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Norikazu Matsuoka

Researcher at University of Tsukuba

Publications -  106
Citations -  4666

Norikazu Matsuoka is an academic researcher from University of Tsukuba. The author has contributed to research in topics: Permafrost & Frost weathering. The author has an hindex of 31, co-authored 105 publications receiving 4118 citations.

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The rate of bedrock weathering by frost action: Field measurements and a predictive model

TL;DR: Shattering rate, surface temperature, moisture content, and physical and strength properties of bedrock were measured in four rockwall sites of the Japanese Alps as mentioned in this paper, and it was shown that the annual shattering rate is dependent on the annual freeze-thaw frequency on the rock surface and the degree of saturation and tensile strength of the rock masses.
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Fast deformation of perennially frozen debris in a warm rock glacier in the Swiss Alps: An effect of liquid water

TL;DR: In this paper, surface movement, internal deformation, and temperature were monitored over 5 years on the Buz North rock glacier, a small rock glacier located at the lower limit of the permafrost belt in the Swiss Alps.
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Rock weathering processes and landform development in the Sør Rondane Mountains, Antarctica

TL;DR: In this paper, field observations of weathering processes and related landforms, combined with laboratory analyses of the weathering products, permit a synthetic evaluation of Late Cenozoic weathering environments in the Sor Rondane Mountains, Antarctica, an arid upland characterized by low temperatures and strong winds.
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Comparison of geophysical investigations for detection of massive ground ice (pingo ice)

TL;DR: In this article, six different geophysical investigations, including ground-penetrating radar, DC resistivity sounding, seismic refraction, very low frequency (VHF) electromagnetic, helicopter borne electromagnetic (HEM), and transient electromagnetic (TEM) techniques, were employed to obtain information on the ice body properties of pingos near Fairbanks, Alaska.
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Monitoring of Periglacial Slope Processes in the Swiss Alps: the First Two Years of Frost Shattering, Heave and Creep

TL;DR: In this article, a synthetic monitoring system was developed in an attempt to evaluate geomorphic processes acting on periglacial rock and debris slopes in the Swiss Alps, including joint widening, soil heave and creep and associated variables.