| Subduction zone magmatism Y Tatsumi, S Eggins Subduction zone magmatism, 1995 | 1452 | 1995 |
| Chemical characteristics of fluid phase released from a subducted lithosphere and origin of arc magmas: evidence from high-pressure experiments and natural rocks Y Tatsumi, DL Hamilton, RW Nesbitt Journal of volcanology and geothermal research 29 (1-4), 293-309, 1986 | 1218 | 1986 |
| Migration of fluid phases and genesis of basalt magmas in subduction zones Y Tatsumi Journal of Geophysical Research: Solid Earth 94 (B4), 4697-4707, 1989 | 913 | 1989 |
| Trace element transport during dehydration processes in the subducted oceanic crust: 1. Experiments and implications for the origin of ocean island basalts T Kogiso, Y Tatsumi, S Nakano Earth and Planetary Science Letters 148 (1-2), 193-205, 1997 | 661 | 1997 |
| Generation of arc basalt magmas and thermal structure of the mantle wedge in subduction zones Y Tatsumi, M Sakuyama, H Fukuyama, I Kushiro Journal of Geophysical Research: Solid Earth 88 (B7), 5815-5825, 1983 | 623 | 1983 |
| The structure of iron in Earth’s inner core S Tateno, K Hirose, Y Ohishi, Y Tatsumi Science 330 (6002), 359-361, 2010 | 499 | 2010 |
| Setouchi high-Mg andesites revisited: geochemical evidence for melting of subducting sediments G Shimoda, Y Tatsumi, S Nohda, K Ishizaka, BM Jahn Earth and Planetary Science Letters 160 (3-4), 479-492, 1998 | 465 | 1998 |
| Formation of the volcanic front in subduction zones Y Tatsumi Geophysical Research Letters 13 (8), 717-720, 1986 | 409 | 1986 |
| High-Mg andesites in the Setouchi volcanic belt, southwestern Japan: analogy to Archean magmatism and continental crust formation? Y Tatsumi Annu. Rev. Earth. Planet. Sci. 34 (1), 467-499, 2006 | 392 | 2006 |
| Hot fingers in the mantle wedge: new insights into magma genesis in subduction zones Y Tamura, Y Tatsumi, D Zhao, Y Kido, H Shukuno Earth and Planetary Science Letters 197 (1-2), 105-116, 2002 | 373 | 2002 |
| Origin of high-magnesian andesites in the Setouchi volcanic belt, southwest Japan, II. Melting phase relations at high pressures Y Tatsumi Earth and Planetary Science Letters 60 (2), 305-317, 1982 | 360 | 1982 |
| The subduction factory: How it operates in the evolving Earth Y Tatsumi GSA today 15 (7), 4, 2005 | 353 | 2005 |
| Origin of high-magnesian andesites in the Setouchi volcanic belt, southwest Japan, I. Petrographical and chemical characteristics Y Tatsumi, K Ishizaka Earth and Planetary Science Letters 60 (2), 293-304, 1982 | 351 | 1982 |
| Geochemical modeling of partial melting of subducting sediments and subsequent melt-mantle interaction: Generation of high-Mg andesites in the Setouchi volcanic belt, southwest … Y Tatsumi Geology 29 (4), 323-326, 2001 | 322 | 2001 |
| Ontong Java Plateau eruption as a trigger for the early Aptian oceanic anoxic event MLG Tejada, K Suzuki, J Kuroda, R Coccioni, JJ Mahoney, N Ohkouchi, ... Geology 37 (9), 855-858, 2009 | 301 | 2009 |
| Remelting of an andesitic crust as a possible origin for rhyolitic magma in oceanic arcs: an example from the Izu–Bonin arc Y Tamura, Y Tatsumi Journal of Petrology 43 (6), 1029-1047, 2002 | 278 | 2002 |
| Oxygen isotope evidence for slab melting in modern and ancient subduction zones IN Bindeman, JM Eiler, GM Yogodzinski, Y Tatsumi, CR Stern, TL Grove, ... Earth and Planetary Science Letters 235 (3-4), 480-496, 2005 | 272 | 2005 |
| Contribution of slab melting and slab dehydration to magmatism in the NE Japan arc for the last 25 Myr: Constraints from geochemistry T Hanyu, Y Tatsumi, S Nakai, Q Chang, T Miyazaki, K Sato, K Tani, ... Geochemistry, Geophysics, Geosystems 7 (8), 2006 | 251 | 2006 |
| Trace element transport during dehydration processes in the subducted oceanic crust: 2. Origin of chemical and physical characteristics in arc magmatism Y Tatsumi, T Kogiso Earth and Planetary Science Letters 148 (1-2), 207-221, 1997 | 237 | 1997 |
| Crustal structure and evolution of the Mariana intra-oceanic island arc N Takahashi, S Kodaira, SL Klemperer, Y Tatsumi, Y Kaneda, K Suyehiro Geology 35 (3), 203-206, 2007 | 212 | 2007 |
