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Dalan Basin

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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2013
GeoArabia (2013) 18 (2): 17–62.
...Vladimir I. Davydov; Arefifard Sakineh ABSTRACT The Middle–Upper Permian (Guadalupian–Lopingian) Dalan Basin was part of a very large carbonate ramp/platform along the passive margin of the Arabian Plate, located at mid-latitude Neo-Tethys Ocean. As shown in the modern world the mid-latitudes...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 April 2006
GeoArabia (2006) 11 (2): 75–176.
... of the Upper Dalan Member and Kangan Formation in the Zagros to the offshore Fars area was carried out. The areas that were studied in detail are the Kuh-e Surmeh and Kuh-e Dena sections of the Zagros Mountains, Iran, and their equivalent in the offshore Fars subsurface. The observations and interpretations...
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Journal Article
Published: 01 November 2009
Petroleum Geoscience (2009) 15 (4): 325–344.
... fields have been discovered in the Persian Gulf Basin since the 1970s. Most of these fields produce from the Permian Dalan and Triassic Kangan formations ( Stratigraphic Committee of Iran 1976 ; Szabo & Kheradpir 1978 ), or Khuff carbonates. According to our estimates, this interval in the Persian...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2007
GeoArabia (2007) 12 (1): 63–130.
... occurs in the Upper Ordovician K1–K4 members and consists of sandstones with a fracture porosity of up to 7.6% and permeability of 0.13 mD. In North Iraq the carbonates of the Permian Chia Zairi and Triassic Mirga Mir formations correlate to gas reservoirs in the Khuff Formation of Arabia and the Dalan...
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Series: Geological Society, London, Memoirs
Published: 03 January 2020
DOI: 10.1144/M50-2018-34
EISBN: 9781786204707
... Ga and, more conspicuously, late-orogenic activity at c. 0.95–0.92 Ga during the Dalane tectonothermal phase ( Bingen et al. 2008 a , b ) form significant components in the Idefjorden terrane. The Idefjorden terrane is either thrust on top of the Eastern Segment or, in the northerly part...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2016
AAPG Bulletin (2016) 100 (10): 1561–1584.
... associated with hydrothermal dolomite precipitation, which may partially occlude any generated porosity ( Smith, 2006 ). The classic example for this type of karst-enhanced hydrocarbon reservoir is the Albion–Scipio field in the Michigan Basin, Michigan ( Harding, 1974 ; Davies and Smith, 2006 ; Smith...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2003
DOI: 10.1306/M78834C2
EISBN: 9781629810539
...%, of the earth’s land surface. In this paper, we present maps showing the location of all 877 giants located on tectonic and sedimentary basin maps of these 27 key regions. We classify the tectonic setting of the giants in these regions using six simplified classes of the tectonic setting for basins...
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Journal Article
Published: 06 February 2015
Journal of the Geological Society (2015) 172 (2): 237–250.
... has undergone lithospheric extension during the Permian–Triassic, which led to the formation of the Neo-Tethys. The aim of this paper is to describe the development of the continental rift basin in the Zagros region based on the tectono-sedimentological evolution. We have studied well-log data...
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Series: Geological Society, London, Memoirs
Published: 03 January 2020
DOI: 10.1144/M50-2017-6
EISBN: 9781786204707
... an erosional relict of a larger and spatially much more extensive early Tonian foreland basin to this orogen, as proposed earlier on the basis of fission-track thermochronology. Chapter 13 addresses early Tonian dolerite dykes and siliciclastic sedimentary rocks intruded by dolerite sills...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 January 2012
GeoArabia (2012) 17 (1): 181–239.
..., obtained from the gravity data, is then used for modeling the basal heat flow within the basin. We use a grid-based stochastic tool (PetroProb) developed by TNO to model basal heat flow. It is based on the inversion of basin subsidence data to calculate the tectonic subsidence in the area and the tectonic...
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Journal Article
Journal: Interpretation
Published: 13 December 2018
Interpretation (2019) 7 (1): T127–T139.
