The use of microstructures for discriminating turbiditic and hemipelagic muds and mudstones

Author:

Kase Yoshihiro1,Sato Maromi1,Nishida Naohisa2,Ito Makoto1,Mukti Muhammad Ma'ruf1,Ikehara Ken2,Takizawa Shigeru3

Affiliation:

1. Department of Earth Sciences; Graduate School of Science; Chiba University; Chiba 263-8522 Japan

2. Institute of Geology and Geoinformation; Geological Survey of Japan; AIST; Ibaraki 305-8567 Japan

3. Graduate School of Life and Environmental Sciences; University of Tsukuba; Ibaraki 305-8572 Japan

Funder

Japan Society for the Promotion of Science

Chiba University

Publisher

Wiley

Subject

Stratigraphy,Geology

Reference54 articles.

1. A phase diagram for turbulent, transitional, and laminar clay suspension flows;Baas;J. Sed. Res.,2009

2. In situ measurement of particle size in estuarine waters;Bale;Estuar. Coast. Shelf Sci.,1987

3. Clay Microstructure

4. Clay fabric of selected submarine sediments: fundamental properties and models;Bennett;J. Sed. Petrol.,1981

5. Clay Sedimentology

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