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Makoto Miura and Shoji Arai (2014) Platinum-group Element and Mineral Characteristics of Sub-arc Chromitite Xenoliths from the Takashima Alkali Basalt, Southwest Japan Arc. Can Mineral 52:899-916

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Year2014
Original EntryMakoto Miura and Shoji Arai (2014) Platinum-group Element and Mineral Characteristics of Sub-arc Chromitite Xenoliths from the Takashima Alkali Basalt, Southwest Japan Arc. Can Mineral 52:899-916
Mindat Ref. ID16058862Long-form Identifiermindat:1:5:16058862:6
GUID0
Full ReferenceMakoto Miura and Shoji Arai (2014) Platinum-group Element and Mineral Characteristics of Sub-arc Chromitite Xenoliths from the Takashima Alkali Basalt, Southwest Japan Arc. Can Mineral 52:899-916
Plain TextMakoto Miura and Shoji Arai (2014) Platinum-group Element and Mineral Characteristics of Sub-arc Chromitite Xenoliths from the Takashima Alkali Basalt, Southwest Japan Arc. Can Mineral 52:899-916

Locality Pages

LocalityCitation Details
Takashima islet, Karatsu City, Saga Prefecture, Japan

Mineral Occurrences

LocalityMineral(s)
Takashima islet, Karatsu City, Saga Prefecture, Japanⓘ Chromite, ⓘ Laurite, ⓘ Pentlandite, ⓘ Spinel

See Also

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

Miura, Makoto, Arai, Shoji (2014) PLATINUM-GROUP ELEMENT AND MINERAL CHARACTERISTICS OF SUB-ARC CHROMITITE XENOLITHS FROM THE TAKASHIMA ALKALI BASALT, SOUTHWEST JAPAN ARC. The Canadian Mineralogist, 52 (5) 899-916 doi:10.3749/canmin.1300049
Arai, S., Abe, N. (1994) Podiform chromitite in the arc mantle: chromitite xenoliths from the Takashima alkali basalt, Southwest Japan arc. Mineralium Deposita, 29 (5) 434-438 doi:10.1007/bf01886963
MUROI, Ritsuko, ARAI, Shoji (2014) Formation process of olivine–clinopyroxene cumulates inferred from Takashima xenoliths, Southwest Japan arc. Journal of Mineralogical and Petrological Sciences, 109 (2) 79-84 doi:10.2465/jmps.131003
MIURA, Makoto, ARAI, Shoji, TAMURA, Akihiro (2014) Formation of discordant chromitite at the initiation of sub-arc mantle processes: Observations from the northern Oman ophiolite. Journal of Mineralogical and Petrological Sciences, 109 (1) 38-43 doi:10.2465/jmps.131006
ARAI, Shoji, HIRAI, Hisatoshi, UTO, Kozo (2000) Mantle peridotite xenoliths from the Southwest Japan arc. A model for the sub-arc upper mantle structure and composition of the Western Pacific rim. Journal of Mineralogical and Petrological Sciences, 95 (4) 9-23 doi:10.2465/jmps.95.9
Arai, Shoji, Akihiro Tamura, Makoto Miura, and Kazuma Seike. (2018) "Abyssal Peridotite as a Component of Forearc Mantle: Inference from a New Mantle Xenolith Suite of Bankawa in the Southwest Japan Arc" Minerals 8, no. 11: 540. https://doi.org/10.3390/min8110540
Arai, Shoji, Tamura, Akihiro, Miura, Makoto, Seike, Kazuma (2018) Abyssal Peridotite as a Component of Forearc Mantle: Inference from a New Mantle Xenolith Suite of Bankawa in the Southwest Japan Arc. Minerals, 8 (11) 540 doi:10.3390/min8110540
ARAI, Shoji, MURAOKA, Hiroyasu (1992) Peridotite xenoliths in alkali basalts from On-yama, the Chugoku district, as a suite of fertile upper mantle peridotites beneath the Southwest Japan arc. Journal of Mineralogy, Petrology and Economic Geology, 87 (6) 240-250 doi:10.2465/ganko.87.240
Ishimaru, Satoko, Arai, Shoji (2009) Highly silicic glasses in peridotite xenoliths from Avacha volcano, Kamchatka arc; implications for melting and metasomatism within the sub-arc mantle. Lithos, 107 (1) 93-106 doi:10.1016/j.lithos.2008.07.005
Arai, Shoji; Tamura, Akihiro; Miura, Makoto; Morishita, Tomoaki (2022) Origin of spinel-hosted mineral inclusions in mantle peridotite from Setogawa in the Circum-Izu Massif Serpentine Belt, central Japan: Implications for the chromitite genesis. Ore Geology Reviews, 140. doi:10.1016/j.oregeorev.2021.104422
Tamura, Akihiro, Arai, Shoji, Takeuchi, Miyuki, Miura, Makoto, Pirnia, Tahmineh (2019) Compositional heterogeneity of a websterite xenolith from Kurose, southwest Japan: insights into the evolution of lower crust beneath the Japan Arc. European Journal of Mineralogy, 31 (1) 35-47 doi:10.1127/ejm/2018/0030-2803
 
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