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Journal articles on the topic 'Diapirs – Oman'

Author: Grafiati
Published: 4 June 2021
Last updated: 20 May 2022

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1

Peters, Jeroen M., Jacek B. Filbrandt, John P. Grotzinger, Mark J. Newall, Mark W. Shuster, and Hisham A. Al-Siyabi. "Surface-piercing salt domes of interior North Oman, and their significance for the Ara carbonate ‘stringer’ hydrocarbon play." GeoArabia 8, no. 2 (2003): 231–70. http://dx.doi.org/10.2113/geoarabia0802231.

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ABSTRACT The six surface-piercing salt domes of interior North Oman form prominent topographic and geological features in an otherwise flat, rocky desert environment. These domes in the central part of the Ghaba Salt Basin have been known since the 1950s but very little data has been published on them. Our geological survey in 2001 provided significant new lithological, stratigraphic, and sedimentological information on the rocks exposed in the domes. This paper provides a comprehensive overview of the morphology, geometry, structural geology and geological evolution of the salt domes. Further
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2

Rabinowicz, M., G. Ceuleneer, and A. Nicolas. "Melt segregation and flow in mantle diapirs below spreading centers: Evidence from the Oman Ophiolite." Journal of Geophysical Research 92, B5 (1987): 3475. http://dx.doi.org/10.1029/jb092ib05p03475.

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3

Cooper, David J. W., Mohammed Y. Ali, Michael P. Searle, and Ali I. Al-Lazki. "Salt intrusions in Jabal Qumayrah, northern Oman Mountains: Implications from structural and gravity investigations." GeoArabia 18, no. 2 (2013): 141–76. http://dx.doi.org/10.2113/geoarabia1802141.

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ABSTRACT The Jabal Qumayrah area, 50 km ESE of Al Ain and Buraimi, preserves a culmination of Jurassic and Cretaceous continental slope deposits (Sumeini Group) that was emplaced during the Late Cretaceous onto the Oman margin with other Neo-Tethyan units and the Semail Ophiolite. Almost uniquely in the Oman Mountains, Jabal Qumayrah also contains outcrops of gypsum and anhydrite that occur as a central complex from which laterally discontinuous linear and arcuate outcrops extend up to 4 km to the northwest and south. The gypsum and anhydrite bodies contain sedimentary clasts and rafts, which
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4

Csontos, László, Tamás Pocsai, Ágoston Sasvári, et al. "Structural evolution of the Hawasina Window, Oman Mountains." GeoArabia 15, no. 3 (2010): 85–124. http://dx.doi.org/10.2113/geoarabia150385.

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ABSTRACT This paper presents field observations and measurements from the Hawasina Window, Oman Mountains. An updated geological map is based partly on previous publications and four NEtrending cross-sections. Along each cross-section key structural features are described, illustrated and interpreted. Based on these (and other) observations several differences between our interpretation and the former published geological maps and cross sections were noted as follows.(1) Late Cretaceous original (Hamrat Duru; Haybi) nappes that formed during intra-oceanic obduction underwent out-of-sequence th
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5

Ali, Mohammed Y., David J. W. Cooper, Michael P. Searle, and Ali Al-Lazki. "Origin of gypsiferous intrusions in the Hawasina Window, Oman Mountains: Implications from structural and gravity investigations." GeoArabia 19, no. 2 (2014): 107–32. http://dx.doi.org/10.2113/geoarabia1902107.

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ABSTRACT Gypsiferous intrusions are exposed in road-cuts in the south-central Hawasina Window in the central Oman Mountains. They are located at lower structural levels in the allochthonous Hawasina Complex and lie along faults that cut Upper Cretaceous structures related to the obduction of the Semail Ophiolite and Hawasina Complex deep-water sediments onto the Arabian Plate. The intrusions form gypsiferous pods that are up to 200 m long, in which the gypsum occurs as a dark, fine-grained matrix that contains a pervasive network of anastomosing veins of gypsum and anhydrite. The intrusions co
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6

Nicolle, Marie, David Jousselin, Laurie Reisberg, Delphine Bosch, and Aurore Stephant. "Major and trace element and Sr and Nd isotopic results from mantle diapirs in the Oman ophiolite: Implications for off-axis magmatic processes." Earth and Planetary Science Letters 437 (March 2016): 138–49. http://dx.doi.org/10.1016/j.epsl.2015.12.005.

