Network


Latest external collaboration on country level. Dive into details by clicking on the dots.

Hotspot


Dive into the research topics where Tomoharu Miyamoto is active.

Publication


Featured researches published by Tomoharu Miyamoto.


Geological Society, London, Special Publications | 2008

Sapphirine+quartz association in garnet: implication for ultrahigh-temperature metamorphism at Rundvågshetta, Lützow-Holm Complex, East Antarctica

Yasutaka Yoshimura; Yoichi Motoyoshi; Tomoharu Miyamoto

Abstract We report the occurrence of sapphirine+quartz association within garnet porphyroblast in the garnet–orthopyroxene–sillimanite granulite (Grt–Opx–Sill granulite) from Rundvågshetta in the Lützow-Holm Complex, East Antarctica. The granulites in the study area show a characteristic mineral assemblage consisting of orthopyroxene+sillimanite+quartz. The presence of sapphirine and quartz inclusions within garnet in the sapphirine-bearing Grt–Opx–Sill granulite suggests that metamorphic conditions changed from the stability field of orthopyroxene+sillimanite+quartz to that of sapphirine+quartz during the garnet growth. Peak metamorphic temperature conditions of about 1000–1100 °C are obtained by ternary feldspar thermometry for these granulites. Similar temperatures were also estimated from the Al-in-orthopyroxene geothermometer. The granulites are also characterized by coarse-grained garnet, being partly surrounded by a fine-grained symplectite composed of orthopyroxene and cordierite, whereas sapphirine+cordierite symplectitic intergrowth occurs in the matrix. These textures imply that the area underwent isothermal decompression subsequent to ultrahigh-temperature metamorphism. The sapphirine-bearing Grt–Opx–Sill granulite is likely to be the restitic product of partial melting and shows signs of segregation and movement of melt.


Geological Society, London, Special Publications | 2008

Pre-metamorphic carbon, oxygen and strontium isotope signature of high-grade marbles from the lützow-holm complex, east antarctica: Apparent age constraints of carbonate deposition

M. Satish-Kumar; Tomoharu Miyamoto; Joerg Hermann; Hiroo Kagami; Yasuhito Osanai; Yoichi Motoyoshi

Abstract C, O and Sr isotope geochemistry of high-grade marbles from the Lützow-Holm Complex, East Antarctica, has given clues on the depositional ages and post-depositional alterations. Dolomitic and calcitic marbles occur as thin layers with varying thickness (up to 100 m) in several outcrops in eastern Dronning Maud Land, most of which underwent post-depositional geochemical alterations. In particular, the Sr and O isotope alterations are extensive, with 87Sr/86Sr(550 Ma) ratios as high as 0.758 and δ18O values as low as −5‰. These data suggest that multiple stages of fluid–rock interaction processes during diagenesis, prograde to peak and retrograde metamorphic events have altered the depositional isotopic signatures. However, some of the marble layers, exceptionally, preserve pre-metamorphic geochemical characteristics, such as low Sr isotope ratios, high δ18O and δ13C values, and well-equilibrated unaltered trace and rare earth element patterns. Lowest 87Sr/86Sr isotopic ratios of 0.7066 and 0.7053 with high δ13C and δ18O values suggest an apparent age of deposition around 730–830 Ma, although total geochemical resetting of carbonates by seawater of this age cannot be ruled out. The apparent depositional ages are consistent with carbonate deposition in the ‘Mozambique Ocean’ that separated East and West Gondwana.


Geological Society, London, Special Publications | 2008

Fe2+-Mg partitioning experiments between orthopyroxene and spinel using ultrahigh-temperature granulite from the Napier Complex, East Antarctica

Kei Sato; Tomoharu Miyamoto; Toshisuke Kawasaki

Abstract Temperature dependence of the Fe2+–Mg exchange between orthopyroxene (Opx) and spinel (Spl), was experimentally determined at 9–13 kbar and 900–1200 °C using an ultrahigh-temperature (UHT) granulite collected from the Napier Complex in Enderby Land, East Antarctica. The Fe2+–Mg distribution coefficient, is empirically obtained as where X is the cationic mole fraction, and pressure P and temperature T are in kbar and Kelvin, respectively. The new geothermometer was applied to various natural UHT and associated high-grade metamorphic rocks from East Antarctica and other regions of the world. The results indicate temperatures between 735 and 902 °C at pressures in the range of 5–14 kbar. This geothermometer utilizing spinel does not give peak metamorphic condition, because it is relatively easy for spinel to re-equilibrate during the cooling stage of metamorphism. Hence, we conclude that the geothermometer is suitable for evaluating the closure temperature for the KD between aluminous orthopyroxene and spinel during retrograde metamorphism rather than the thermal peak.


