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Relevant bibliographies by topics / Gabbro – Oman

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Academic literature on the topic 'Gabbro – Oman'

Author: Grafiati

Published: 4 June 2021

Last updated: 9 February 2022

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Journal articles on the topic "Gabbro – Oman"

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Arafin, Sayyadul, and Ram N. Singh. "Thermal and Transport Properties of Mafic and Ultramafic Rocks of Oman Ophiolite." Sultan Qaboos University Journal for Science [SQUJS] 21, no. 1 (2016): 69. http://dx.doi.org/10.24200/squjs.vol21iss1pp69-81.

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Thermal and other physical properties of rocks and minerals are of considerable significance for deriving mineralogical and compositional models of the Earth's mantle. We have determined these properties for the mafic rock such as gabbro and ultramafic rock like harzburgite of the Oman ophiolite suite by utilizing the Debye characteristic property ,Θ-

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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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Falaknazi, Majid, and Mehrdad Karimi. "Mineralogy and Geochemistry of Titaniferous Gabbros of Ophiolitic Fanouj Zone (Sistan & Baluchestan, Iran)." Modern Applied Science 10, no. 4 (2016): 189. http://dx.doi.org/10.5539/mas.v10n4p189.

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<p><span lang="EN-US">Ophiolite complex in the west of Fanuj is 200 Km south west of Iranshahr in Sistan and Baluchestan province. This ophiolite complex lies in the uplift zone of the oceanic crust of Oman between Makran and Fanuj faults. Ophiolite of the west part of Fanuj is consisted of three parts including gabbro, diabase dikes and small quantity microdiorite masses. Ilmenite is the main mineral of titanium which along with magnetite has been formed independently or inter-crystalline way after crystallization of plagioclase, pyroxene and often along with amphibole in gabbro r

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ARAI, Shoji, and Marie PYTHON. "Pictorial 3: Possible Mohorovicic Discontinuities and Gabbro-peridotite Transitions Observed in the Oman Ophiolite." Chigaku Zasshi (Jounal of Geography) 117, no. 1 (2008): iii—viii. http://dx.doi.org/10.5026/jgeography.117.iii.

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Lamoureux, Gwenaëlle, Benoı̂t Ildefonse, and David Mainprice. "Modelling the seismic properties of fast-spreading ridge crustal Low-Velocity Zones: insights from Oman gabbro textures." Tectonophysics 312, no. 2-4 (1999): 283–301. http://dx.doi.org/10.1016/s0040-1951(99)00183-3.

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SHAFAII MOGHADAM, HADI, and ROBERT J. STERN. "Geodynamic evolution of Upper Cretaceous Zagros ophiolites: formation of oceanic lithosphere above a nascent subduction zone." Geological Magazine 148, no. 5-6 (2011): 762–801. http://dx.doi.org/10.1017/s0016756811000410.

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AbstractThe Zagros fold-and-thrust belt of SW Iran is a young continental convergence zone, extending NW–SE from eastern Turkey through northern Iraq and the length of Iran to the Strait of Hormuz and into northern Oman. This belt reflects the shortening and off-scraping of thick sediments from the northern margin of the Arabian platform, essentially behaving as the accretionary prism for the Iranian convergent margin. Distribution of Upper Cretaceous ophiolites in the Zagros orogenic belt defines the northern limit of the evolving suture between Arabia and Eurasia and comprises two parallel b

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Koepke, J., J. Berndt, I. Horn, J. Fahle, and P. E. Wolff. "Partial melting of oceanic gabbro triggered by migrating water-rich fluids: a prime example from the Oman Ophiolite." Geological Society, London, Special Publications 392, no. 1 (2014): 195–212. http://dx.doi.org/10.1144/sp392.10.

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Rajendran, Sankaran, and Sobhi Nasir. "Recognition of Minerals Using Multispectral Remote Sensing Data: A Case Study in the Sultanate of Oman." Sultan Qaboos University Journal for Science [SQUJS] 19, no. 2 (2015): 37. http://dx.doi.org/10.24200/squjs.vol19iss2pp37-52.

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The present study demonstrates the capability of a multispectral sensor for the detection of the minerals in the rocks surrounding the Rusayl and Al Jafnayn regions, Sultanate of Oman. The study of spectral absorptions of rocks and minerals in the visible and near infrared (VNIR) and short wavelength infrared (SWIR) spectral bands of the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) using the Spectral Angle Mapper (SAM) supervised image classification technique has provided information on the occurrence of minerals in the rock types of the regions. The study shows the

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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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Kelemen, Peter B., Ken Koga, and Nobu Shimizu. "Geochemistry of gabbro sills in the crust-mantle transition zone of the Oman ophiolite: implications for the origin of the oceanic lower crust." Earth and Planetary Science Letters 146, no. 3-4 (1997): 475–88. http://dx.doi.org/10.1016/s0012-821x(96)00235-x.

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Dissertations / Theses on the topic "Gabbro – Oman"

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Python, Marie. "Nature et répartition des filons basiques dans la section mantellaire de l'ophiolite d'Oman : implications pour la genèse des MORBs." Toulouse 3, 2002. https://tel.archives-ouvertes.fr/tel-00010212.

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Lamoureux, Gwenae͏̈lle. "Structure des gabbros de l'ophiolite d'Oman : caractérisation physique des chambres magmatiques des dorsales océaniques rapides." Montpellier 2, 1999. http://www.theses.fr/1999MON20104.

