Morpho-sedimentary features and sediment dispersal systems of the southwest end of the Ryukyu Trench: a source-to-sink approach-Reference-Cited by-同舟云学术

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Morpho-sedimentary features and sediment dispersal systems of the southwest end of the Ryukyu Trench: a source-to-sink approach

Published:2017-05-29 Issue:6 Volume:37 Page:561-577
ISSN:0276-0460
Container-title:Geo-Marine Letters
language:en
Short-container-title:Geo-Mar Lett

Author:

Hsiung Kan-Hsi,Kanamatsu Toshiya,Ikehara Ken,Shiraishi Kazuya,Horng Chorn-Shern,Usami Kazuko

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Geotechnical Engineering and Engineering Geology,Environmental Science (miscellaneous),Oceanography

Link

http://link.springer.com/article/10.1007/s00367-017-0509-3/fulltext.html

Reference69 articles.

1. Abrahams SC, Calhoun BA (1953) The low-temperature transition in magnetite. Acta Crystallogr 6(1):105–106

2. Aiba J, Sekiya E (1979) Distribution and characteristics of the Neogene sedimentary basins around the Nansei-Shoto (Ryukyu Islands) (in Japanese with English abstract). J Japanese Assoc Petrol Technol 44:329–340

3. Angelier J (1986) Geodynamics of the Eurasia-Philippine Sea Plate Boundary: preface. Tectonophysics 125(1-3):IX–X

4. Bentahila Y, Othman DB, Luck JM (2008) Strontium, lead and zinc isotopes in marine cores as tracers of sedimentary provenance: a case study around Taiwan orogen. Chem Geol 248:62–82

5. Collot JY, Fisher MA (1991) The collision zone between the north d’Entrecasteaux ridge and the new Hebrides island arc 1. Sea beam morphology and shallow structure. J Geophys Res 96:4457–4478. doi: 10.1029/90JB00715

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