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Miyashita, S., Adachi, Y., Neo, N., Tomatsu, T., & Tanaka, S. Large chloritite bodies found in the upper gabbro unit of the Oman ophiolite: New aspect for the hydrothermal systems beneath ocean ridges.

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Original EntryMiyashita, S., Adachi, Y., Neo, N., Tomatsu, T., & Tanaka, S. Large chloritite bodies found in the upper gabbro unit of the Oman ophiolite: New aspect for the hydrothermal systems beneath ocean ridges.
Mindat Ref. ID16059432Long-form Identifiermindat:1:5:16059432:0
GUID0
Full ReferenceMiyashita, S., Adachi, Y., Neo, N., Tomatsu, T., & Tanaka, S. Large chloritite bodies found in the upper gabbro unit of the Oman ophiolite: New aspect for the hydrothermal systems beneath ocean ridges.
Plain TextMiyashita, S., Adachi, Y., Neo, N., Tomatsu, T., & Tanaka, S. Large chloritite bodies found in the upper gabbro unit of the Oman ophiolite: New aspect for the hydrothermal systems beneath ocean ridges.

Map of Localities

Mineral Occurrences

LocalityMineral(s)
Wadi Hilti, Northern Oman Ophiolite, Al Buraimi Governorate, Omanβ“˜ Actinolite, β“˜ Anatase, β“˜ Apatite, β“˜ Brunsvigite, β“˜ Calcite, β“˜ Chlorite Group, β“˜ Clinochlore, β“˜ Epidote, β“˜ Magnetite, β“˜ Prehnite, β“˜ Ripidolite, β“˜ Rutile, β“˜ Serpentine Subgroup, β“˜ Talc, β“˜ Titanite

See Also

These are possibly similar items as determined by title/reference text matching only.

Kusano, Yuki, Adachi, Yoshiko, Miyashita, Sumio, Umino, Susumu (2012) Lava accretion system around mid-ocean ridges: Volcanic stratigraphy in the Wadi Fizh area, northern Oman ophiolite. Geochemistry Geophysics Geosystems, 13. doi:10.1029/2011gc004006
Adachi, Yoshiko, Tomatsu, Takashi, Okazawa, Shiki, Miyashita, Sumio (2002) Layering structures of gabbros of the Oman ophiolite. The Journal of the Geological Society of Japan, 108 (8) doi:10.5575/geosoc.108.xvii
Miyashita, Sumio, Umino, Susumu, Adachi, Yoshiko (2002) A new perspective of ophiolite studies with special reference to the Oman ophiolite. The Journal of the Geological Society of Japan, 108 (8) 520-535 doi:10.5575/geosoc.108.520
Rollinson, Hugh, Adetunji, Jacob (2013) Mantle podiform chromitites do not form beneath mid-ocean ridges: A case study from the Moho transition zone of the Oman ophiolite. Lithos, 177. 314-327 doi:10.1016/j.lithos.2013.07.004
Tsuchiya, Nobutaka, Shibata, Tomoyuki, Yoshikawa, Masako, Adachi, Yoshiko, Miyashita, Sumio, Adachi, Tatsurou, Nakano, Nobuhiko, Osanai, Yasuhito (2013) Petrology of Lasail plutonic complex, northern Oman ophiolite, Oman: An example of arc-like magmatism associated with ophiolite detachment. Lithos, 156. 120-138 doi:10.1016/j.lithos.2012.10.013
Gregory, Robert T., Taylor, Hugh P. (1981) An oxygen isotope profile in a section of Cretaceous oceanic crust, Samail Ophiolite, Oman: Evidence for Ξ΄18O buffering of the oceans by deep (>5 km) seawater-hydrothermal circulation at mid-ocean ridges. Journal of Geophysical Research: Solid Earth, 86. 2737-2755 doi:10.1029/jb086ib04p02737
Miyashita, Sumio, Adachi, Yoshiko, Umino, Susumu (2003) Along-axis magmatic system in the northern Oman ophiolite: Implications of compositional variation of the sheeted dike complex. Geochemistry, Geophysics, Geosystems, 4 (9) doi:10.1029/2001gc000235
Arai, S., Akizawa, N. (2014) Precipitation and dissolution of chromite by hydrothermal solutions in the Oman ophiolite: New behavior of Cr and chromite. American Mineralogist, 99 (1) 28-34 doi:10.2138/am.2014.4473
Adachi, Yoshiko, Miyashita, Sumio (2003) Geology and petrology of the plutonic complexes in the Wadi Fizh area: Multiple magmatic events and segment structure in the northern Oman ophiolite. Geochemistry, Geophysics, Geosystems, 4 (9) doi:10.1029/2001gc000272
Haymon, R. M., Koski, R. A., & Abrams, M. J. (1989). Hydrothermal discharge zones beneath massive sulfide deposits mapped in the Oman ophiolite. Geology, 17(6), 531-535.
Silantyev, S. A., Aranovich, L. Ya., Bortnikov, N. S. (2010) Oceanic plagiogranites as a result of interaction between magmatic and hydrothermal systems in the slow-spreading mid-ocean ridges. Petrology, 18 (4) 369-383 doi:10.1134/s0869591110040041
 
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