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7

Reuning, Lars, Schoenherr Johannes, Heimann Ansgar, et al. "Constraints on the diagenesis, stratigraphy and internal dynamics of the surface-piercing salt domes in the Ghaba Salt Basin (Oman): A comparison to the Ara Group in the South Oman Salt Basin." GeoArabia 14, no. 3 (2009): 83–120. http://dx.doi.org/10.2113/geoarabia140383.

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ABSTRACT In the South Oman Salt Basin (SOSB), the Ara carbonates form an extensively cored, deeply buried intra-salt hydrocarbon play. Six surface-piercing salt domes in the Ghaba Salt Basin (northern Oman) provide the only outcrop equivalents for carbonates and evaporites of the Ediacaran – Early Cambrian Ara Group (upper Huqf Supergroup). Based on fieldwork, satellite images and isotope analysis it is concluded that most of the carbonate bodies (so-called stringers) in the Ghaba salt domes are time-equivalent to the stratigraphically uppermost stringer intervals in the SOSB (A5–A6). Maturity
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8

Collier, J. S., and R. S. White. "Mud diapirism within Indus fan sediments: Murray Ridge, Gulf of Oman." Geophysical Journal International 101, no. 2 (1990): 345–53. http://dx.doi.org/10.1111/j.1365-246x.1990.tb06573.x.

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9

Nicolas, A., G. Ceuleneer, F. Boudier, and M. Misseri. "Structural mapping in the Oman ophiolites: Mantle diapirism along an oceanic ridge." Tectonophysics 151, no. 1-4 (1988): 27–56. http://dx.doi.org/10.1016/0040-1951(88)90239-9.

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10

Benoit, Mathieu, Mireille Polvé, and Georges Ceuleneer. "Trace element and isotopic characterization of mafic cumulates in a fossil mantle diapir (Oman ophiolite)." Chemical Geology 134, no. 1-3 (1996): 199–214. http://dx.doi.org/10.1016/s0009-2541(96)00087-3.

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11

Jousselin, David, Adolphe Nicolas, and Françoise Boudier. "Detailed mapping of a mantle diapir below a paleo-spreading center in the Oman ophiolite." Journal of Geophysical Research: Solid Earth 103, B8 (1998): 18153–70. http://dx.doi.org/10.1029/98jb01493.

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12

Oterdoom, W. Heiko, Mike A. Worthing, and Mark Partington. "Petrological and Tectonostratigraphic Evidence for a Mid Ordovician Rift Pulse on the Arabian Peninsula." GeoArabia 4, no. 4 (1999): 467–500. http://dx.doi.org/10.2113/geoarabia0404467.

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ABSTRACT During late Early Ordovician times an increase in the rate of subsidence in the Ghaba Salt Basin and western South Oman Salt Basin is suggested by the thick sequence of continental clastics of the Ghudun Formation. After a phase of rift-shoulder uplift and erosion, related to a renewed pulse of extension which may have initiated diapiric growth of salt structures in the Ghaba Salt Basin, sedimentation resumed again in the Mid Ordovician. During this period, the center of deposition shifted to the Saih Hatat area in North Oman. This paper documents seismic and well data, field investig
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13

Becker, Stephan, Lars Reuning, Joachim E. Amthor, and Peter A. Kukla. "Diagenetic Processes and Reservoir Heterogeneity in Salt-Encased Microbial Carbonate Reservoirs (Late Neoproterozoic, Oman)." Geofluids 2019 (November 4, 2019): 1–19. http://dx.doi.org/10.1155/2019/5647857.

