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Journal articles on the topic 'Oman ophiolite'

Author: Grafiati

Published: 4 June 2021

Last updated: 8 June 2024

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1

Ibragimov, Iskander, Daniel Kiss, and Evangelos Moulas. "A thermo-mechanical model of the thermal evolution and incorporation of metamorphic soles in Tethyan ophiolites: a case study from Oman." Austrian Journal of Earth Sciences 117, no. 1 (2024): 13–24. http://dx.doi.org/10.17738/ajes.2024.0002.

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Abstract Ophiolites are remnants of oceanic crust and mantle, now typically found within continental mountain ranges like the Alps. Particularly in areas once part of the Tethys Ocean, ophiolites are often accompanied by narrow stripes of metamorphic rocks, commonly referred to as metamorphic soles. These metamorphic soles typically exhibit peak metamorphic conditions characteristic of either granulite or amphibolite facies. Geochronological studies of Tethyan ophiolites indicate that the development of these metamorphic soles occurred almost simultaneously with the crystallization of the ophi

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2

UMINO, Susumu, Shuichi YANAI, Yasuo NAKAMURA, and J. Toshimichi IIYAMA. "Semail Ophiolite in Oman." Journal of Geography (Chigaku Zasshi) 98, no. 3 (1989): plate1—plate3. http://dx.doi.org/10.5026/jgeography/98.3_plate1.

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3

IMMENHAUSER, ADRIAN, GUIDO SCHREURS, EDWIN GNOS, HEIKO W. OTERDOOM, and BERNHARD HARTMANN. "Late Palaeozoic to Neogene geodynamic evolution of the northeastern Oman margin." Geological Magazine 137, no. 1 (2000): 1–18. http://dx.doi.org/10.1017/s0016756800003526.

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When the highlands of Arabia were still covered with an ice shield in the latest Carboniferous/Early Permian period, separation of Gondwana started. This led to the creation of the Batain basin (part of the early Indian Ocean), off the northeastern margin of Oman. The rifting reactivated an Infra-Cambrian rift shoulder along the northeastern Oman margin and detritus from this high was shed into the interior Oman basin. Whereas carbonate platform deposits became widespread along the margin of the Neo-Tethys (northern rim of Oman), drifting and oceanization of the Batain basin started only in La

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4

Olsson, J., S. L. S. Stipp, and S. R. Gislason. "Element scavenging by recently formed travertine deposits in the alkaline springs from the Oman Semail Ophiolite." Mineralogical Magazine 78, no. 6 (2014): 1479–90. http://dx.doi.org/10.1180/minmag.2014.078.6.15.

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Ultramafic rocks, such as the Semail Ophiolite in the Sultanate of Oman, are considered to be a potential storage site for CO2. This type of rock is rich in divalent cations that can react with dissolved CO2 and form carbonate minerals, which remain stable over geological periods of time. Dissolution of the ophiolite mobilizes heavy metals, which can threaten the safety of surface and groundwater supplies but secondary phases, such as iron oxides, clays and carbonate minerals, can take up significant quantities of trace elements both in their structure and adsorbed on their surfaces.Hyperalkal

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5

Abbou-Kebir, Khadidja, Shoji Arai, Ahmed Hassan Ahmed, and Georges Ceuleneer. "Spinel-free and spinel-poor dunite veins crosscutting the Wadi Rajmi ophiolite chromitite (northern Oman ophiolite)." Bulletin de la Société Géologique de France 184, no. 3 (2013): 261–66. http://dx.doi.org/10.2113/gssgfbull.184.3.261.

