The sediments of Dagh-e-Sorkh playa, Ardestan, central Iran.

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Title: The sediments of Dagh-e-Sorkh playa, Ardestan, central Iran.
Authors: Pazand, Kaveh1 kaveh.pazand@gmail.com, Behzadinasab, Ali2, Ghaderi, Mohammad Reza3, Reza Rezvanianzadeh, Mohammad4
Source: Carbonates & Evaporites. Mar2018, Vol. 33 Issue 1, p55-64. 10p.
Subjects: Sediment analysis, Calcite analysis, Ergs (Landforms), Facies, Stratigraphic geology
Abstract: The Dagh-e-Sorkh playa is a closed basin in central Iran. The sediments of this playa were studied for sedimentologic and geomorphologic characteristics, the interaction of sedimentation mode of a terminal ephemeral fluvial-fan system and adjacent lacustrine/aeolian sediments in the area. Evaporite minerals including calcite, gypsum and halite were the most dominant minerals. The two main types (pediment and playa type) and few subtypes facies were identified. Based on the surface and subsurface study, the area was zoned and sedimentary- stratigraphic column for each zone was interpreted and six zones were characterized. These data clearly show that different conditions are dominant for the deposition of sediment and vertical changes in sedimentary facies around the area. [ABSTRACT FROM AUTHOR]
Copyright of Carbonates & Evaporites is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: <searchLink fieldCode="DE" term="%22Sediment+analysis%22">Sediment analysis</searchLink><br /><searchLink fieldCode="DE" term="%22Calcite+analysis%22">Calcite analysis</searchLink><br /><searchLink fieldCode="DE" term="%22Ergs+%28Landforms%29%22">Ergs (Landforms)</searchLink><br /><searchLink fieldCode="DE" term="%22Facies%22">Facies</searchLink><br /><searchLink fieldCode="DE" term="%22Stratigraphic+geology%22">Stratigraphic geology</searchLink>
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  Data: The Dagh-e-Sorkh playa is a closed basin in central Iran. The sediments of this playa were studied for sedimentologic and geomorphologic characteristics, the interaction of sedimentation mode of a terminal ephemeral fluvial-fan system and adjacent lacustrine/aeolian sediments in the area. Evaporite minerals including calcite, gypsum and halite were the most dominant minerals. The two main types (pediment and playa type) and few subtypes facies were identified. Based on the surface and subsurface study, the area was zoned and sedimentary- stratigraphic column for each zone was interpreted and six zones were characterized. These data clearly show that different conditions are dominant for the deposition of sediment and vertical changes in sedimentary facies around the area. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Carbonates & Evaporites is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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      – SubjectFull: Calcite analysis
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      – SubjectFull: Ergs (Landforms)
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      – SubjectFull: Facies
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              Text: Mar2018
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