Arabian Plate Sequence Stratigraphy – revisions to SP2

Sharland, Peter R.; Casey, David M.; Davies, Roger B.; Simmons, Michael D.; Sutcliffe, Owen E.

doi:10.2113/geoarabia0901199

Cited by 262 publications

(176 citation statements)

References 25 publications

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“…The created CPI for the wells HR-2, HR-8, HR-9, and HR-16 presenting Jeribe Formation at Hamrin oil field as a reservoir that is composed of dolomite with some limestone and anhydrite layers and consisting of two reservoir units extend along the field. Figures 3,4,5,6 show Computer Processed Interpretation of wells HR-2, HR-8, HR-9, and HR-16, respectively.…”

Section: Resultsmentioning

confidence: 99%

“…It is nearly 10km from north of Salahaddin Governorate and about 80km southwest of Kirkuk City, north of Iraq [3]. The Jeribe Limestone was defined by Bellen in 1957 from the type locality near Jaddala village in the Sinjar anticline and assumed to be of the Early Miocene age [4]. However, the formation was later included within the Middle Miocene sequence [5].…”

Section: Study Areamentioning

confidence: 99%

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Determination of Petrophysical characteristics using Techlog Software of Jeribe Reservoir in Hamrin - Allas Oilfield, Northern Iraq

Kamal

Jassim

2022

eijs

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This study aims to assess the formation evaluation of the Jeribe Formation in Hamrin oilfield. The present study involved four selected wells of (Early- Mid Miocene) Jeribe Formation in Hamrin structure-Allas field; HR-2, HR-8, HR-9, and HR-16 located North of Iraq. The work deals with the available data that includes the most required information to improve such studies. Techlog Software V.2015 was used to carry out a reliable calculation of petrophysical properties utilizing conventional logs to determine the reservoir characteristics (lithology, porosity, and saturation). The computed CPI (software resulted) based on log information divided the Jeribe reservoir into two reservoir units (Jr-1 and Jr-2) within the studied wells. The calculated effective porosity and water saturation revealed that the unit Jr-1 in Hamrin- Allas oil field contains hydrocarbons at wells HR-2 and HR-16. In contrast, unit Jr-2 was 100% water-saturated along the selected well depths at wells HR-2, HR-8, HR-9, and HR-16.

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Section: Resultsmentioning

confidence: 99%

Section: Study Areamentioning

confidence: 99%

Determination of Petrophysical characteristics using Techlog Software of Jeribe Reservoir in Hamrin - Allas Oilfield, Northern Iraq

Kamal

Jassim

2022

eijs

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“…3) together with sparse 2D seismic data plus supporting studies, are integrated within a consistent biostratigraphically age-constrained sequence stratigraphic framework (Fig. 2) derived from the Arabian Plate Sequence Stratigraphic model of Sharland et al (2001).…”

Section: Methodsmentioning

confidence: 99%

“…During the mid-Cretaceous, the Arabian Plate lay on the southern margin of NeoTethys in a position close to the equator (Sharland et al, 2001;Scotese, 2021). Relatively high sea levels (Miller et al, 2005;Haq, 2014; Wright et al, 2020) led to inundation of the plate and the widespread deposition of shallow-marine carbonates, although siliciclastic units were deposited proximal to the Arabian Shield and prograded basinwards during lowstands (Davies et al, 2002;2019;van Buchem et al, 2011).…”

Section: Tectonostratigraphic Overviewmentioning

confidence: 99%

“…Kazhdumi Formation; Davies et al, 2002;Bordenave, 2014;Sfidari et al, 2016). In the late Albian, these siliciclastic systems were suppressed during a transgression (K110 MFS sensu Sharland et al, 2001) and a broad carbonate ramp (Mauddud Formation and regional equivalents) was established across the plate (Davies et al, 2002(Davies et al, , 2019Strohmenger et al, 2006;Cross et al, 2010;van Buchem et al, 2011).…”

Section: Albianmentioning

confidence: 99%

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Sequence Stratigraphy, Palaeogeography and Petroleum Plays of the Cenomanian – Turonian Succession of the Arabian Plate: An Updated Synthesis

Bromhead

Buchem

Simmons

et al. 2022

Journal of Petroleum Geology

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The Cenomanian -Turonian succession of the Arabian Plate By contrast in the Najaf intrashelf basin (Iraq), there is a significant siliciclastic component sourced from the Arabian Shield. This influx resulted in a mixed carbonatesiliciclastic ramp depositional system on the proximal, western margin of the basin, and an apparent absence of organic-rich intervals within the central basin succession. Grainy carbonate reservoir rocks are restricted to the eastern margin and are charged by older source rocks within the underlying stratigraphy.The GDE maps record the configuration of these petroleum systems elements within the Cenomanian-Turonian interval and form the basis for play screening. The Cenomanian-Turonian interval is punctuated by the major mid-Turonian unconformity which is a tectonostratigraphic boundary of considerable geological and economic significance. In the southern and eastern part of the Arabian Plate, this unconformity has a differential erosion profile that facilitates a subcrop play with exploration potential. Identifying subtle stratigraphic traps is challenging, but by combining GDE facies with the mapped preservation limit for each sequence, it is possible to identify areas where rudist-rich reservoir facies with potential karst enhancement are overlain by a regional claystone seal, high-grading areas with subcrop trap potential.

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The Cambrian and Earliest Ordovician Quiescent Margin of Gondwana

Woodcock

2012

Geological History of Britain and Ireland

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Arabian Plate Sequence Stratigraphy – revisions to SP2

Cited by 262 publications

References 25 publications

Determination of Petrophysical characteristics using Techlog Software of Jeribe Reservoir in Hamrin - Allas Oilfield, Northern Iraq

Determination of Petrophysical characteristics using Techlog Software of Jeribe Reservoir in Hamrin - Allas Oilfield, Northern Iraq

Sequence Stratigraphy, Palaeogeography and Petroleum Plays of the Cenomanian – Turonian Succession of the Arabian Plate: An Updated Synthesis

The Cambrian and Earliest Ordovician Quiescent Margin of Gondwana

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