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Abstract Peculiar dunitic veins almost or totally free of spinels crosscut a podiform chromitite ore body in the Wadi Rajmi, northern Oman ophiolite. They probably originated from a komatiitic melt which was oversaturated in Fo≤94 olivines and which evolved to precipitate simultaneously both chromian spinels, with Cr# ranging from 0.6 to 0.8, and Fo91-93 olivines. The absence or the low modal amounts of spinels are possibly governed by a Cr-undersaturation state of the involved melt which crystallized under relatively low cooling rates to generate the spinel-free and the spinel-poor dunites. A

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6

Scharf, A., F. Mattern, M. Al-Wardi, et al. "About this title - The Geology and Tectonics of the Jabal Akhdar and Saih Hatat Domes, Oman Mountains." Geological Society, London, Memoirs 54, no. 1 (2021): NP. http://dx.doi.org/10.1144/m54.

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The geology of the Oman Mountains, including the Jabal Akhdar and Saih Hatat domes, is extraordinarily well-exposed and diverse, spanning a geological record of more than 800 Ma. The area is blessed with first-class outcrops and is well known in the geological community for its ophiolite. The Oman Mountains have much more to offer; including, Neoproterozoic diamictites (“Snowball Earth”), fossil-rich Permo-Mesozoic carbonates and metamorphic rocks. The arid climate and deep incision of wadis allow for nearly complete rock exposure which can be investigated in all three dimensions. The diverse

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7

Nicolas, A., and F. Boudier. "Mapping oceanic ridge segments in Oman ophiolite." Journal of Geophysical Research: Solid Earth 100, B4 (1995): 6179–97. http://dx.doi.org/10.1029/94jb01188.

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8

ROLLINSON, Hugh, and Jacob ADETUNJI. "Chromite in the Mantle Section of the Oman Ophiolite: Implications for the Tectonic Evolution of the Oman Ophiolite." Acta Geologica Sinica - English Edition 89, s2 (2015): 73–76. http://dx.doi.org/10.1111/1755-6724.12308_44.

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9

SAVELYEVA, G. N., and V. G. BATANOVA. "Chromite in the Mantle Section of the Oman Ophiolite: Implications for the Tectonic Evolution of the Oman Ophiolite." Acta Geologica Sinica - English Edition 89, s2 (2015): 77–78. http://dx.doi.org/10.1111/1755-6724.12308_45.

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10

Tsuchiya, Nobutaka, Tomoyuki Shibata, Masako Yoshikawa, et al. "Petrology of Lasail plutonic complex, northern Oman ophiolite, Oman: An example of arc-like magmatism associated with ophiolite detachment." Lithos 156-159 (January 2013): 120–38. http://dx.doi.org/10.1016/j.lithos.2012.10.013.

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11

SEARLE, MICHAEL P., and JON COX. "Subduction zone metamorphism during formation and emplacement of the Semail ophiolite in the Oman Mountains." Geological Magazine 139, no. 3 (2002): 241–55. http://dx.doi.org/10.1017/s0016756802006532.

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The metamorphic sole along the base of the Semail ophiolite in Oman records the earliest thrust slice subducted and accreted to the base of the ophiolite mantle sequence. In the Bani Hamid area (United Arab Emirates) a c. 870 m thick thrust slice of granulite facies rocks includes garnet+ diopside amphibolites, enstatite+cordierite+sillimanite+spinel±sapphirine quartzites, alkaline mafic granulites (meta-jacupirangites) quartzo-feldspathic gneisses and calc-silicates. The latter contain garnet+diopside+scapolite+plagioclase±wollastonite. P–T conditions of granulite facies metamorphism are in t

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12

Miyashita, Sumio, Susumu Umino, and Yoshiko Adachi. "A new perspective of ophiolite studies with special reference to the Oman ophiolite." Journal of the Geological Society of Japan 108, no. 8 (2002): 520–35. http://dx.doi.org/10.5575/geosoc.108.520.

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13

Adachi, Yoshiko, Takashi Tomatsu, Shiki Okazawa, and Sumio Miyashita. "Layering structures of gabbros of the Oman ophiolite." Journal of the Geological Society of Japan 108, no. 8 (2002): XVII—XVIII. http://dx.doi.org/10.5575/geosoc.108.xvii.

