2018
DOI: 10.1071/eg16057
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Investigating subsurface structures of Gachsaran oil field in Iran using 2D inversion of magnetotelluric data

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Cited by 7 publications
(4 citation statements)
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“…The Asmari reservoir thickness is about 500 m in the west and 250 m in the east. It consists mainly of limestone and dolomite with minor siliciclastic intercalations [32]. The stratigraphic chart of Cretaceous-Tertiary sequences in Dezful Embayment illustrating the Oligo-Miocene Asmari Formation is shown in Figure 1.…”
Section: Geological Settingmentioning
confidence: 99%
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“…The Asmari reservoir thickness is about 500 m in the west and 250 m in the east. It consists mainly of limestone and dolomite with minor siliciclastic intercalations [32]. The stratigraphic chart of Cretaceous-Tertiary sequences in Dezful Embayment illustrating the Oligo-Miocene Asmari Formation is shown in Figure 1.…”
Section: Geological Settingmentioning
confidence: 99%
“…The Gaussian random function simulation (GRFS) algorithm generated a mud loss map for the Asmari Formation (Figure 6). It should be noted that the source of "complete losses" could be either fractures or localized cavities, and they tend to occur in geological formations that have pre-existing fractures [32,34].…”
Section: Mud Loss Mapmentioning
confidence: 99%
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“…The MT method is one of various the geophysical methods that can be applied to delineate subsurface structures [13]. Delineation is a geologycal methods to identify the geological structures [14].…”
Section: Introductionmentioning
confidence: 99%