Research Achievements - Original paper -
-
Transition from magmatic to phreatomagmatic eruptions in Young Ciremai volcano, Indonesia: insights from stratigraphy, componentry, and textural analysis of tephra deposits
Wildan N. Hamzah, Tsukasa Ohba, Muhammad Andriansyah Gurusinga, Mradipta L. A. Moktikanana, Jananda N. Indriyanto, Takashi Hoshide, Mirzam Abdurrahman, Idham A. Kurniawan, Fadlin
Earth, Planets and Space 2025.02 [Refereed]
Research paper (journal) International Co-author
-
Rinaldi Ikhram, Takashi Hoshide, Tsukasa Ohba, Mega Fatimah Rosana, Adi Hardiyono
Journal of Asian Earth Sciences: X 2025.01 [Refereed]
Research paper (journal) International Co-author
-
Origin of two types of olivine from the Ogi Picritic Dolerite Sill, northeast Japan
Akira CHIBA, Takashi HOSHIDE, Satoshi TANABE
Journal of Mineralogical and Petrological Sciences 119 ( 1 ) 2024.11 [Refereed]
Research paper (journal) Domestic Co-author
-
Takashi Hoshide, Nao Ishibashi, Keisuke Iwahashi
Bulletin of Volcanology 2024.01 [Refereed]
Research paper (journal) Domestic Co-author
-
Takashi Hoshide, Angela Bokuik, Tatsuki Ishikawa
Open Geosciences ( De Gruyter ) 2023.12 [Refereed]
Research paper (journal) International Co-author
-
Gurusinga, M. A., Ohba, T., Harijoko, A. and Hoshide, T.
Volcanica 2023.11 [Refereed]
Research paper (journal) International Co-author
-
Eruptive history of the last-1300-years activity of Kelud volcano, Indonesia: Inferences from stratigraphy, chronology, sedimentology, componentry, and geochemistry
Jananda N. Indriyanto, Tsukasa Ohba, Takashi Hoshide, Syahreza S. Angkasa, Mirzam Abdurrachman
Journal of Volcanology and Geothermal Research ( Elsevier ) 2022.11 [Refereed]
Research paper (journal) International Co-author
-
Kentaro Kondo, Takashi Hoshide
Geosciences Journal ( Springer Nature ) 2022.01 [Refereed]
Research paper (journal) Domestic Co-author
The upper Kayaoka sheet in the Atsumi area, Northeast Japan, has an alkaline-basaltic composition. The modal olivine and Ni enrichment in the lower part of the sheet indicates the accumulation of early formed olivine crystals. Overall, the average aspect ratio of plagioclase increases from the central part of the sheet toward both the top and bottom margins. The average aspect ratios of plagioclase and calculated crystallisation times at each height of the sheet, except for the lowermost margin, are roughly plotted near the regression line drawn based on those from many sills in previous research. However, we observed that the average aspect ratios of plagioclase in some horizons of the central part of the sheet exhibit an offset from the regression line. The olivine analcite dolerite in the central part of the sheet is rich in zeolite amygdules and glassy mesostasis with a quench texture. These observations suggest that the cooling rate in the central part of the sheet was faster compared with assuming conductive cooling only. A plausible mechanism for the rapid cooling at the centre of the sheet is heat transport by the convection of seawater that has infiltrated the columnar joint.
-
Hikaru Iwamori, Kenta Ueki, Takashi Hoshide, Hiroshi Sakuma, Masahiro Ichiki, Tohru Watanabe, Michihiko Nakamura, Hitomi Nakamura, Tatsuji Nishizawa, Atsushi Nakao, Yasuo Ogawa, Tatsu Kuwatani, Kenji Nagata, Tomomi Okada, Eiichi Takahashi
Journal of Geophysical Research: Solid Earth ( American Geophysical Union ) 126 ( 9 ) 2021.09 [Refereed]
Research paper (journal) International Co-author
-
Genesis of magmatic ilmenite ores associated with the Mazua ultramafic intrusion, NE Mozambique
David A. B. Unganai, Akira Imai, Ryohei Takahashi, Daud L. Jamal, Andrea Agangi, Takashi Hoshide, Hinako Sato
Ore Geology Reviews ( Elsevier ) 2022.02 [Refereed]
Research paper (journal) International Co-author
-
Deep crustal crystallization of tholeiitic melt: Insights from Manguao Basalt, Palawan, Philippines
James Cesar, Avisado REFRAN, Tsukasa OHBA, Carlo Abundo ARCILLA, Takashi HOSHIDE, Maria Ines Rosana, D. BALANGUE–TARRIELA
Journal of Mineralogical and Petrological Sciences ( Japan Association of Mineralogical Sciences ) 115 ( 6 ) 440 - 456 2020.12 [Refereed]
Research paper (journal) International Co-author
-
Reza Firmansyah Hasibuan, Tsukasa Ohba, Mirzam Abdurrachman, Takashi Hoshide
Indonesian Journal on Geoscience ( Geological AgencyMinistry of Energy and Mineral Resources ) 7 ( 2 ) 135 - 159 2020.08 [Refereed]
Research paper (journal) International Co-author
-
Site GT2: transition from foliated to layered gabbros
