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1-3 OF 3
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Seiichi Toshimitsu
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Book Chapter
The Kyushu–Ryukyu Arc
Book: The Geology of Japan
Series: Geological Society, London, Geology of Series
Publisher: Geological Society of London
Published: 01 January 2016
DOI: 10.1144/GOJ.6
EISBN: 9781862397064
Abstract The Kyushu-Ryukyu Arc extends for over 1000 km south from the large island of Kyushu down the Ryukyu Island chain towards Taiwan. It has been produced by subduction of oceanic plates beneath the Eurasian continent and exposes a wide range of Palaeozoic, Mesozoic and Cenozoic rocks formed in an active continental margin setting (Maruyama et al. 1997; Isozaki et al. 2010). In this chapter we describe the geology of the arc from the oldest (Palaeozoic and Triassic) to youngest (Neogene and Quaternary) rocks, and discuss the geodynamic evolution of the area.
Journal Article
Backward stacking of submarine channel–fan successions controlled by strike-slip faulting: The Izumi Group (Cretaceous), southwest Japan
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2009
Lithosphere (2009) 1 (1): 41–59.
Journal Article
Nielsenicrinus japonicus new species (Echinodermata; Crinoidea) from the Late Cretaceous of Japan and its paleobiogeographic implications
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 November 1996
Journal of Paleontology (1996) 70 (6): 964–968.