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14

UMINO, Susumu. "Geology of the Semail Ophiolite, Northern Oman Mountains." Journal of Geography (Chigaku Zasshi) 104, no. 3 (1995): 321–49. http://dx.doi.org/10.5026/jgeography.104.3_321.

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15

YANAI, Shuichi, Susumu UMINO, Yasuo NAKAMURA, and J. Toshimichi IIYAMA. "Stress Structure of Semail Ophiolite, Northern Oman Mountains." Journal of Geography (Chigaku Zasshi) 98, no. 3 (1989): 279–89. http://dx.doi.org/10.5026/jgeography.98.3_279.

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16

Rollinson, Hugh. "A (virtual) field excursion through the Oman ophiolite." Geology Today 30, no. 3 (2014): 110–18. http://dx.doi.org/10.1111/gto.12055.

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17

Gass, Ian G., Stephen J. Lippard, and Anthony W. Shelton. "Ophiolite in the Oman: The Open University Project." Episodes 8, no. 1 (1985): 13–20. http://dx.doi.org/10.18814/epiiugs/1985/v8i1/002.

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18

Coogan, Laurence A. "Contaminating the lower crust in the Oman ophiolite." Geology 31, no. 12 (2003): 1065. http://dx.doi.org/10.1130/g20129.1.

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19

Boudier, F., A. Nicolas, B. Ildefonse, and D. Jousselin. "EPR microplates, a model for the Oman Ophiolite." Terra Nova 9, no. 2 (1997): 79–82. http://dx.doi.org/10.1111/j.1365-3121.1997.tb00007.x.

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20

Scharf, Andreas, Frank Mattern, Mohammed Al-Wardi, et al. "Chapter 5 Tectonic evolution of the Oman Mountains." Geological Society, London, Memoirs 54, no. 1 (2021): 67–103. http://dx.doi.org/10.1144/m54.5.

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AbstractThe tectonic evolution of the Oman Mountains as of the Neoproterozoic begins with a major extensional event, the Neoproterozoic Abu Mahara rifting. It was followed by the compressional Nabitah event, still during the Neoproterozoic, in Oman but possibly not in the study area. During the earliest Cambrian, the Jabal Akhdar area was affected by the Cadomian Orogeny, marked by NE--SW shortening. It is unclear, whether the Saih Hatat area was exposed to the Cadomian deformation, too. Still during the lower Cambrian, the Angudan Orogeny followed, characterized by NW--SE shortening. An episo

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21

Braathen, Alvar, and Per Terje Osmundsen. "Extensional tectonics rooted in orogenic collapse: Long-lived disintegration of the Semail Ophiolite, Oman." Geology 48, no. 3 (2019): 258–62. http://dx.doi.org/10.1130/g47077.1.

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Abstract Significant post-orogenic extension of the renowned Semail Ophiolite and substrata in Oman resulted in the formation of metamorphic core complexes juxtaposed with an array of Maastrichtian-Paleogene extensional basins. During this evolution, basins became progressively localized. The geometry of the large-scale and long-lived extensional system changes laterally across the core complexes and reveals several generations of domes and detachments, some of which were progressively exhumed. Progressive excision and dismemberment of the ophiolite link to major fabrics in the core complexes

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22

Belgrano, Thomas M., Larryn W. Diamond, Yves Vogt, Andrea R. Biedermann, Samuel A. Gilgen, and Khalid Al-Tobi. "A revised map of volcanic units in the Oman ophiolite: insights into the architecture of an oceanic proto-arc volcanic sequence." Solid Earth 10, no. 4 (2019): 1181–217. http://dx.doi.org/10.5194/se-10-1181-2019.

