M. Aoya

发表

A new approach to develop the Raman carbonaceous material geothermometer for low‐grade metamorphism using peak width

H. Mori, T. Mizukami, D. Nakamura, 2014 .

Recognition of the ‘early’ Sambagawa metamorphism and a schematic cross-section of the Late-Cretaceous Sambagawa subduction zone

S. Endo, M. Aoya, 2017 .

High‐P metamorphism, pattern of induced flow in the mantle wedge, and the link with plutonism in paired metamorphic belts

S. Uehara, T. Mizukami, S. Wallis, 2009 .

Regional‐Scale Excess Ar wave in a Barrovian type metamorphic belt, eastern Tibetan Plateau

T. Tsujimori, S. Wallis, M. Aoya, 2009 .

Middle to late Miocene extremely rapid exhumation and thermal reequilibration in the Kung Co rift, southern Tibet

D. Stockli, M. Whitehouse, Jeffrey Lee, 2011 .

Role of nappe boundaries in subduction-related regional deformation: spatial variation of meso- and microstructures in the Seba eclogite unit, the Sambagawa belt, SW Japan

S. Wallis, M. Aoya, 2003 .

Origin of eclogitic metagabbro mass in the Sambagawa belt: Geological and geochemical constraints

S. Wallis, M. Tsuboi, M. Aoya, 2006 .

Slow subduction and buoyant exhumation of the Sanbagawa eclogite

S. Uehara, S. Wallis, M. Tsuboi, 2012 .

Introduction: from snowball Earth to the Cambrian explosion–evidence from China

M. Aoya, U. Nzh, 2017 .

P–T–D Path of Eclogite from the Sambagawa Belt Deduced from Combination of Petrological and Microstructural Analyses

M. Aoya, 2001 .

A re‐evaluation of eclogite facies metamorphism in SW Japan: proposal for an eclogite nappe

S. Wallis, M. Aoya, 2000 .

Chloritoid and barroisite-bearing pelitic schists from the eclogite unit in the Besshi district, Sanbagawa metamorphic belt

M. Enami, M. Aoya, Zaw Win Ko, 2005 .

Chloritoid-bearing basic schists from the Sanbagawa metamorphic belt, central Shikoku: their petrologic significance and tectonic implications

M. Enami, M. Aoya, Zaw Win Ko, 2005 .

Extending the applicability of the Raman carbonaceous‐material geothermometer using data from contact metamorphic rocks

H. Shimizu, T. Mizukami, D. Nakamura, 2010 .

Phase equilibria modelling of blueschist and eclogite from the Sanbagawa metamorphic belt of southwest Japan reveals along‐strike consistency in tectonothermal architecture

T. Nagaya, S. Wallis, O. Weller, 2015 .

Plate movements, ductile deformation and geochronology of the Sanbagawa belt, SW Japan: tectonic significance of 89–88 Ma Lu–Hf eclogite ages

J. Platt, M. Thirlwall, R. Anczkiewicz, 2009 .

Illustrated Introduction to Eclogite in Japan

T. Tsujimori, T. Mizukami, M. Aoya, 2000 .

Thermal calculation for high-pressure contact metamorphism: application to eclogite formation in the Sebadani area, the Sambagawa belt, SW Japan

M. Aoya, 1998 .

Geologic traverse of the Sambagawa metamorphic belt in central Shikoku, SW Japan:: from the lowest-pressure metasediments to the highest-pressure ultramafic rocks@@@最浅部変成岩から最深部超苦鉄質岩まで

T. Mizukami, S. Endo, M. Aoya, 2017 .

Paleo-mantle wedge preserved in the Sambagawa high-pressure metamorphic belt and the thickness of forearc continental crust

T. Mizukami, S. Wallis, S. Endo, 2013 .

Derivation of Subduction-Stage Pressure-Temperature Path of Sambagawa Eclogite and its Tectonic Significance

M. Aoya, 2004 .

Petrological constraints on the formation conditions and retrograde P–T path of the Kotsu eclogite unit, central Shikoku

S. Wallis, Y. Seto, M. Aoya, 2003 .

Structural and microstructural constraints on the mechanism of eclogite formation in the Sambagawa belt, SW Japan

S. Wallis, M. Aoya, 1999 .

Subduction-stage pressure-temperature path of eclogite from the Sambagawa belt: Prophetic record for oceanic-ridge subduction

S. Uehara, S. Wallis, M. Enami, 2003 .

Cenozoic and Mesozoic metamorphism in the Longmenshan orogen: Implications for geodynamic models of eastern Tibet

Kazuhiro Suzuki, T. Tsujimori, S. Wallis, 2003 .

Structural position of the Seba eclogite unit in the Sambagawa Belt: Supporting evidence for an eclogite nappe

M. Aoya, 2002 .

Monument for IEC2001 made from a loose block of well developed schistose eclogite from the Besshi area, Japan.

Masayuki, S. Wallis, T. Hirajima, 2001 .

Contact metamorphism in the Malashan dome, North Himalayan gneiss domes, southern Tibet: an example of shallow extensional tectonics in the Tethys Himalaya

M. Heizler, Jeffrey Lee, S. Wallis, 2007 .

North-south extension in the Tibetan crust triggered by granite emplacement

M. Heizler, Jeffrey Lee, S. Wallis, 2005 .

The Malashan gneiss dome in south Tibet: comparative study with the Kangmar dome with special reference to kinematics of deformation and origin of associated granites

Jeffrey Lee, S. Wallis, Yu Wang, 2006, Geological Society, London, Special Publications.

E–W extension at 19 Ma in the Kung Co area, S. Tibet: Evidence for contemporaneous E–W and N–S extension in the Himalayan orogen

M. Mitsuishi, Jeffrey Lee, S. Wallis, 2011 .

Thermal consequences of a subduction boundary jump: A numerical model for generating subduction‐related clockwise pressure‐temperature paths

S. Uehara, S. Wallis, M. Aoya, 2002 .

Petrological feature of the Uzukiyama mafic plutonic complex, Iida city, Nagano Prefecture

T. Yamasaki, M. Aoya, K. Miyazaki, 2012 .

The Malashan metamorphic complex in southern Tibet: Dominantly top-to-the north deformation and intrusive origin of its associated granites

Jeffrey Lee, S. Wallis, Yu Wang, 2008 .

Thermal model for approach of a spreading ridge to subduction zones and its implications for high‐P/high‐T metamorphism: Importance of subduction versus ridge approach ratio

S. Uehara, M. Aoya, 2005 .