Sedimentary inputs to the Nankai subduction zone: The importance of dispersed ash

Author:

Scudder Rachel P.1,Murray Richard W.1,Kutterolf Steffen2,Schindlbeck Julie C.2,Underwood Michael B.3,Wang Kuo-Lung4

Affiliation:

1. Department of Earth and Environment, Boston University, 685 Commonwealth Avenue, Boston, Massachusetts 02215, USA

2. Research Center for Marine Geosciences (GEOMAR) Helmholtz Centre for Ocean Research Kiel, Wischhofstraße 1-3, Kiel 24148, Germany

3. Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801, USA

4. Institute of Earth Sciences, Academia Sinica, Taipei 11529, Taiwan

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Reference75 articles.

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2. Volcanic activity recorded in deep-sea sediments and the geodynamic evolution of western Pacific island arcs;Cambray,1995

3. Grain size of Miocene volcanic ash layers from Sites 998, 999, and 1000: Implications for source areas and dispersal;Carey,2000

4. Optimization of end-members used in multiple linear regression geochemical mixing models;Dunlea;Geochemistry Geophysics Geosystems,2015

5. Cobalt-based age models of pelagic clay in the South Pacific Gyre;Dunlea;Geochemistry Geophysics Geosystems,2015

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