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A common problem in dolomite reservoirs is the heterogeneous distribution of porosity-reducing diagenetic phases. The intrasalt carbonates of the Ediacaran-Early Cambrian Ara Group in the South Oman Salt Basin represent a self-sourcing petroleum system. Depositional facies and carbonate/evaporite platform architecture are well understood, but original reservoir properties have been modified by diagenesis. Some of the carbonate reservoirs failed to produce hydrocarbons at acceptable rates, which triggered this study. The extent of primary porosity reduction by diagenetic phases was quantified u
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14

Reuber, I., P. Nehlig, and T. Juteau. "Axial segmentation at a fossil oceanic spreading centre in the Haylayn block (Semail nappe, Oman): off-axis mantle diapir and advancing ridge tip." Journal of Geodynamics 13, no. 2-4 (1991): 253–78. http://dx.doi.org/10.1016/0264-3707(91)90041-c.

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15

Clénet, Harold, Georges Ceuleneer, Patrick Pinet, et al. "Thick sections of layered ultramafic cumulates in the Oman ophiolite revealed by an airborne hyperspectral survey: Petrogenesis and relationship to mantle diapirism." Lithos 114, no. 3-4 (2010): 265–81. http://dx.doi.org/10.1016/j.lithos.2009.09.002.

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16

Samadi, Hamid Reza. "Retracted: Pierced Salt Domes in the Persian Gulf and in the Zagros Mountain Ranges in Southern Iran and their Relationship to Hydrocarbon and Basement Tectonics." International Journal of Geography and Geology 2, no. 10 (2013): 116–33. http://dx.doi.org/10.18488/journal.10/2013.2.10/10.10.116.133.

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The most enigmatic problems with the nearly 200 salt domes pierced in the Persian Gulf and in the Zagros Mountain Ranges (ZMR) in southern Iran, a unique morphology in the world, have been the matter of this study, which is based on a combination of field work, enhancement of satellite and aerial photographs etc. In the ZMR, structural anomalies are frequently associated with similar facies distribution patterns. In the eastern portion of the region, emergent salt plugs of Infra-Cambrian age exhibit the same alignment patterns. Such trends bear no apparent genetic relationship to the Tertiary
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17

Rospabé, Mathieu, Georges Ceuleneer, Nicolas Granier, Shoji Arai, and Anastassia Y. Borisova. "Multi-scale development of a stratiform chromite ore body at the base of the dunitic mantle-crust transition zone (Maqsad diapir, Oman ophiolite): The role of repeated melt and fluid influxes." Lithos 350-351 (December 2019): 105235. http://dx.doi.org/10.1016/j.lithos.2019.105235.

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18

Rospabé, Mathieu, Georges Ceuleneer, Vanessa Le Guluche, Mathieu Benoit, and Mary-Alix Kaczmarek. "The Chicken and Egg Dilemma Linking Dunites and Chromitites in the Mantle–Crust Transition Zone beneath Oceanic Spreading Centres: a Case Study of Chromite-hosted Silicate Inclusions in Dunites Formed at the Top of a Mantle Diapir (Oman Ophiolite)." Journal of Petrology 62, no. 4 (2021). http://dx.doi.org/10.1093/petrology/egab026.

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Abstract The mantle–crust boundary beneath oceanic spreading centres is a major chemical and thermal interface on Earth. Observations in ophiolites reveal that it is underlined by a dunitic transition zone (DTZ) that can reach a few hundred meters in thickness and host abundant chromitite ore bodies. The dunites have been deciphered as essentially mantle-derived in most ophiolitic massifs; that is, reactional residues of interactions between peridotite and percolating melt(s). Although both dunite and chromitite in ophiolites have been the focus of many studies, the reasons for their systemati
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19

Jousselin, David, Robert Dunn, and Douglas R. Toomey. "Modeling the seismic signature of structural data from the Oman Ophiolite: Can a mantle diapir be detected beneath the East Pacific Rise?" Geochemistry, Geophysics, Geosystems 4, no. 7 (2003). http://dx.doi.org/10.1029/2002gc000418.

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