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Relevant bibliographies by topics / Diapirs – Oman

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Academic literature on the topic 'Diapirs – Oman'

Author: Grafiati

Published: 4 June 2021

Last updated: 20 May 2022

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Journal articles on the topic "Diapirs – Oman"

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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