Relevant bibliographies by topics / Oman Moho Transition Zone

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Academic literature on the topic 'Oman Moho Transition Zone'

Author: Grafiati
Published: 9 March 2023

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Journal articles on the topic "Oman Moho Transition Zone"

1

BOUDIER, F., and A. NICOLAS. "Nature of the Moho Transition Zone in the Oman Ophiolite." Journal of Petrology 36, no. 3 (1995): 777–96. http://dx.doi.org/10.1093/petrology/36.3.777.

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2

Jousselin, David, Luiz F. G. Morales, Marie Nicolle, and Aurore Stephant. "Gabbro layering induced by simple shear in the Oman ophiolite Moho transition zone." Earth and Planetary Science Letters 331-332 (May 2012): 55–66. http://dx.doi.org/10.1016/j.epsl.2012.02.022.

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3

Michibayashi, Katsuyoshi, and Tatsuya Oohara. "Olivine fabric evolution in a hydrated ductile shear zone at the Moho Transition Zone, Oman Ophiolite." Earth and Planetary Science Letters 377-378 (September 2013): 299–310. http://dx.doi.org/10.1016/j.epsl.2013.07.009.

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4

Rajendran, Sankaran, and Sobhi Nasir. "Mapping of Moho and Moho Transition Zone (MTZ) in Samail ophiolites of Sultanate of Oman using remote sensing technique." Tectonophysics 657 (August 2015): 63–80. http://dx.doi.org/10.1016/j.tecto.2015.06.023.

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5

Jousselin, David, Adolphe Nicolas, Françoise Boudier, Laurie Reisberg, Mathilde Henri, and Marie Nicolle. "Formation of the Moho transition zone in the Oman ophiolite, and comparison with sub-Moho melt lenses at fast spreading ridges." Tectonophysics 821 (December 2021): 229148. http://dx.doi.org/10.1016/j.tecto.2021.229148.

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6

Korenaga, Jun, and Peter B. Kelemen. "Origin of gabbro sills in the Moho transition zone of the Oman ophiolite: Implications for magma transport in the oceanic lower crust." Journal of Geophysical Research: Solid Earth 102, B12 (1997): 27729–49. http://dx.doi.org/10.1029/97jb02604.

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7

Rollinson, Hugh, and Jacob Adetunji. "Mantle podiform chromitites do not form beneath mid-ocean ridges: A case study from the Moho transition zone of the Oman ophiolite." Lithos 177 (September 2013): 314–27. http://dx.doi.org/10.1016/j.lithos.2013.07.004.

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8

Negishi, Hironori, Shoji Arai, Hisayoshi Yurimoto, et al. "Sulfide-rich dunite within a thick Moho transition zone of the northern Oman ophiolite: Implications for the origin of Cyprus-type sulfide deposits." Lithos 164-167 (April 2013): 22–35. http://dx.doi.org/10.1016/j.lithos.2012.11.024.

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9

Rospabé, Mathieu, Mathieu Benoit, Georges Ceuleneer, Florent Hodel, and Mary-Alix Kaczmarek. "Extreme geochemical variability through the dunitic transition zone of the Oman ophiolite: Implications for melt/fluid-rock reactions at Moho level beneath oceanic spreading centers." Geochimica et Cosmochimica Acta 234 (August 2018): 1–23. http://dx.doi.org/10.1016/j.gca.2018.05.012.

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10

Al-Lazki, Ali I., Dogan Seber, Eric Sandvol, and Muawia Barazangi. "A crustal transect across the Oman Mountains on the eastern margin of Arabia." GeoArabia 7, no. 1 (2002): 47–78. http://dx.doi.org/10.2113/geoarabia070147.

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Abstract:
ABSTRACT The unique tectonic setting of the Oman Mountains and the Semail Ophiolite, together with ongoing hydrocarbon exploration, have focused geological research on the sedimentary and ophiolite stratigraphy of Oman. However, there have been few investigations of the crustal-scale structure of the eastern Arabian continental margin. In order to rectify this omission, we made a 255-km-long, southwesterly oriented crustal transect of the Oman Mountains from the Coastal Zone to the interior Foreland via the 3,000-m-high Jebel Akhdar. The model for the upper 8 km of the crust was constrained using 152 km of 2-D seismic reflection profiles, 15 exploratory wells, and 1:100,000- to 1:250,000-scale geological maps. Receiver-function analysis of teleseismic earthquake waveform data from three temporary digital seismic stations gave the first reliable estimates of depth-to-Moho. Bouguer gravity modeling provided further evidence of depths to the Moho and metamorphic basement. Four principal results were obtained from the transect. (1) An interpreted mountain root beneath Jebel Akhdar has a lateral extent of about 60 km along the transect. The depth-to-Moho of 41 to 44 km about 25 km southwest of Jebel Akhdar increased to 48 to 51 km on its northeastern side but decreased to 39 to 42 km beneath the coastal plain farther to the northeast. (2) The average depth to the metamorphic basement was inferred from Bouguer gravity modeling to be 9 km in the core of Jebel Akhdar and immediately to the southwest. A relatively shallow depth-to-basement of 7 to 8 km coincided with the Jebel Qusaybah anticline south of the Hamrat Ad Duru Range. (3) Based on surface, subsurface, and gravity modeling, the Nakhl Ophiolite block extends seaward for approximately 80 km from its most southerly outcrop. It has an average thickness of about 5 km, whereas ophiolite south of Jebel Akhdar is only 1 km thick. The underlying Hawasina Sediments are between 2 and 3 km thick in the Hamrat Ad Duru Zone, and 2 km thick in the Coastal Zone. (4) Southwest of Jebel Akhdar, reactivated NW-oriented strike-slip basement faults that deformed Miocene to Pliocene sediments were inferred from the interpretation of seismic reflection profiles.
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