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...

Bibliográfalaš dieđut
Váldodahkkit:	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
Materiálatiipa:	Artihkal
Giella:	English
Almmustuhtton:	Wiley 2021-08-01
Ráidu:	Geochemistry, Geophysics, Geosystems
Fáttát:	Fe oxides nanophase material sedimentation sediment color redox‐stratified lake
Liŋkkat:	https://doi.org/10.1029/2020GC009582

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