سازند پابده

Open Access Article

1 - Geochemical Investigation and Effect of Sedimentary Environment Changes on Pabdeh Formation Hydrocarbon Potentiality in Mansuri Oilfield
بهرام علیزاده ندا جنت مکان هرمز قلاوند محمد حسین حیدری فرد

Pabdeh Formation is one of the most important probable source rocks in Mansuri oifield being under investigation . In this study, hydrocarbon potential of pabdeh formation is evaluated. Also effect of sedimentary environment changes on geo More

Pabdeh Formation is one of the most important probable source rocks in Mansuri oifield being under investigation . In this study, hydrocarbon potential of pabdeh formation is evaluated. Also effect of sedimentary environment changes on geochemical and hydrocarbon potential variation is studied ,To achieve this , hydrocarbon potential of Pabdeh Formation with Rock Eval Pyrolysis was investigated .Besides that, gas chromatography and gas chromatography-mass spectrometry data were utilized . Based on this study , in the Late Eocene age , relative sea level had raised , while in the Oligocene age, falling in sea level was occurred .Variation in sea level caused Pabdeh Formation to be heterogeneous in hydro carbon potential . Pabdeh Formation in Mansuri oilfield from geochemical aspects is divided into three divisions. Lower ad Upper zones I this formation, have fair (0.5-1%TOC) to good (1-2%TOC0 hydrocarbon potential and contain Kerogen type III. These zones have gas production potential . Middel zone, has very good (2-4%TOC) to excellent (TOC>4%) potential and contains Kerogen type II and III.Middel zone has oil production potential . Rock Eval data as well as thermal history modeling demonstrate that; Pabdeh Formaion is in early oil window, started yielding petroleum since 5-6 million years Manuscript profile

Open Access Article

2 - Geochemical Investigation and Effect of Sedimentary Environment Changes on Pabdeh Formation Hydrocarbon Potentiality in Mansuri Oilfield
بهرام علیزاده ندا جنت مکان هرمز قلاوند محمد حسین حیدری فرد

Pabdeh Formation is one of the most important probable source rocks in Mansuri oifield being under investigation . In this study, hydrocarbon potential of pabdeh formation is evaluated. Also effect of sedimentary environment changes on geo More

Pabdeh Formation is one of the most important probable source rocks in Mansuri oifield being under investigation . In this study, hydrocarbon potential of pabdeh formation is evaluated. Also effect of sedimentary environment changes on geochemical and hydrocarbon potential variation is studied ,To achieve this , hydrocarbon potential of Pabdeh Formation with Rock Eval Pyrolysis was investigated .Besides that, gas chromatography and gas chromatography-mass spectrometry data were utilized . Based on this study , in the Late Eocene age , relative sea level had raised , while in the Oligocene age, falling in sea level was occurred .Variation in sea level caused Pabdeh Formation to be heterogeneous in hydro carbon potential . Pabdeh Formation in Mansuri oilfield from geochemical aspects is divided into three divisions. Lower ad Upper zones I this formation, have fair (0.5-1%TOC) to good (1-2%TOC0 hydrocarbon potential and contain Kerogen type III. These zones have gas production potential . Middel zone, has very good (2-4%TOC) to excellent (TOC>4%) potential and contains Kerogen type II and III.Middel zone has oil production potential . Rock Eval data as well as thermal history modeling demonstrate that; Pabdeh Formaion is in early oil window, started yielding petroleum since 5-6 million years Manuscript profile

Open Access Article

3 - Biostratigraphy and Lithostratigraphy of Pabdeh Formation is based on planktonic foraminifera in the section of Jahangirabad (south Ilam_ Zagros basin)
somaye taherizade Mohammad Vahidinia mohammadhossein mahmoudi gharaii

10.61186/ispg.40920.11.22.66

After the Late Cretaceous and during the Paleogene, with the sea level rising, the Zagros sedimentary basin is covered with a progressive sea in which the Pabdeh Formation is deposited. The dual function of this formation as a source of oil and its reservoir capacity More

After the Late Cretaceous and during the Paleogene, with the sea level rising, the Zagros sedimentary basin is covered with a progressive sea in which the Pabdeh Formation is deposited. The dual function of this formation as a source of oil and its reservoir capacity due to the diversity of lithology and its location between the two reservoirs Asmari and Bangistan, and the age of this formation is one of the issues that has attracted the attention of geologists. In order to study the stratigraphic and biostratigraphic rock of the Pabdeh Formation, the Jahangirabad section in the northwest of Zagros sedimentary basin has been selected and sampled. 320 samples were taken, of which 230 samples were prepared by washing method, and 90 samples were prepared by thin section method and examined. Based on studies conducted in the Jahangirabad section, 25 genera and 110 species have been identified, and based on the identified fossils, 27 biozones and 7 sub-biozones have been identified. Based on the identified biozones, the age of the Pabdeh Formation in the Jahangirabad Danian Early-Late Chattian section has been obtained. Pabdeh Formation deposits in the Jahangirabad section have a thickness of 676 m (beginning of purple shale to anhydrite Kalhor) which includes units of purple shale (2 parts), marl limestone with lower limestone, limestone, and marl limestone with limestone It is high. In this section, the lower boundary of the Pabdeh Formation is continuous with shales and marls of Gurpi Formation, and its upper boundary is with continuous limestone of Asmari Formation. Manuscript profile

