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Nguyen, Du, Morishita, Tomoaki, Soda, Yusuke, Tamura, Akihiro, Ghosh, Biswajit, Harigane, Yumiko, France, Lydéric, Liu, Chuanzhou, Natland, James, Sanfilippo, Alessio, MacLeod, Christopher, Blum, Peter, Dick, Henry (2018) Occurrence of Felsic Rocks in Oceanic Gabbros from IODP Hole U1473A: Implications for Evolved Melt Migration in the Lower Oceanic Crust. Minerals, 8 (12) 583 doi:10.3390/min8120583

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Reference TypeJournal (article/letter/editorial)
TitleOccurrence of Felsic Rocks in Oceanic Gabbros from IODP Hole U1473A: Implications for Evolved Melt Migration in the Lower Oceanic Crust
JournalMinerals
AuthorsNguyen, DuAuthor
Morishita, TomoakiAuthor
Soda, YusukeAuthor
Tamura, AkihiroAuthor
Ghosh, BiswajitAuthor
Harigane, YumikoAuthor
France, LydéricAuthor
Liu, ChuanzhouAuthor
Natland, JamesAuthor
Sanfilippo, AlessioAuthor
MacLeod, ChristopherAuthor
Blum, PeterAuthor
Dick, HenryAuthor
Year2018 (December 10)Volume8
Issue12
PublisherMDPI AG
URL
Download URLhttps://www.mdpi.com/2075-163X/8/12/583/pdf?version=1544519132
DOIdoi:10.3390/min8120583Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID7735013Long-form Identifiermindat:1:5:7735013:2
GUID0
Full ReferenceNguyen, Du, Morishita, Tomoaki, Soda, Yusuke, Tamura, Akihiro, Ghosh, Biswajit, Harigane, Yumiko, France, Lydéric, Liu, Chuanzhou, Natland, James, Sanfilippo, Alessio, MacLeod, Christopher, Blum, Peter, Dick, Henry (2018) Occurrence of Felsic Rocks in Oceanic Gabbros from IODP Hole U1473A: Implications for Evolved Melt Migration in the Lower Oceanic Crust. Minerals, 8 (12) 583 doi:10.3390/min8120583
Plain TextNguyen, Du, Morishita, Tomoaki, Soda, Yusuke, Tamura, Akihiro, Ghosh, Biswajit, Harigane, Yumiko, France, Lydéric, Liu, Chuanzhou, Natland, James, Sanfilippo, Alessio, MacLeod, Christopher, Blum, Peter, Dick, Henry (2018) Occurrence of Felsic Rocks in Oceanic Gabbros from IODP Hole U1473A: Implications for Evolved Melt Migration in the Lower Oceanic Crust. Minerals, 8 (12) 583 doi:10.3390/min8120583
In(2018, December) Minerals Vol. 8 (12) MDPI AG

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