Geological Society, London, Special Publications | 2008

Post-peak (<530 Ma) thermal history of Lützow-Holm Complex, East Antarctica, based on Rb–Sr and Sm–Nd mineral chronology

Tomoharu Miyamoto; M. Satish-Kumar; Daniel J. Dunkley; Yasuhito Osanai; Yasutaka Yoshimura; Yoichi Motoyoshi; Christopher J. Carson

Abstract Rb–Sr and Sm–Nd mineral dating of metamorphic rocks from Skallen, Skallevikshalsen and Rundvågshetta, in the southwestern part of the Lützow-Holm Complex, Dronning Maud Land, assists in constructing a thermal history after peak metamorphism. The results fall into two groups: (1) a record of regional cooling after peak metamorphism (524–488 Ma); (2) local resetting 50–80 Ma after peak metamorphism (474–446 Ma). This grouping is consistently observed in published ages from various localities in the Lützow-Holm Complex. A Sm–Nd age of 524 Ma is indistinguishable from published zircon and monazite ages. Ages of 511 and 488 Ma are related to cooling after peak metamorphism. The younger age group overlaps with ages of post-metamorphic magmatism and related hydrothermal activity reported from localities throughout East Antarctica. This intracontinental, post-orogenic igneous activity continued after the tectonic assembly of Gondwana.


Comptes Rendus Geoscience | 2008

Discovery of high-pressure granulite-facies metamorphism in northern Vietnam : Constraints on the Permo-Triassic Indochinese continental collision tectonics

Nobuhiko Nakano; Yasuhito Osanai; Nguyen Thi Minh; Tomoharu Miyamoto; Yasutaka Hayasaka; Masaaki Owada


Journal of Metamorphic Geology | 2010

Triassic eclogite from northern Vietnam: Inferences and geological significance

Nobuhiko Nakano; Yasuhito Osanai; K. Sajeev; Yasutaka Hayasaka; Tomoharu Miyamoto; Nguyen Thi Minh; Masaaki Owada; Brian F. Windley


Journal of Science of the Hiroshima University, Series C: Geology and Mineralogy | 1990

Tectonic evolution of the Sambagawa schists and its implications in convergent margin processes

Ikuo Hara; T. Shiota; K. Hide; K. Kanai; M. Goto; S. Seki; K. Kaikiri; K. Takeda; Yasutaka Hayasaka; Tomoharu Miyamoto; Y. Sakurai; Yukiko Ohtomo


Journal of Mineralogical and Petrological Sciences | 2008

Collision zone metamorphism in Vietnam and adjacent South-eastern Asia: Proposition for Trans Vietnam Orogenic Belt

Yasuhito Osanai; Nobuhiko Nakano; Masaaki Owada; Tran Ngoc Nam; Tomoharu Miyamoto; Nguyen Thi Minh; Nguyen Van Nam; Tran Van Tri


Journal of Metamorphic Geology | 2011

Origin of zircon in jadeitite from the Nishisonogi metamorphic rocks, Kyushu, Japan

Yasushi Mori; Yuji Orihashi; Tomoharu Miyamoto; Kazuhiko Shimada; Miki Shigeno; Tadao Nishiyama


Gondwana Research | 2006

Experimental calibration of sapphirine-spinel Fe2+-Mg exchange thermometer: Implication for constraints on P-T condition of Howard Hills, Napier Complex, East Antarctica

Kei Sato; Tomoharu Miyamoto; Toshisuke Kawasaki

Collaboration


Dive into the Tomoharu Miyamoto's collaboration.

Top Co-Authors

Avatar

Yoichi Motoyoshi

National Institute of Polar Research

View shared research outputs
Top Co-Authors

Avatar

Daniel J. Dunkley

American Museum of Natural History

View shared research outputs
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Top Co-Authors

Avatar
Researchain Logo
Decentralizing Knowledge