Deducing the Lateral Growth of Anticlines using Drainage Analysis and Geomorphological Features.

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Title: Deducing the Lateral Growth of Anticlines using Drainage Analysis and Geomorphological Features.
Authors: Sissakian, V. K.1 (AUTHOR), Elias, Z.2 (AUTHOR), Al-Ansari, N.3 (AUTHOR) nadhir.alansari@ltu.se
Source: Geotectonics. Jan2019, Vol. 53 Issue 1, p140-154. 15p.
Subject Terms: *Anticlines, *Alluvium, *Alluvial streams, *Alluvial fans, *Drainage, *Neotectonics
Geographic Terms: Iraq
Abstract: The Low Folded Zone in Iraq is an active tectonic area witnessing different evidences for Neotectonic activities, among them are the lateral growth of Jambour, Pulkhana, and Qumar anticlines which are part of anticlinal series in the Low Folded Zone and Zagros Fold–Thrust Belt. The exposed rocks are of Middle Miocene – Pleistocene age overlain unconformably by different types of Quaternary sediments which show different indications for lateral growth. Three anticlines are dissected by tens of different size valleys crossing the anticlines forming water gaps and wind gaps which are good indication for the anticlines lateral growth. We studied the lateral growth of three anticlines using different means of qualitative analysis of satellite imagery and digital topography and ArcGIS technique. The anticlines lateral growth was mainly manifested by the drainage system and patterns which exhibited strange courses during dissecting the three studied anticlines. Moreover, the main streams deposited alluvial fans during Early Pleistocene and even Early Holocene which were also influenced by both lateral and vertical anticlines growth. Their abnormal shapes, abandoned fans and streams were among indications. We measured different geomorphological indices which indicated tectonic activity of the study area. [ABSTRACT FROM AUTHOR]
Database: Energy & Power Source
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  Label: Title
  Group: Ti
  Data: Deducing the Lateral Growth of Anticlines using Drainage Analysis and Geomorphological Features.
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  Data: <searchLink fieldCode="AR" term="%22Sissakian%2C+V%2E+K%2E%22">Sissakian, V. K.</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Elias%2C+Z%2E%22">Elias, Z.</searchLink><relatesTo>2</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Al-Ansari%2C+N%2E%22">Al-Ansari, N.</searchLink><relatesTo>3</relatesTo> (AUTHOR)<i> nadhir.alansari@ltu.se</i>
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  Data: <searchLink fieldCode="JN" term="%22Geotectonics%22">Geotectonics</searchLink>. Jan2019, Vol. 53 Issue 1, p140-154. 15p.
– Name: Subject
  Label: Subject Terms
  Group: Su
  Data: *<searchLink fieldCode="DE" term="%22Anticlines%22">Anticlines</searchLink><br />*<searchLink fieldCode="DE" term="%22Alluvium%22">Alluvium</searchLink><br />*<searchLink fieldCode="DE" term="%22Alluvial+streams%22">Alluvial streams</searchLink><br />*<searchLink fieldCode="DE" term="%22Alluvial+fans%22">Alluvial fans</searchLink><br />*<searchLink fieldCode="DE" term="%22Drainage%22">Drainage</searchLink><br />*<searchLink fieldCode="DE" term="%22Neotectonics%22">Neotectonics</searchLink>
– Name: SubjectGeographic
  Label: Geographic Terms
  Group: Su
  Data: <searchLink fieldCode="DE" term="%22Iraq%22">Iraq</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: The Low Folded Zone in Iraq is an active tectonic area witnessing different evidences for Neotectonic activities, among them are the lateral growth of Jambour, Pulkhana, and Qumar anticlines which are part of anticlinal series in the Low Folded Zone and Zagros Fold–Thrust Belt. The exposed rocks are of Middle Miocene – Pleistocene age overlain unconformably by different types of Quaternary sediments which show different indications for lateral growth. Three anticlines are dissected by tens of different size valleys crossing the anticlines forming water gaps and wind gaps which are good indication for the anticlines lateral growth. We studied the lateral growth of three anticlines using different means of qualitative analysis of satellite imagery and digital topography and ArcGIS technique. The anticlines lateral growth was mainly manifested by the drainage system and patterns which exhibited strange courses during dissecting the three studied anticlines. Moreover, the main streams deposited alluvial fans during Early Pleistocene and even Early Holocene which were also influenced by both lateral and vertical anticlines growth. Their abnormal shapes, abandoned fans and streams were among indications. We measured different geomorphological indices which indicated tectonic activity of the study area. [ABSTRACT FROM AUTHOR]
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RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1134/S0016852119010072
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 15
        StartPage: 140
    Subjects:
      – SubjectFull: Anticlines
        Type: general
      – SubjectFull: Alluvium
        Type: general
      – SubjectFull: Alluvial streams
        Type: general
      – SubjectFull: Alluvial fans
        Type: general
      – SubjectFull: Drainage
        Type: general
      – SubjectFull: Neotectonics
        Type: general
      – SubjectFull: Iraq
        Type: general
    Titles:
      – TitleFull: Deducing the Lateral Growth of Anticlines using Drainage Analysis and Geomorphological Features.
        Type: main
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          Name:
            NameFull: Sissakian, V. K.
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          Name:
            NameFull: Elias, Z.
      – PersonEntity:
          Name:
            NameFull: Al-Ansari, N.
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          Dates:
            – D: 01
              M: 01
              Text: Jan2019
              Type: published
              Y: 2019
          Identifiers:
            – Type: issn-print
              Value: 00168521
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            – Type: volume
              Value: 53
            – Type: issue
              Value: 1
          Titles:
            – TitleFull: Geotectonics
              Type: main
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