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Abstract. Numerous studies have revealed genetic similarities between Tethyan ophiolites and oceanic “proto-arc” sequences formed above nascent subduction zones. The Semail ophiolite (Oman–U.A.E.) in particular can be viewed as an analogue for this proto-arc crust. Though proto-arc magmatism and the mechanisms of subduction initiation are of great interest, insight is difficult to gain from drilling and limited surface outcrops in marine settings. In contrast, the 3–5 km thick upper-crustal succession of the Semail ophiolite, which is exposed in an oblique cross section, presents an opportunit

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23

Perez, Americus, Susumu Umino, Graciano P. Yumul Jr., and Osamu Ishizuka. "Boninite and boninite-series volcanics in northern Zambales ophiolite: doubly vergent subduction initiation along Philippine Sea plate margins." Solid Earth 9, no. 3 (2018): 713–33. http://dx.doi.org/10.5194/se-9-713-2018.

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Abstract. A key component of subduction initiation rock suites is boninite, a high-magnesium andesite that is uniquely predominant in western Pacific forearc terranes and in select Tethyan ophiolites such as Oman and Troodos. We report, for the first time, the discovery of low-calcium, high-silica boninite in the middle Eocene Zambales ophiolite (Luzon Island, Philippines). Olivine–orthopyroxene microphyric high-silica boninite, olivine–clinopyroxene–phyric low-silica boninite and boninitic basalt occur as lapilli fall deposits and pillow lava flows in the upper volcanic unit of the juvenile a

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24

Searle, Michael P., Alan G. Cherry, Mohammed Y. Ali, and David J. W. Cooper. "Tectonics of the Musandam Peninsula and northern Oman Mountains: From ophiolite obduction to continental collision." GeoArabia 19, no. 2 (2014): 135–74. http://dx.doi.org/10.2113/geoarabia1902137.

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ABSTRACT The tectonics of the Musandam Peninsula in northern Oman shows a transition between the Late Cretaceous ophiolite emplacement related tectonics recorded along the Oman Mountains and Dibba Zone to the SE and the Late Cenozoic continent-continent collision tectonics along the Zagros Mountains in Iran to the northwest. Three stages in the continental collision process have been recognized. Stage one involves the emplacement of the Semail Ophiolite from NE to SW onto the Mid-Permian–Mesozoic passive continental margin of Arabia. The Semail Ophiolite shows a lower ocean ridge axis suite of

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25

KIKAWA, Eiichi, Hideo SAKAI, and Tomoyuki KUDO. "Magnetization of Upper Mantle: Results from Oman Samail Ophiolite." Journal of Geography (Chigaku Zasshi) 112, no. 5 (2003): 720–31. http://dx.doi.org/10.5026/jgeography.112.5_720.

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26

MICHIBAYASHI, Katsuyoshi. "Distal View of “5 o'clock Moho” at Oman Ophiolite." Journal of Geography (Chigaku Zasshi) 112, no. 5 (2003): Plate1—Plate2. http://dx.doi.org/10.5026/jgeography.112.5_plate1.

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27

YANAI, Shuichi, Susumu UMINO, Yasuo NAKAMURA, and Toshimichi J. IIYAMA. "Obduction of Semail Ophiolite, Northern Oman Mountains-An Outline-." Journal of Geography (Chigaku Zasshi) 98, no. 4 (1989): 499–506. http://dx.doi.org/10.5026/jgeography.98.4_499.

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28

Chenevez, Jérôme, Philippe Machetel, and Adolphe Nicolas. "Numerical models of magma chambers in the Oman ophiolite." Journal of Geophysical Research: Solid Earth 103, B7 (1998): 15443–55. http://dx.doi.org/10.1029/98jb00597.

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29

Thiel, S., G. Heinson, D. R. Gray, and R. T. Gregory. "Ophiolite emplacement in NE Oman: constraints from magnetotelluric sounding." Geophysical Journal International 176, no. 3 (2009): 753–66. http://dx.doi.org/10.1111/j.1365-246x.2008.04053.x.

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30

Fones, Elizabeth M., Daniel R. Colman, Emily A. Kraus, et al. "Physiological adaptations to serpentinization in the Samail Ophiolite, Oman." ISME Journal 13, no. 7 (2019): 1750–62. http://dx.doi.org/10.1038/s41396-019-0391-2.