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Les etudes structurales anterieures dans l'ophiolite d'oman ont mis en evidence une chambre magmatique permanente et continue le long de l'axe des dorsales oceaniques rapides (nicolas et al. , 1996). Les campagnes sismiques realisees sur la dorsale est-pacifique ont permis de deceler une lentille liquide surplombee d'une zone a faible vitesse sismique (lvz) (wilcock et al. , 1995). L'objectif de ce travail est d'effectuer un inventaire detaille des microstructures et petrofabriques des gabbros d'oman, de contraindre la fraction de magma presente dans la lvz et de preciser le mode de circulatio

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Dewandel, Benoît. "Structure et fonctionnement hydrogéologique d'un aquifère discontinu : l'ophiolite d'Oman." Montpellier 2, 2002. http://www.theses.fr/2002MON20023.

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Einaudi, Florence. "Analyse de séquences magmatiques océaniques continues : approche pétrophysique et géochimique." Aix-Marseille 3, 2002. http://www.theses.fr/2002AIX30044.

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Cette thèse présente les résultats de l'étude de deux séquences magmatiques continues. La première est une section de laves de l'ophiolite d'Oman. Cette séquence a été étudiée en termes de propriétés physiques, pétrologie et géochimie afin d'accéder à l'évolution temporelle des laves à l'axe de la paléographe omanaise, décrite comme étant rapide. Ces mesures ont montré la présence de cinq cycles magmatiques. La composante temporelle adoptée dans ce travail a permis l'étude des processus volcaniques depuis l'extraction des magmas jusqu'à l'échelle du cycle volcanique. La seconde section continu

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Meyer, Matthew Charles. "Magnetic fabric, palaeomagnetic and structural investigation of the accretion of lower oceanic crust using ophiolitic analogues." Thesis, University of Plymouth, 2016. http://hdl.handle.net/10026.1/5022.

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This thesis presents the results of a combined magnetic fabric and palaeomagnetic analysis of lower crustal rocks exposed in the Oman (Semail) ophiolite. This has long been an important natural laboratory for understanding the construction of oceanic crust at fast spreading axes and its subsequent tectonic evolution, but magnetic investigations in the ophiolite have been limited. Analyses presented here involve using: (i) magnetic anisotropies as a proxy for magmatic petrofabrics in lower crustal rocks in order to contribute to outstanding questions regarding the mode of accretion of fast-spre

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Trutner, Sarah D. "An Investigation of AMS in Oman Ophiolite Gabbros." Oberlin College Honors Theses / OhioLINK, 2016. http://rave.ohiolink.edu/etdc/view?acc_num=oberlin1470493515.

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Lamour, Marianne. "Étude géochimique et pétrologique des filons intrusifs dans les Gabbros de l'ophiolite d'Oman : rôle et origine des fluides de très haute température." Montpellier 2, 2005. http://www.theses.fr/2005MON20176.

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Madi, Atman. "Géologie de la partie nord de l'ophiolite d'Oman : pétrologie et géochimie de la séquence plutonique du massif de Fizh." Phd thesis, Grenoble 1, 1995. http://www.theses.fr/1995GRE10061.

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La séquence plutonique du massif de Fizh (partie nord de l'ophiolite d'Oman) offre une complexité crustale, liée à une diversité des corps magmatiques et du système filonien. La cartographie détaillée montre une succession d'événements magmatiques dont les séries principales sont formées de gabbros lités, des wehrlites et pyroxénites, des gabbronorites. Le magmatisme gabbroïque est généré dans une grande chambre magmatique axiale, alors que le magmatisme wehrlitique est dit hors-axe ; ceci est conditionné par la segmentation axiale de la paléodorsale. L'asymétrie ainsi observée dans la séquenc

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9

Wolff, Paul Eric [Verfasser]. "Hydrothermal circulation from very high to low temperatures in the lower oceanic crust : evidence from layered gabbros from the Oman ophiolite and from partial melting experiments on oceanic gabbros / Paul Eric Wolff." Hannover : Technische Informationsbibliothek und Universitätsbibliothek Hannover (TIB), 2014. http://d-nb.info/1059517434/34.

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Gaber, Abdo Nasser Ali Verfasser], Abbas S. [Akademischer Betreuer] Omar, and Christian [Akademischer Betreuer] [Diedrich. "Wireless indoor positioning based on TDOA and DOA estimation techniques using IEEE 802.11 standards / Abdo Nasser Ali Gaber. Betreuer: Abbas S. Omar ; Christian Diedrich." Magdeburg : Universitätsbibliothek, 2015. http://d-nb.info/1072146673/34.

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Book chapters on the topic "Gabbro – Oman"

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Lachize, M., J. P. Lorand, and T. Juteau. "Cu-Ni-PGE Magmatic Sulfide Ores and their Host Layered Gabbros in the Haymiliyah Fossil Magma Chamber (Haylayn Block, Semail Ophiolite Nappe, Oman)." In Ophiolite Genesis and Evolution of the Oceanic Lithosphere. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3358-6_12.

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Conference papers on the topic "Gabbro – Oman"

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Horst, Andrew J., Sarah Trutner, Elena Sohn Hartley, and Joe Martin. "DEVELOPMENT OF FOLIATION IN UPPERMOST GABBROS IN THE OMAN OPHIOLITE AND IMPLICATIONS FOR CRUSTAL ACCRETION ALONG A PALEORIDGE AXIS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-288053.

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