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...

Celý popis

Podrobná bibliografie
Hlavní autoři: 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
Médium: Článek
Jazyk:English
Vydáno: Wiley 2021-08-01
Edice:Geochemistry, Geophysics, Geosystems
Témata:
Fe oxides
nanophase material
sedimentation
sediment color
redox‐stratified lake
On-line přístup:https://doi.org/10.1029/2020GC009582

Internet

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

Podobné jednotky