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31

A'Shaikh, Durair, Hiroharu Matsueda, Toshio Mizuta, and Sumio Miyashita. "Hydrothermal Alteration of Oman Ophiolite Extrusives in Ghuzayn Area." Resource Geology 56, no. 2 (2006): 167–82. http://dx.doi.org/10.1111/j.1751-3928.2006.tb00277.x.

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32

Kelemen, Peter. "Planning the Drilling of the Samail Ophiolite in Oman." Eos, Transactions American Geophysical Union 94, no. 3 (2013): 32. http://dx.doi.org/10.1002/2013eo030008.

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33

Moseley, F. "The upper cretaceous ophiolite complex of Masirah Island, Oman." Geological Journal 6, no. 2 (2007): 293–306. http://dx.doi.org/10.1002/gj.3350060211.

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34

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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35

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 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 us

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36

Abdalla, O., A. Izady, T. Al-Hosni, M. Chen, H. Al-Mamari, and K. Semhi. "Modern Recharge in a Transboundary Groundwater Basin Deduced from Hydrochemical and Isotopic Investigations: Al Buraimi, Oman." Geofluids 2018 (September 12, 2018): 1–14. http://dx.doi.org/10.1155/2018/7593430.

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Groundwater samples (54) collected from different geological units (alluvium, Tertiary, ophiolite, and Hawasina) located in the transboundary groundwater basin in north Oman at the United Arab Emirates (UAE) borders were analyzed for general hydrochemistry and water isotopes, and subsets thereof were analyzed for 14C and 3H and 87Sr/86Sr. The chemical composition, percentage of modern carbon (pmc), δ2H, δ18O, and 87Sr/86Sr of the groundwater in the study area progressively change from the recharge zone in the elevated area of the North Oman Mountains (NOM) to the flat plains at the UAE borders

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37

Cooper, David J. W., Michael P. Searle, and Mohammed Y. Ali. "Structural evolution of Jabal Qumayrah: A salt-intruded culmination in the northern Oman Mountains." GeoArabia 17, no. 2 (2012): 121–50. http://dx.doi.org/10.2113/geoarabia1702121.

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ABSTRACT The Jabal Qumayrah area of the northern Oman Mountains records the evolution and subsequent destruction of a Mesozoic passive continental margin in the Oman segment of the Neo-Tethys Ocean, followed by the re-establishment of a passive margin, punctuated by phases of Tertiary compression. Almost uniquely along the Oman Mountains, it also contains intrusions of salt. Detachment of oceanic sediments and volcanics during the early phases of NE-directed subduction beneath the nascent Semail Ophiolite created an in-sequence stack of imbricated thrust units comprising distal trench units (H

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38

Scharf, Andreas, Frank Mattern, Mohammed Al-Wardi, et al. "Chapter 2 Tectonostratigraphy of the eastern part of the Oman Mountains." Geological Society, London, Memoirs 54, no. 1 (2021): 11–47. http://dx.doi.org/10.1144/m54.2.

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AbstractThis chapter provides comprehensive descriptions of 52 numbered formations/rock units of the Southeastern Oman Mountains, based on available literature. The oldest eight siliciclastic and carbonate formations are positioned below the ‘Hercynian’ Unconformity. The overlying formation (9–16) mostly represent carbonates which accumulated in a passive margin platform setting during or after the opening of the Neo-Tethys Ocean. The passive margin slope and platform collapsed during the late Cretaceous because of the obduction of the Semail Ophiolite along with the deep marine Hawasina sedim

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39

Ali, Mohammed Y., and A. B. Watts. "Subsidence history, gravity anomalies and flexure of the United Arab Emirates (UAE) foreland basin." GeoArabia 14, no. 2 (2009): 17–44. http://dx.doi.org/10.2113/geoarabia140217.

