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Rare earth elements in the soil environment
SJ Ramos, GS Dinali, C Oliveira, GC Martins… - Current Pollution …, 2016 - Springer
Rare earth elements (REE) are a homogenous group of 17 chemical elements in the
periodic table that are key to many modern industries including chemicals, consumer …
periodic table that are key to many modern industries including chemicals, consumer …
Nature of parent rocks, mineralization styles and ore genesis of regolith-hosted REE deposits in South China: An integrated genetic model
Regolith-hosted rare earth element (REE) deposits, also called ion-adsorption or weathered
crust elution-deposited REE deposits are distributed over Jiangxi, Guangdong, Fujian …
crust elution-deposited REE deposits are distributed over Jiangxi, Guangdong, Fujian …
Quantifying chemical weathering intensity and trace element release from two contrasting basalt profiles, Deccan Traps, India
Weathering profiles developed on basalt substrate contain information relevant to climate,
atmospheric composition and evolution, nutrient release into the hydrosphere, and …
atmospheric composition and evolution, nutrient release into the hydrosphere, and …
Rare earth elements and neodymium isotopes in world river sediments revisited
Over the past decades, rare earth elements (REE) and their radioactive isotopes have
received tremendous attention in sedimentary geochemistry, as tracers for the geological …
received tremendous attention in sedimentary geochemistry, as tracers for the geological …
Quantitative paleoenvironmental and paleoclimatic reconstruction using paleosols
Paleosols (fossil soils) are preserved throughout the geologic record in depositional settings
ranging from alluvial systems to between basalt flows. Until recently, paleosols were studied …
ranging from alluvial systems to between basalt flows. Until recently, paleosols were studied …
The geochemistry of shales, siltstones and sandstones of Pennsylvanian–Permian age, Colorado, USA: implications for provenance and metamorphic studies
RL Cullers - Lithos, 2000 - Elsevier
A series of shales and sandstones found near the source of the Sangre de Cristo, Belden,
and Maroon Formations from central Colorado were examined petrographically and were …
and Maroon Formations from central Colorado were examined petrographically and were …
Contrasting geochemical and Sm-Nd isotopic compositions of Archean metasediments from the Kongling high-grade terrain of the Yangtze craton: evidence for …
S Gao, W Ling, Y Qiu, Z Lian, G Hartmann… - … et cosmochimica acta, 1999 - Elsevier
Twenty-three clastic metasediments from the Kongling high-grade terrain of the Yangtze
craton, South China were analyzed for major, trace and rare earth elements and Sm-Nd …
craton, South China were analyzed for major, trace and rare earth elements and Sm-Nd …
Geochemistry of sandstones from the Upper Miocene Kudankulam Formation, southern India: implications for provenance, weathering, and tectonic setting
JS Armstrong-Altrin, YI Lee… - Journal of …, 2004 - pubs.geoscienceworld.org
Petrographic, major, trace, and rare earth element compositions of sandstones from the
upper Miocene Kudankulam Formation, Southern India, have been investigated to …
upper Miocene Kudankulam Formation, Southern India, have been investigated to …
Geochemistry of the Mesoproterozoic Lakhanda shales in southeastern Yakutia, Russia: implications for mineralogical and provenance control, and recycling
RL Cullers, VN Podkovyrov - Precambrian Research, 2000 - Elsevier
Shales of the Lakhanda Group of Late Mezoproterozoic age (1050–1000 Ma) from the
southeastern Siberian craton in Russia have been analyzed for major elements and a …
southeastern Siberian craton in Russia have been analyzed for major elements and a …
A review on the potentiality of rare earth elements to trace pedogenetic processes
C Laveuf, S Cornu - Geoderma, 2009 - Elsevier
This review aims at considering the use of REEs to trace pedogenetic processes, in order to
quantify the respective contribution of the successive processes on pedogenesis. We first …
quantify the respective contribution of the successive processes on pedogenesis. We first …