Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Kosuke Naemura"'
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-12 (2018)
Abstract The shallow oxidized asthenosphere may contain a small fraction of potassic silicate melts that are enriched in incompatible trace elements and volatiles. Here, to determine the chemical composition of such melt, we analysed fossilized melt
Externí odkaz:
https://doaj.org/article/9c44343b5e2049ae8d90e2c2d81bd833
Autor:
Choindonjamts Erdenejargal, Terbishiinkhen O. Javkhlan, Kosuke Naemura, Takao Hirajima, Takenori Kato
Publikováno v:
Journal of Mineralogical and Petrological Sciences. 115:357-364
Publikováno v:
Scientific Reports
Scientific Reports, Vol 10, Iss 1, Pp 1-1 (2020)
Scientific Reports, Vol 10, Iss 1, Pp 1-1 (2020)
The shallow oxidized asthenosphere may contain a small fraction of potassic silicate melts that are enriched in incompatible trace elements and volatiles. Here, to determine the chemical composition of such melt, we analysed fossilized melt inclusion
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-12 (2018)
Scientific Reports
Scientific Reports
The shallow oxidized asthenosphere may contain a small fraction of potassic silicate melts that are enriched in incompatible trace elements and volatiles. Here, to determine the chemical composition of such melt, we analysed fossilized melt inclusion
Publikováno v:
Journal of Mineralogical and Petrological Sciences. 110:20-28
Publikováno v:
Mineralogy and Petrology. 107(6):881-895
An isochemical kelyphite (orthopyroxene+spinel+plagioclase) that has nearly the same bulk chemical composition as the precursor garnet was found within a matrix of ordinary kelyphites (orthopyroxene+clinopyroxene+spinel±amphibole) in garnet peridoti
Publikováno v:
Journal of Mineralogical and Petrological Sciences. 104:168-175
An ultra-high-pressure metamorphic condition (~ 140 km) at ~ 950 °C is identified from a garnet -pyroxenite, containing primary supersilicic clinopyroxene, as a part of the mafic -ultramafic lenses enclosed in the Gfohl granulite at the Horni Bory q
Publikováno v:
Journal of Mineralogical and Petrological Sciences. 103:285-290
Publikováno v:
Journal of Metamorphic Geology. 22:593-603
Equilibrium pressure-temperature (P-T) conditions were estimated for kyanite-bearing eclogite from NoveDvory, Czech Republic, by using garnet-clinopyroxene thermometry and garnet-clinopyroxene- kyanite-coesite (or quartz) barometry. The estimated P-T
Autor:
Kosuke Naemura, Tomoyuki Kobayashi, Martin Svojtka, Daijo Ikuta, Takao Hirajima, Shugo Ohi, Hiroyuki Kagi, Tadamasa Ueda, Shoko Odake
Publisher Summary In the Plesovice peridotite, several lines of evidence suggesting an ultradeep condition are found. All of these facts suggest that the Plesovice peridotite once resided in the diamond-stability field, which could not be identified
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b18a4cf55fa941aecee9f0c17ffed6c
https://doi.org/10.1016/b978-0-12-385144-4.00002-3
https://doi.org/10.1016/b978-0-12-385144-4.00002-3