Open Access Article

4 - Depositional Environmental Analysis of Shally Units of Pabdeh-Gurpi Formation and Clay Minerals Effect on Wellbore Stability, Aghajari Oil Field
بهمن سلیمانی Zahra Dehghani

<!-- [if gte mso 9]><xml> <w:WordDocument> <w:View>Normal</w:View> <w:Zoom>0</w:Zoom> <w:TrackMoves/> <w:TrackForm More

<span style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; font-family: 'Times New Roman',serif; mso-fareast-font-family: Calibri; mso-bidi-theme-font: major-bidi; mso-bidi-language: FA; mso-bidi-font-weight: bold;">This research is related to detect of clay minerals and geochemical changes of Pabdeh-Gurpi shale formations and their role in borehole instability in Aghajari oil field. For this purpose, these formations were investigated using NGS well log (one well ring), X-ray diffraction method (XRD) and XRF analytical method (11 samples from two wells). In the NGS log, the detected minerals are illite, montmorillonite, mixed layer, glauconite and feldspar. In the XRD method, clay minerals illite, montmorillonite, mixed layer, chlorite and kaolinite were identified in order of abundance.These minerals due to their sensitivity to react with water causes the instability of the borehole. The high ratio of Si/Al and changes of Ti and high level of Fe3+ and Mg are also a sign of the widespread presence of illite, chlorite and montmorillonite in the mentioned formations.   <span style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; font-family: 'Times New Roman',serif; mso-fareast-font-family: Calibri; mso-bidi-theme-font: major-bidi; mso-bidi-language: FA; mso-bidi-font-weight: bold;">The changes of major and trace elements compared to Al2O3 except for MnO, CaO, and P2O5 showed a positive linear relationship. The changes in the amount of Fe2O3 show the oxidizing conditions in the upper part of the base, but the reducing conditions towards the upper side. Based on the amount of iron, manganese and vanadium, the sediments were formed under conditions of reduction, non-sulphide reduction Eh and medium to low pH. Variations in Th/U ratio (1-4.5) indicate marine to transitional environments. The existence of horizons rich in organic matter (more than 2%) confirms the reduction conditions.   <span style="font-size: 10.0pt; mso-bidi-font-size: 11.0pt; font-family: 'Times New Roman',serif; mso-fareast-font-family: Calibri; mso-bidi-theme-font: major-bidi; mso-bidi-language: FA; mso-bidi-font-weight: bold;">Based on the low values of the Zr/Rb ratio, the sediments in the upper and lower parts are finer than the middle part of the grain. The relative accumulation of biogenic carbonate along with the shale is periodic and is reflected in the changes in the (Zr+Rb)/Sr ratio. Based on the Sr/Ba ratio, marine conditions prevail in the lower part and continental and metamorphic and sometimes marine conditions prevail in the upper part of the formation. Oxidation-reduction conditions were also investigated. The values of the V/(V + Ni) ratio of the semi-reduction region, the Ni/Co ratio of the reduction region and the V/Cr diagram show the almost reduction region and in some cases the oxidant conditions. Paleoclimatic conditions at the time of sedimentation based on low values of Rb/Sr ratio (less than 0.14) were completely hot and dry.   Manuscript profile

Open Access Article

5 - Lithostratigraphy and Biostratigraphy of Pabdeh Formation based on planktonic foraminifera in the Ilam dam section (south Ilam_ Zagros sedimentari basin)
somaye taherizade Mohammad Vahidinia Mohammadhossein mahmoudi gharaii

Zagros Sedimentary basin is located in the south and southwest of Iran and Pabdeh Formation is one of the most important Cenozoic units of Zagros Sedimentary basin. In addition, Pabdeh Formation is of special importance as one of the source rocks of Zagros Sedimentary b More

Zagros Sedimentary basin is located in the south and southwest of Iran and Pabdeh Formation is one of the most important Cenozoic units of Zagros Sedimentary basin. In addition, Pabdeh Formation is of special importance as one of the source rocks of Zagros Sedimentary basin. In order to study the Lithostratigraphic and Biostratigraphic rocks of Pabdeh Formation, the section of Ilam dam in the northwest of Zagros sedimentary basin has been selected and sampled. 360 samples were taken, of which 260 washing samples and 100 thin section samples were prepared. Based on the studies performed on these samples, 25 genera and 105 species have been identified in the Ilam dam section. 26 biozones and 2 sub-biozones have been identified based on the biological zoning of Wade et al., 2011 in the Tethys area. Based on the identified biozones, the age of Pabdeh Formation in the Ilam dam section, Middle Danian-Early Aquitanian has been obtained. The deposits of Pabdeh Formation in the section of Ilam dam have a thickness of 764 m (beginning of Pabdeh to the beginning of Kalhor anhydrite) which includes purple shale units (2 Units), marl limestone with lower limestone, cherti limestone, marl limestone with upper limestone. The lower boundary of Pabdeh Formation in this section is conform and continuous with shales and marls of Gurpi Formation but its upper boundary with the gypsums of the Asmari formation is most likely accompanied by a disconform. Manuscript profile

List of Articles سازند پابده

Rimag

Links

Related Centers

Technical Support

Official pages