichiro,Hosseini-Barzi Mahboubeh,Sadeghi Abbas,Ghassemi Mohammad Reza

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/s41598-017-11042-1.pdf

Reference65 articles.

1. Decelles, P. G. & Giles, K. A. Foreland basin systems. Basin Res. 2, 105–123 (1996).

2. Garzanti, E., Doglioni, C., Vezzoli, G. & Ando, S. Orogenic Belts and Orogenic Sediment Provenance. J. Geol. 115, 315–334 (2007).

3. Garzanti, E. From static to dynamicprovenance analysis-Sedimentary petrology upgraded. Sediment. Geol. 336, 3–13 (2015).

4. Dickinson, W. In1terpreting provenance relations from detrital modes of sandstones. In Zuifa, G. G. (ed.) Provenance of arenites: Dordrecht, Reidel 333–361 (1985).

5. Arai, S. Chemistry of chromian spinel in volcanic rocks as a potential guide to magma chemistry. Mineral. Mag. 56, 84–173 (1992).

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