Watch the Dallas Symposium LIVE, and fundraiser auction
Ticket proceeds support mindat.org! - click here...
Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Arai, Shoji, Miura, Makoto (2016) Reply to the comment of rollinson and adetunji “podiform chromitites do form beneath mid-ocean ridges” by Arai, S. And Miura, M. Lithos, 254. 134-136 doi:10.1016/j.lithos.2016.03.004

Advanced
   -   Only viewable:
Reference TypeJournal (article/letter/editorial)
TitleReply to the comment of rollinson and adetunji “podiform chromitites do form beneath mid-ocean ridges” by Arai, S. And Miura, M
JournalLithos
AuthorsArai, ShojiAuthor
Miura, MakotoAuthor
Year2016 (June)Volume254
PublisherElsevier BV
DOIdoi:10.1016/j.lithos.2016.03.004Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID275957Long-form Identifiermindat:1:5:275957:3
GUID0
Full ReferenceArai, Shoji, Miura, Makoto (2016) Reply to the comment of rollinson and adetunji “podiform chromitites do form beneath mid-ocean ridges” by Arai, S. And Miura, M. Lithos, 254. 134-136 doi:10.1016/j.lithos.2016.03.004
Plain TextArai, Shoji, Miura, Makoto (2016) Reply to the comment of rollinson and adetunji “podiform chromitites do form beneath mid-ocean ridges” by Arai, S. And Miura, M. Lithos, 254. 134-136 doi:10.1016/j.lithos.2016.03.004
In(2016) Lithos Vol. 254. Elsevier BV

See Also

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

Rollinson, Hugh, Adetunji, Jacob (2016) Comment on ‘Podiform chromitites do form beneath mid-ocean ridges’ by Arai, S. and Miura, M. Lithos, 254. 131-133 doi:10.1016/j.lithos.2015.10.023
Arai, Shoji, Miura, Makoto (2015) Podiform chromitites do form beneath mid-ocean ridges. Lithos, 232. 143-149 doi:10.1016/j.lithos.2015.06.015
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
Arai, Shoji, Miura, Makoto (2016) Formation and modification of chromitites in the mantle. Lithos, 264. 277-295 doi:10.1016/j.lithos.2016.08.039
Arai, Shoji, Hoshikawa, Chihiro, Miura, Makoto, Ando, Jun-ichi, Ishimaru, Satoko, Mochizuki, Nobutatsu, Tamura, Akihiro (2021) Dehydrogenation of deep-seated hydrous olivine in “black-colored” dunites of arc origin. Lithos, 384. 105967pp. doi:10.1016/j.lithos.2021.105967
Sanfilippo, Alessio, Morishita, Tomoaki, Kumagai, Hidenori, Nakamura, Kentaro, Okino, Kyoko, Hara, Kaori, Tamura, Akihiro, Arai, Shoji (2015) Hybrid troctolites from mid-ocean ridges: inherited mantle in the lower crust. Lithos, 232. 124-130 doi:10.1016/j.lithos.2015.06.025
Arai, Shoji, Miura, Makoto, Tamura, Akihiro, Akizawa, Norikatsu, Ishikawa, Akira (2020) Hydrothermal Chromitites from the Oman Ophiolite: The Role of Water in Chromitite Genesis. Minerals, 10 (3) 217 doi:10.3390/min10030217
Miura, Makoto, Arai, Shoji, Mizukami, Tomoyuki, Shmelev, Vladimir, Ishimaru, Satoko (2018) Petrology of Chromitites in the Higashi-Akaishi Ultrahigh-Pressure (UHP) Peridotite Complex, Japan: Toward Understanding of General Features of the UHP Chromitites. Minerals, 8 (11) 525 doi:10.3390/min8110525
Arai, Shoji (2021) Genetic Link between Podiform Chromitites in the Mantle and Stratiform Chromitites in the Crust: A Hypothesis. Minerals, 11 (2) 209 doi:10.3390/min11020209
Miura, Makoto, Shoji Arai, Tomoyuki Mizukami, Vladimir R. Shmelev, and Satoko Ishimaru. (2018) "Petrology of Chromitites in the Higashi-Akaishi Ultrahigh-Pressure (UHP) Peridotite Complex, Japan: Toward Understanding of General Features of the UHP Chromitites" Minerals 8, no. 11: 525. https://doi.org/10.3390/min8110525
Khedr, Mohamed Zaki, Arai, Shoji (2016) Chemical variations of mineral inclusions in Neoproterozoic high-Cr chromitites from Egypt: Evidence of fluids during chromitite genesis. Lithos, 240. 309-326 doi:10.1016/j.lithos.2015.11.029
 
and/or  
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: August 19, 2025 05:12:25
Go to top of page