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ABSTRACT Seismic reflection profile, gravity anomaly, and exploratory well data have been used to determine the structure and evolution of the United Arab Emirates (UAE) foreland basin. The basin is of tectonic significance because it formed by ophiolite obduction in the northern Oman Mountains and flexural loading of an underlying Tethyan rifted margin. Existing stratigraphic data shows that this margin is characterised by an early syn-rift sequence of mainly Triassic age that is overlain by a post-rift sequence of Lower Jurassic to Upper Cretaceous age. Backstripping of the well data provide

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40

Augé, Thierry. "Platinum-group-mineral inclusions in chromitites from the Oman ophiolite." Bulletin de Minéralogie 109, no. 3 (1986): 301–4. http://dx.doi.org/10.3406/bulmi.1986.7937.

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41

Ahmed, A. H., and S. Arai. "PLATINUM-GROUP MINERALS IN PODIFORM CHROMITITES OF THE OMAN OPHIOLITE." Canadian Mineralogist 41, no. 3 (2003): 597–616. http://dx.doi.org/10.2113/gscanmin.41.3.597.

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42

SHIRAO, Motomaro. "Pictorial: The Samail Ophiolite, Oman: An ancient mid-oceanic ridge." Journal of Geography (Chigaku Zasshi) 108, no. 3 (1999): plate3—plate6. http://dx.doi.org/10.5026/jgeography/108.3_plate3.

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43

Mée, Laurent Le, Jacques Girardeau, and Christophe Monnier. "Mantle segmentation along the Oman ophiolite fossil mid-ocean ridge." Nature 432, no. 7014 (2004): 167–72. http://dx.doi.org/10.1038/nature03075.

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44

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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45

Jordan, Benjamin R., Abdel-Rahman Fowler, Bahaa El Dein Mahmoud, Ayman K. El-Saiy, and Osman Abdelghanny. "Peperites and associated pillow lavas subjacent to the Oman Ophiolite." Journal of Volcanology and Geothermal Research 173, no. 3-4 (2008): 303–12. http://dx.doi.org/10.1016/j.jvolgeores.2008.01.019.

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46

Oeser, Martin, Harald Strauss, Paul Eric Wolff, et al. "A profile of multiple sulfur isotopes through the Oman ophiolite." Chemical Geology 312-313 (June 2012): 27–46. http://dx.doi.org/10.1016/j.chemgeo.2012.04.008.

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47

Hacker, B. R., J. L. Mosenfelder, and E. Gnos. "Rapid emplacement of the Oman ophiolite: Thermal and geochronologic constraints." Tectonics 15, no. 6 (1996): 1230–47. http://dx.doi.org/10.1029/96tc01973.

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48

Pezard, Philippe A., Florence Einaudi, Daniel Hermitte, Jean-Jacques Cochemé, Christian Coulon, and Christine Laverne. "MORB emplacement and structure: Insights from the Semail Ophiolite, Oman." Geophysical Research Letters 27, no. 23 (2000): 3933–36. http://dx.doi.org/10.1029/2000gl011877.

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49

Kawahata, H., M. Nohara, H. Ishizuka, S. Hasebe, and H. Chiba. "Sr isotope geochemistry and hydrothermal alteration of the Oman ophiolite." Journal of Geophysical Research: Solid Earth 106, B6 (2001): 11083–99. http://dx.doi.org/10.1029/2000jb900456.

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50

Christiansen, F. G., and S. Roberts. "Formation of olivine pseudo-crescumulates by syntectonic axial planar growth during mantle deformation." Geological Magazine 123, no. 1 (1986): 73–79. http://dx.doi.org/10.1017/s0016756800026558.

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AbstractLarge elongated euhedral olivines, resembling olivines appearing in crescumulates, from dunite bodies of ophiolite mantle sequences have been subjected to a detailed structural and fabric study. Localities from the Semail Ophiolite, Oman and the Vourinos Complex, Greece are described. The studies indicate that the regional mantle flow structures control the shape and crystallographic orientation of the large euhedral olivines, which are elongated parallel to [001] and flattened parallel to (100) due to syntectonic high temperature metamorphic growth. The growth is controlled by the def

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