Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Solid Earth Discuss., 7, 2347–2379, 2015 www.solid-earth-discuss.net/7/2347/2015/ doi:10.5194/sed-7-2347-2015 SED © Author(s) 2015. CC Attribution 3.0 License. 7, 2347–2379, 2015 This discussion paper is/has been under review for the journal Solid Earth (SE). Folding pattern in the Please refer to the corresponding final paper in SE if available. Fars province Folding pattern in the Fars province, Z. Maleki et al. Zagros folded belt: case study on the Title Page Karbasi and Khaftar anticlines, interior Abstract Introduction Fars, Iran Conclusions References Tables Figures Z. Maleki, M. Arian, and A. Solgi Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran J I Received: 25 July 2015 – Accepted: 28 July 2015 – Published: 17 August 2015 J I Correspondence to: M. Arian (
[email protected]) Back Close Published by Copernicus Publications on behalf of the European Geosciences Union. Full Screen / Esc Printer-friendly Version Interactive Discussion 2347 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract SED The anticlines in Fars region, which are located in Zagros fold-thrust belt, are valu- able because they possess several hydrocarbons and this area is easily recognized by 7, 2347–2379, 2015 the NW–SE trending parallel anticlines that verge to the SW. According to the geolog- 5 ical classification, the study area is located in Interior Fars region. Due to increasing Folding pattern in the complication of structural geometry in Fars region and necessity to explore activities Fars province for deeper horizons especially the Paleozoic ones, the analysis of fold style elements, which is known as one of the main parts in structural studies, seems necessary.