...Yuan Huang; Zhenyu Fan; Bing He; Song Tang; Weifeng Du Abstract Lower Triassic Feixianguan oolithic shoal complexes are widely developed in the northwestern Sichuan Basin, southwest China, where they host large natural gas reserves. To understand their development and the factors that controlled...
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Journal Article
Journal: Interpretation
Published: 15 October 2019
Interpretation (2019) 7 (4): SJ67–SJ75.
...Chao Liu; Lidong Sun; Jijun Li; Shuangfang Lu; Lei Tian; Pei Liu; Jia Yu Abstract To lay the foundation for the exploration of shale gas, we calculated the total organic carbon (TOC) of Shahezi Formation source rocks in the Xujiaweizi Fault Depression in the Songliao Basin by using the measuring...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2012
GSA Bulletin (2012) 124 (3-4): 484–498.
...Alireza Nadimi; Andrzej Konon Abstract The Gaw-Khuni Basin is located in the central part of the Sanandaj-Sirjan zone, on the northeastern margin of the Zagros orogen. This basin is one of the continuous zones of Sanandaj-Sirjan zone basins that is filled by Pliocene–Holocene sediments. The Gaw...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 2012
AAPG Bulletin (2012) 96 (8): 1389–1414.
...Daniel J. Lehrmann; Marcello Minzoni; Xiaowei Li; Meiyi Yu; Jonathan L. Payne; Brian M. Kelley; Ellen K. Schaal; Paul Enos Abstract Lower Triassic platforms in the Nanpanjiang Basin contain extensive oolites. Interior oolites are stacked in meter-scale cycles arranged into larger coarsening-upward...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2015
GeoArabia (2015) 20 (3): 99–140.
... Basins covering the northern, central and southeastern parts of Iraq, Kuwait and western and southwestern Iran, particularly the Lurestan and Khuzestan provinces. These source rocks include the Bajocian–Bathonian Sargelu, the Callovian–Lower Kimmeridgian Naokelekan and the Upper Tithonian–Lower...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2014
DOI: 10.1144/SP392.19
EISBN: 9781862396685
... in Figure 3 , and the Phanerozoic tectonic events listed in Table 2 . Fig. 3. Major tectonic elements in the Middle East showing sedimentary basins and sub-basins, palaeohighs, trends and faults (compiled from various sources: Henson 1951 ; Beydoun 1991 ; Alsharhan & Nairn 1997...
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Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 485–498.
...C.M. Burberry; C.A.-L. Jackson; J.W. Cosgrove Abstract: The Persian Gulf is part of an asymmetric foreland basin related to the Zagros Orogen. Few published studies of this basin and associated onshore areas include seismic reflection data. We present a seismic-stratigraphic interpretation based...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 July 2001
GeoArabia (2001) 6 (3): 407–442.
... Permian. The sediments were deposited in arid to glacial settings, reflecting the drift of the region from equatorial to high southern latitudes and back. Following late Precambrian rifting that formed salt basins in Oman and the Arabian Gulf region, the Cambrian-Devonian sequences were deposited...
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Journal Article
Journal: GeoArabia
Publisher: Gulf Petrolink
Published: 01 October 2007
GeoArabia (2007) 12 (4): 41–60.
...Shakeri Alireza; Douraghinejad Jalal; Moradpour Mehran ABSTRACT The late Oligocene-early Miocene Qom Formation in the Central Iran Basin contains oil and gas in the Alborz and Sarajeh fields. Organic geochemical analyses in previous studies indicated that the hydrocarbons migrated from deeper...
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Series: GSA Special Papers
Published: 21 December 2017
DOI: 10.1130/2016.2525(09)
EISBN: 9780813795256
... tectonics Postcollisional land uplift 11 Postorogenic molasse-type sediments Intramontane basin Obduction-collision 10 Oligocene-Miocene sequence Retro-arc foreland basin 9 Tertiary flysch-type sediments Foreland flysch basin Jurassic-Cretaceous 8 Zagros suture zone Collisional margin...
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