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<!DOCTYPE ArticleSet PUBLIC "-//NLM//DTD PubMed 2.7//EN" "https://dtd.nlm.nih.gov/ncbi/pubmed/in/PubMed.dtd">
<ArticleSet>
<Article>
<Journal>
<PublisherName>OICC Press</PublisherName>
<JournalTitle>Iranian Journal of Earth Sciences</JournalTitle>
<Issn>2228-785X</Issn>
<Volume>7</Volume>
<Issue>2</Issue>
<PubDate PubStatus="epublish">
<Year>2015</Year>
<Month>03</Month>
<Day>21</Day>
</PubDate>
</Journal>
<ArticleTitle>Structural overview of the Halab-Gheydar area, southwest of Zanjan, NW Iran</ArticleTitle>
<VernacularTitle></VernacularTitle>
<FirstPage>50</FirstPage>
<LastPage>58</LastPage>
<ELocationID EIdType="doi"></ELocationID>
<Language>EN</Language>
<AuthorList>
<Author>
<FirstName>Rasoul</FirstName>
<LastName>Esmaeili</LastName>
<Affiliation>Department of Earth Sciences, College of Sciences, Shiraz University, Shiraz, Iran.</Affiliation>
<Identifier Source="ORCID"></Identifier>
</Author>
<Author>
<FirstName>Ali</FirstName>
<LastName>Faghih</LastName>
<Affiliation>Department of Earth Sciences, College of Sciences, Shiraz University, Shiraz, Iran.</Affiliation>
<Identifier Source="ORCID"></Identifier>
</Author>
<Author>
<FirstName>Mahnaz</FirstName>
<LastName>Rezaian</LastName>
<Affiliation>Department of Earth Sciences, Faculty of Sciences, Institute for Advanced Studies in Basic Sciences, Zanjan, Iran.</Affiliation>
<Identifier Source="ORCID"></Identifier>
</Author>
<Author>
<FirstName>Mohammad</FirstName>
<LastName>Ebrahimi</LastName>
<Affiliation>Department of Geology, Faculty of Sciences, University of Zanjan, Zanjan, Iran.</Affiliation>
<Identifier Source="ORCID"></Identifier>
</Author>
</AuthorList>
<PublicationType>Journal Article</PublicationType>
<History>
<PubDate PubStatus="received">
<Year>2015</Year>
<Month>03</Month>
<Day>21</Day>
</PubDate>
</History>
<Abstract>Understanding the folding style of a fold-thrust belt is crucial to understand the nature and structural history of structures that may trap natural resources within the belt. In this research, the geometry and mechanism of a number of fault-related folds has been investigated based on field data and satellite image interpretations. The main study areas are: the Sohrevard and Ushtaniyan anticlines, Bahman and Halab synclines, and Gharahdagh, Halab, and Gheydar thrust faults, which have a NW-SE direction. These thrust faults control the morphology and structural framework of the Halab-Gheydar area. Geomorphic features of the folds suggest that they are fault-related folds. The structural style of the faults and associated folds indicate that these faults were reactivated during the Alborz deformation event.</Abstract>
</Article>
</ArticleSet>