Growth of a salt diapir in an anticline - A record from the Cenozoic halokinetic sequences in the Zagros Fold and Thrust Belt, Iran
Author:
Funder
Charles University
Grantová Agentura, Univerzita Karlova
Grantová Agentura České Republiky
Publisher
Elsevier BV
Subject
Geology
Reference86 articles.
1. Convergence history across Zagros (Iran): constraints from collisional and earlier deformation;Agard;Int. J. Earth Sci.,2005
2. Style and timing of salt movement in the Persian Gulf basin, offshore Iran: Insights from halokinetic sequences adjacent to the Tonb-e-Bozorg salt diapir;Asl;J. Struct. Geol.,2019
3. Effect of spatial distribution of Hormuz salt on deformation style in the Zagros fold and thrust belt: an analogue modelling approach;Bahroudi;J. Geol. Soc.,2003
4. Tectono-sedimentary framework of the Gachsaran Formation in the Zagros foreland basin;Bahroudi;Mar. Petrol. Geol.,2004
5. Towards a paleogeography and tectonic evolution of Iran: reply;Berberian;Can. J. Earth Sci.,1981
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