Late Quaternary uplift rate inferred from marine terraces, Muroto Peninsula, southwest Japan: Forearc deformation in an oblique subduction zone-Reference-Cited by-同舟云学术

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Late Quaternary uplift rate inferred from marine terraces, Muroto Peninsula, southwest Japan: Forearc deformation in an oblique subduction zone

Published:2015-04 Issue: Volume:234 Page:133-150
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Matsu'ura Tabito

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference67 articles.

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3. The astronomical theory of climate and the age of the Brunhes–Matuyama magnetic reversal;Bassinot;Earth Planet. Sci. Lett.,1994

4. Growth folding and active thrusting in the Montello region, Vento, northern Italy;Benedetti;J. Geophys. Res.,2000

5. Kinematics of fault-related folding derived from a sandbox experiment;Bernard;J. Geophys. Res.,2007

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