Kazuaki Nakamura

National Center For Child Health and Development

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John N. Davies

Columbia University

Klaus Jacob

Freie Universität Berlin

Vincent Renard

Nantes Université

Kantaro Fujioka

Kanagawa University

Tokihiko Matsuda

Association for the Development of Earthquake Prediction

Philippe Huchon

Institut des Sciences de la Terre de Paris

Jacques Bourgois

Sorbonne Université

Akira Takeuchi

Toyama Science Museum

Guy Pautot

Ifremer

Jacques Angelier

Sorbonne Université

Cooperative Institutions

The University of Tokyo

Centre National de la Recherche Scientifique

Earthquake Engineering Research Institute

Tokyo University of Science

Association for the Development of Earthquake Prediction

Sorbonne Université

Geophysical Division of the Earth Science Institute of the Slovak Academy of Sciences

Japan Agency for Marine-Earth Science and Technology

United States Geological Survey

Kyoto University

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Deep-sea submersible survey in the Suruga, Sagami and Japan Trenches: preliminary results of the 1985 Kaiko cruise, Leg 2

Earth and Planetary Science Letters (1987)

Guy Pautot Kazuaki Nakamura Philippe Huchon Jacques Angelier Jacques Bourgois

Seamount

Trough (economics)

Convergent boundary

Pacific Plate

10.1016/0012-821x(87)90073-2

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Citations (39)

Volcanoes as possible indicators of tectonic stress orientation — Aleutians and Alaska

Pure and Applied Geophysics (1977)

Kazuaki Nakamura Klaus Jacob John N. Davies

Dike

Island arc

Stress field

Volcanic arc

10.1007/bf01637099

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Citations (198)

An Interpretation of Current Crustal Deformations around the Suruga Bay, Japan

Zisin (Journal of the Seismological Society of Japan 2nd ser ) (1981)

Kazuaki Nakamura

10.4294/zisin1948.34.2_272

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Citations (2)

36. Volcano-Stratigraphic Study of Oshima Volcano, Izu

東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo (1964)

Kazuaki Nakamura

Source

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Citations (91)

Surface faulting during the Matsushiro earthquakes*

Eos (1969)

Kazuaki Nakamura

More than ten en echelon cracks, ranging from 100–700 meters in length, successively formed on alluvial deposits and continued to creep during higher seismicity periods of the Matsushiro swarm earthquakes in 1966. Some of these cracks are still creeping at present with a velocity of a few millimeters per year. The en echelon cracks, especially those with left‐lateral displacement, define a straight zone, 0.1–0.5 km wide and 4 km long, and are again arranged en echelon. The amount of displacement along the zone is estimated by various field measurements at about 50 cm in the left‐lateral component and 10–20‐cm uplift of the southwest side. The double en echelon cracks in the zone are best interpreted as surface traces of a left‐lateral strike‐slip fault newly formed in the bed rock. There are other evidences of the faulting on the northwest extension of the zone. They are the left‐lateral shift of railroad tracks in an interval of a few hundred meters and systematic breakage of a network of dikes between the rice paddy.

Echelon formation

Dike

10.1029/eo050i005p00389

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Citations (7)

Recent and present-day subduction and collision along the northern tip of the Philippine sea plate

Tectonophysics (1983)

Kazuaki Nakamura Kunihiko Shimazaki Nobuyuki Yonekura

Peninsula

Eurasian Plate

Convergent boundary

North American Plate

10.1016/0040-1951(83)90133-6

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Citations (0)

σ<i>H</i><sub>max</sub> Trajectories East of SURUGA Trough, Japan-an Effect of Flexure of Lithospheric Plate

Zisin (Journal of the Seismological Society of Japan 2nd ser ) (1979)

Kazuaki Nakamura

Trough (economics)

Sigma

10.4294/zisin1948.32.3_370

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Citations (6)

Distribution of Quaternary rhyolite domes of the Coso Range, California: Implications for extent of the geothermal anomaly

Journal of Geophysical Research Atmospheres (1980)

Charles R. Bacon Wendell A. Duffield Kazuaki Nakamura

Thirty‐eight separate domes and flows of phenocryst‐poor, high‐silica rhyolite of similar major element chemical composition were erupted over the past 1 m.y. from vents arranged in a crudely S ‐shaped array atop a granitic horst in the Coso Range, California. Most of the extrusions are probably less than about 0.3 m.y. old. The area is one of Quaternary basaltic volcanism and crustal extension. The central part of the rhyolite field is characterized by high heat flow, low apparent resistivity, and substantial fumarolic activity indicative of an active geothermal system. The immediate source of heat for the surficial geothermal phenomena is probably a silicic magma reservoir that may still contain molten or partially molten material at a depth of at least 8 km beneath the central part of the rhyolite field. Outlying rhyolite extrusions probably reflect the presence of feeder dikes emanating from the reservoir beneath the central region. Azimuths of dikes appear to be parallel to the regional tectonic axis of maximum horizontal compression, analogous to some dike‐fed flank eruptions on basaltic shields and andesitic stratovolcanoes. The areal extent of a magma reservoir and the present total heat content of the silicic magma system at Coso may be less than was previously estimated. However, the area is still considered to be one of significant geothermal potential.

Silicic

Caldera

Phenocryst

Dike

Magma chamber

10.1029/jb085ib05p02425

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Citations (60)

Quantitative distribution of late Cenozoic volcanic materials in Japan

Bulletin of Volcanology (1963)

Arata Sugimura Tokihiko Matsuda Kiyotaka Chinzei Kazuaki Nakamura

Neogene