2020
DOI: 10.1016/j.marpetgeo.2020.104301
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How a mud-dominated ramp changed to a carbonate–clastic oil reservoir: Sea-level fluctuations in cretaceous of the central Persian Gulf

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Cited by 15 publications
(2 citation statements)
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“…In the Zagros, three unconformities have been identified in middle Cretaceous deposits [40,53,57,58]. The lower unconformity (Mid-Cenomanian) has been observed at the base of this interval in the southern part of the Fars area and Bandar Abbas.…”
Section: Cenomanian Palaeoheightmentioning
confidence: 97%
See 1 more Smart Citation
“…In the Zagros, three unconformities have been identified in middle Cretaceous deposits [40,53,57,58]. The lower unconformity (Mid-Cenomanian) has been observed at the base of this interval in the southern part of the Fars area and Bandar Abbas.…”
Section: Cenomanian Palaeoheightmentioning
confidence: 97%
“…So far, many studies have been carried out in the Dezful Embayment, Izeh, Fars, and the Persian Gulf area (Figure 1). These studies have shown a simple ramp or shelf profile for Sarvak depositional environment [40][41][42][43]. In the Lurestan Zone, the Late Albian-mid-Turonian, Sarvak carbonate factories were dominated by deeper platform environments and some special climatic conditions that led to different facies characteristics compared with other parts of the Zagros area [26] (Figures 1 and 2).…”
Section: Geological Settingmentioning
confidence: 99%