Iron Mineralogy and Sediment Color in a 100 m Drill Core From Lake Towuti, Indonesia Reflect Catchment and Diagenetic Conditions

Iron Mineralogy and Sediment Color in a 100 m Drill Core From Lake Towuti, Indonesia Reflect Catchment and Diagenetic Conditions

Abstract Iron is the most abundant redox‐sensitive element on the Earth's surface, and the oxidation state, mineral host, and crystallinity of Fe‐rich phases in sedimentary systems can record details of water‐rock interactions and environmental conditions. However, we lack a complete understand...

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Detalles Bibliográficos
Main Authors: Rachel Y. Sheppard, Ralph E. Milliken, James M. Russell, Elizabeth C. Sklute, M. Darby Dyar, Hendrik Vogel, Martin Melles, Satria Bijaksana, Ascelina K. M. Hasberg, Marina A. Morlock
Formato: Artigo
Idioma:English
Publicado: Wiley 2021-08-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Fe oxides
nanophase material
sedimentation
sediment color
redox‐stratified lake
Acceso en liña:https://doi.org/10.1029/2020GC009582

Internet

https://doi.org/10.1029/2020GC009582

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