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- W1975401567 abstract "Asmari anticline is a NW-SE fold in the Dezful Embayment sub-basin of Zagros. Fars group (Late Moicene-Quaternary) is cropping out in the cores of anticlines in this area, but Pabdeh and Asmari formations (Oligocene-Early Miocene) have cropped out only in Asmari anticline in the Dezful Embayment. Therefore, it has formed a unique exposure for above formations. In order to this situation, folding mechanism of Asmari anticline has investigated in this research. According to our results, Asmari anticline has two mechanisms: flexural-slip in post-Cretaceous sequences (Khami-Quaternary) and fault-bend folding in pre-Cretaceous sequences. So, there is a hybrid folding mechanism that has introduced for the first time in this paper." @default.
- W1975401567 created "2016-06-24" @default.
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- W1975401567 date "2015-01-01" @default.
- W1975401567 modified "2023-09-30" @default.
- W1975401567 title "Folding Mechanism in the Asmari Anticline, Zagros, Iran" @default.
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- W1975401567 doi "https://doi.org/10.4236/ojg.2015.54018" @default.
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