Kelemen, P.B., Matter, J.M., Teagle, D.A.H., Coggon, J.A., and the Oman Drilling Project Science Team
Proceedings of the Oman Drilling Project: College Station, TX (International Ocean Discovery Program) ( International Ocean Discovery Program ) 2020.08 [Refereed]
Research paper (journal) International Co-author
-
Site GT1: layered cumulate gabbros and deep fault zones
Kelemen, P.B., Matter, J.M., Teagle, D.A.H., Coggon, J.A., and the Oman Drilling Project Science Team
Proceedings of the Oman Drilling Project: College Station, TX (International Ocean Discovery Program) ( International Ocean Discovery Program ) 2020.08 [Refereed]
Research paper (journal) International Co-author
-
Topography and landslides in weathered granitic rock areas—Hai Van landslide in central Vietnam
Abe S, Dinh Van Tien, Do Ngoc Ha, Takashi Hoshide, Tadashi Nishitani & Toyohiko Miyagi
Landslides ( Springer Nature ) 15 ( 8 ) 1675 - 1689 2018.08 [Refereed]
Research paper (journal) International Co-author
-
Takashi Hoshide, Masaaki Obata
Contributions to Mineralogy and Petrology ( Springer Nature ) 168 2014.08 [Refereed]
Research paper (journal) Domestic Co-author
The problem of whether cumulate rocks were formed by crystal settling or by in situ crystallization after magma emplacement is an important issue concerning the mechanisms of magmatic differentiation. However, it is hard to distinguish these two processes for plutonic rocks because the primary texture and chemical composition have generally been modified by postcumulus processes. To contribute this problem, we studied the distribution and compositions of Cr-spinel inclusions hosted in olivine and plagioclase in the Murotomisaki Gabbroic Intrusion (MGI), SW Japan. It is shown that the olivine-hosted inclusions are restricted to specific horizons where accumulation of olivine phenocrysts is thought to have occurred and that the compositional variations of the Cr-spinel are explained by a secondary compositional modification that probably took place after the magma emplacement. It is also shown that the Cr-spinel inclusions in a chilled margin have suffered the least compositional modification and nearly retains the primary composition. Those in the interior of the intrusion, on the contrary, have been significantly modified by re-equilibration with residual melt driven by cation diffusions through the host phases. Those in plagioclase have been less modified. It is shown that all the spinel inclusions had primarily the same and common composition at the time of magma emplacement. This implies that all the inclusion-bearing crystals, olivine and plagioclase, represent primary phenocrysts that had already existed in the emplaced magma. In this way, spinel inclusion in the MGI may be regarded to be a useful petrographic “marker” for identifying intratelluric phenocrysts and also as a “tracer” to trace the motion of the primary phenocrysts after the magma emplacement.
-
Proc. IODP, 345: College Station, TX (Integrated Ocean Drilling Program)
Gillis, K.M., Snow, J.E., Klaus, A., and the Expedition 345 Scientists
Proceedings of the Integrated Ocean Drilling Program ( Integrated Ocean Drilling Program ) 2014.02 [Refereed]
Research paper (journal) International Co-author
-
Primitive layered gabbros from fast-spreading lower oceanic crust
Kathryn M. Gillis, Jonathan E. Snow, Adam Klaus, Natsue Abe, Álden B. Adrião, Norikatsu Akizawa, Georges Ceuleneer, Michael J. Cheadle, Kathrin Faak, Trevor J. Falloon, Sarah A. Friedman, Marguerite Godard, Gilles Guerin, Yumiko Harigane, Andrew J. Horst, Takashi Hoshide, Benoit Ildefonse, Marlon M. Jean, Barbara E. John, Juergen Koepke, Sumiaki Machi, Jinichiro Maeda, Naomi E. Marks, Andrew M. McCaig, Romain Meyer, Antony Morris, Toshio Nozaka, Marie Python, Abhishek Saha & Robert P. Wintsch
Nature ( Springer Nature ) 505 204 - 207 2014.01 [Refereed]
Research paper (journal) International Co-author
-
Expedition 345 Scientists
IODP Preliminary Report ( Integrated Ocean Drilling Program ) 2014.01 [Refereed]
Research paper (journal) International Co-author
-
Takashi Hoshide and Masaaki Obata
Journal of Petrology ( Oxford University Press ) 53 ( 2 ) 419 - 449 2012.01 [Refereed]
Research paper (journal) Domestic Co-author
室戸岬斑れい岩体の集積鉱物(かんらん石・斜長石)に包有される含角閃石多相固体包有物の産状と化学組成を詳細に調べた。その結果、多相固体包有物の化学組成は、本岩体の結晶分化でできるメルトの組成から大きくかけ離れ、包有物のホスト鉱物の化学組成の方へ偏っていることがわかった。そのことから、集積鉱物に見られる多相固体包有物は、固液境界層内での流体相の移動に伴って起きた集積鉱物の再溶解で局所的にできた特異な化学組成のメルトを取り込んだことで形成されたと主張した。