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The late quaternary tephra layers from the caldera volcanoes in and around kagoshima bay, southern kyushu, japan

Shinji Nagaoka
- 01 Jan 1988 - 
- Vol. 23, Iss: 23, pp 49-122
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This article is published in Geographical reports of Tokyo Metropolitan University.The article was published on 1988-01-01 and is currently open access. It has received 53 citations till now. The article focuses on the topics: Tephra & Caldera.

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Subsidence of ash-flow calderas: Relation to caldera size and magma-chamber geometry

TL;DR: In this paper, a review of features at eroded pre-Quaternary calderas is inferred to reflect varying sizes, roof geometries, and depths of the source magma chambers, in combination with prior volcanic and regional tectonic influences.
Journal ArticleDOI

Chronology of Tephra Layers in Southern Kyushu, SW Japan, for the Last 30, 000 Years

TL;DR: In this paper, K-Ah et al. proposed a method to solve the problem of the lack of information about the source of the information in order to improve the quality of the data.
Journal ArticleDOI

Late Quaternary Shorelines in the Japanese Islands

TL;DR: The recent progress of late Quaternary shoreline studies in Japan are reviewed in this paper, where outcomes of the estimation of ages and elevations of shorelines during high sea-level stand of the late Pleistocene are exemplified for five localities, Hateruma Island in the Ryukyus, Matsumae Peninsula of Hokkaido, Tanegashima Island to the south of Kyushu, Noto Peninsula in the Japan Sea side of Chubu district, and Muroto Peninsula of southeastern Shikoku.
Journal ArticleDOI

Preferred Clast Orientation in Volcaniclastic Mass-Flow Deposits: Application of a New Photo-Statistical Method

TL;DR: A photo-statistical method has been developed to quantify the strength of directional clast fabric in various types of volcaniclastic mass-flow deposits as mentioned in this paper, which is defined as the resultant vec- tor length of clast alignment computed from clast angles visible on a vertical outcrop face.
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