Sequence stratigraphic evolution of the Kumano forearc basin during the last deglaciation: Influence of eustasy and tectonically-controlled shelf morphology on deep-marine sediment dynamics-Reference-Cited by-同舟云学术

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Sequence stratigraphic evolution of the Kumano forearc basin during the last deglaciation: Influence of eustasy and tectonically-controlled shelf morphology on deep-marine sediment dynamics

Published:2022-03 Issue: Volume:430 Page:106100
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Cornard P.H.,Moernaut J.,Moore G.F.,Kioka A.,Kopf A.,dos Santos Ferreira C.,Strasser M.

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference160 articles.

1. Short paper: accretion and uplift in the Shimanto Belt, SW Japan;Agar;Journal of the Geological Society,1989

2. Late Quaternary equilibrium line altitude in the Kiso Mountain Range, central Japan;Aoki,2000

3. Explanatory notes of sedimentological map of Kumano Nada;Arita,1988

4. Shelfal sediment transport by an undercurrent forces turbidity-current activity during high sea level along the Chile continental margin;Bernhardt;Geology,2016

5. Immediate propagation of deglacial environmental change to deep-marine turbidite systems along the Chile convergent margin;Bernhardt;Earth and Planetary Science Letters,2017

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1. Spatial variations in the consolidation of sediments in the Neogene Miyazaki forearc basin, Southwest Japan;Tectonophysics;2023-09

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