List of Articles سازند سروک

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  1 - Biostratigraphy of the Sarvak and Ilam formations in Abteymoor Oil Field (Wells no. 1 and 14)
  Reza Omidi Mahmoud Jalali Mahboubeh Hooseni-barzi Narges Akbari
  In order to carry out biostratigraphic studies on Sarvak and Ilam formations, two subsurface sections in wells 1 and 14 of Abteymoor oil field were selected in the south of Dezful embayment. Sarvak Formation in well #1 has 812.98 (m) thickness and in Well No. 14 only 23 More

  In order to carry out biostratigraphic studies on Sarvak and Ilam formations, two subsurface sections in wells 1 and 14 of Abteymoor oil field were selected in the south of Dezful embayment. Sarvak Formation in well #1 has 812.98 (m) thickness and in Well No. 14 only 234 (m) of this formation was drilled, in terms of lithology the Sarvak Formation consists mainly of limestone with dolomitic and clay interbeds. Its lower boundary in Well # 1 with Kazhdumi Formation is conformable but in Well # 14 it is unclear. The upper boundary is disconformable with Ilam Formation in both wells. Ilam Formation in two wells of 1 and 14, has thickness of 151.72 and 136 (m) respectively and in terms of lithology, it consists of limestone and shaley, marly and dolomitic limestone interbeds. The upper boundary of Ilam Formation with Gurpi Formation is conformable with sharp changes in lithology. In biostratigraphy studies 71 species were detected which belong to 57 genera of foraminifera, a biozones (biozone 1) in Ilam Formation and three biozones (biozones 2, 3 and 4) were identified in Sarvak Formation. They include: 1- Rotorbinella-Pararotalia Assemblage Zone 2- Nezzazatinella picardi-Dicyclina schlumbergeri Assemblage Zone 3- Rotorbinella mesogeensis Total Range Zone 4- Nezzazata-alveolinid Assemblage Zone Based on identified biozones, age of Sarvak Formation is considered as Cenomanian- Turonian and the age of Ilam Formation is Designated as Santonian- Campanian? Manuscript profile
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  2 - Three-dimensional geological modeling in two zones of eastern side of Ahvaz oil field
  Razeyeh . Doosti Irani Maryam Payrovi Mohammad .rahim karimi Mehdi . Doosti Irani
  The Ahvaz field is one of the most important oil fields in the Zagros Basin which is located in the Dezful Embayment. The trend of Ahvaz oil field is northwest- southeast parallel to the Zagros mountains. The purpose of this study is the geological 3D simulation (petrop More

  The Ahvaz field is one of the most important oil fields in the Zagros Basin which is located in the Dezful Embayment. The trend of Ahvaz oil field is northwest- southeast parallel to the Zagros mountains. The purpose of this study is the geological 3D simulation (petrophysical) for the zone one and two in the eastern part of the Ahvaz oil field. In this investigation, porosity modeling, water saturation and shale volume by using sequential Gaussian Simulation (SGS) was performed. At first, well logs, cores, well’s coordination, top and thickness of formations of the zone three of Ilam Formation and zone one of Sarvak Formation were collected. These information related to 25 wells in the eastern part of the Ahvaz oil field was used for the 3D modeling of the reservoir by using Petrel software. For the recognition of spatial correlation, variograms based on water saturation and permeability and three dimensional model of the petrophysical parameters and net to gross ratio (NTG) were drawn. Manuscript profile
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  3 - The application of Normalized Cumulative Gamma Deviation Log (NCGDL) in sequence stratigraphic analysis and correlation, a case study from the Sarvak Formation, Abadan Plain, SW, Iran
  A. Asaadi A. Imandoust J.  Honarmand ایرج عبدالهی فرد O.R. Salmian
  Identification of key sequence stratigraphic surfaces is an essential task in geological evaluation of hydrocarbon reservoirs. The Sarvak Formation with Late Albian-Early Turonian age constitute the important reservoir unit in the Abadan Plain region, SW Iran. This stud More

  Identification of key sequence stratigraphic surfaces is an essential task in geological evaluation of hydrocarbon reservoirs. The Sarvak Formation with Late Albian-Early Turonian age constitute the important reservoir unit in the Abadan Plain region, SW Iran. This study investigates the application of Normalized Cumulative Gamma Deviation Log (NCGDC) to discriminate and correlate key sequence stratigraphic surfaces in six wells in a giant oil field in the Abadan Plain. To achieve this goal, identified key stratigraphic surfaces from core and thin sections were compared with interpretation of NCGDC method. From sequence stratigraphic point of view and based on the results from geological studies, the Sarvak Formation has been sub-divided into four third-order sequences which are described and interpreted. Two main disconformity surfaces, considered as sequence boundaries, are characterized by features of karstification, dissolution-collapse brecciation, and development of paleosol horizons. Generally, positive surfaces correspond to maximum flooding surfaces and negative surfaces occur at sequence boundary. Comparison of the results shows that, the identified sequence by NCGDC method can be effectively used for discrimination and correlation of sequences in different carbonate and siliciclastic reservoirs in the field scale. Manuscript profile
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  4 - Investigating the reservoir quality of Sarvk formation using multi-resolution graph-based and comparing it with petrographic data in an oilfield of Dezful Embayment
  Seyedeh Akram  Jooybari Payman Rezaee Majid Mehdipour
  Sarvak Formation is one of the important carbonate reservoirs in Dezful Embayment. In order to evaluate the reservoir quality of this formation in one of the Dezful Embayment fields, multi-resolution graph-based method was used and compared with petrographic findings. T More

  Sarvak Formation is one of the important carbonate reservoirs in Dezful Embayment. In order to evaluate the reservoir quality of this formation in one of the Dezful Embayment fields, multi-resolution graph-based method was used and compared with petrographic findings. The findings showed that the Sarvak formation in the studied field consists of 8 microfacies belonging to the sub-environments of the lagoon, carbonate bar, middle ramp and outer ramp, which were deposited in a homoclinal ramp environment. The main diagenesis processes affecting this reservoir include cementation, dissolution, fracture, stylolitization, and dolomitization. The results of multi-resolution graph-based analysis led to the identification of 3 electrofacies, EF1 electrofacies had the weakest reservoir parameters and EF3 facies had the best reservoir status. The majority of EF1 microfacies are grainstone microfacies and the majority of EF3 microfacies correspond to wackstone and packstone microfacies. Based on this, it seems that the lagoon sub-environment has a better reservoir condition than other sub-environments, especially the carbonate bar, and this is an important sign of the different performance of diagenesis processes in these sub-environments. In a vertical trend, the highest volume of hydrocarbon column is in the EF3 electrofacies and the lowest is EF1. In general, it can be stated that the use of multi-resolution graph-based analysis and comparison with petrographic findings is a suitable solution for accurate evaluation of the reservoir quality of carbonate reservoirs. Manuscript profile