Dehydroxylation Kinetics of Clay Minerals and Its Application to Friction Heating Along an Imbricate Thrust in an Accretionary Prism

Author:

Masumoto Hirokazu1ORCID,Kameda Jun2ORCID,Arima Hiroshi3,Sugiyama Kazumasa3,Nagai Takaya2,Yamamoto Yuzuru4ORCID

Affiliation:

1. Department of Natural History Sciences, Graduate School of Science; Hokkaido University; Sapporo Japan

2. Department of Earth and Planetary Sciences, Faculty of Science; Hokkaido University; Sapporo Japan

3. Institute for Materials Research (IMR), Tohoku University; Sendai Japan

4. Japan Agency for Marine-Earth Science and Technology; Yokohama Japan

Funder

Japan Society for the Promotion of Science

Tohoku University

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference71 articles.

1. Kinetic study of the kaolinite-mullite reaction sequence. Part I: Kaolinite dehydroxylation;Bellotto;Physics and Chemistry of Minerals,1995

2. Rietveld refinement of non-hydrogen atomic positions in kaolinite;Bish;Clays and Clay Minerals,1989

3. Chlorite dissolution in the acid pH-range: A combined microscopic and macroscopic approach;Brandt;Geochimica et Cosmochimica Acta,2003

4. X-ray study of thermal transformations in some magnesian chlorite minerals;Brindley;Acta Crystallographica,1950

5. Development of long basal spacings in chlorites by thermal treatment;Brindley;American Mineralogist,1974

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