Authigenic Clays Versus Carbonate Formation as Products of Marine Silicate Weathering in the Input Sequence to the Sumatra Subduction Zone

Author:

Torres M. E.1ORCID,Milliken K. L.2,Hüpers A.3,Kim J.‐H.4,Lee S.‐G.5

Affiliation:

1. College Earth Ocean and Atmospheric Science Oregon State University Corvallis OR USA

2. Bureau of Economic Geology University of Texas at Austin Austin TX USA

3. MARUM‐Center for Marine Environmental Sciences University of Bremen Bremen Germany

4. Petroleum & Marine Division Korea Institute of Geoscience and Mineral Resources Daejeon South Korea

5. Geology Division Korea Institute of Geoscience and Mineral Resources Daejeon South Korea

Funder

National Science Foundation

Deutsche Forschungsgemeinschaft

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference47 articles.

1. Silica activity and the smectite-illite reaction

2. Illite/smectite formation and potassium transfer during burial diagenesis of mudrocks. A study from the Texas gulf coast Paleocene‐Eocene;Awwiller D. N.;Journal of Sedimentary Petrology,1993

3. Detrital mica influence on reservoir‐scale diagenesis;Boles J. R.;Annual Meeting Abstracts, American Association of Petroleum Geologists,2007

4. The mangrove reactor: Fast clay transformation and potassium sink

5. Cenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering

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