Results 221 to 230 of about 410,633 (280)

Lead isotope evidence for Antarctic Ice Sheet changes in the Weddell Sea sector since the Last Glacial Maximum

open access: yesBoreas, EarlyView.
The Weddell Sea influences global ocean circulation and sea level through modulating Antarctic Bottom Water formation and Antarctic Ice Sheet discharges, but the history of ice‐sheet dynamics in this region remains poorly constrained due to limited well‐dated geological records.
Huang Huang   +9 more
wiley   +1 more source

Spatial distribution and driving factors of molybdenum in soil in the Pearl river delta, China. [PDF]

open access: yesiScience
Wu Z   +9 more
europepmc   +1 more source

Synergistic Structuring and Stabilization of Arid Agro-Soils via a Binary Metacid-Chitosan Interpolymer Complex. [PDF]

open access: yesPolymers (Basel)
Kerimkulova M   +7 more
europepmc   +1 more source

Optimization of Cadmium Adsorption onto a Cellulose Acetate-Clay Composite Membrane Using Box-Behnken Design. [PDF]

open access: yesMolecules
Dhieb S   +6 more
europepmc   +1 more source

Accessory minerals as tracers of crustal processes

open access: yesChemical Geology, 2009
This Chemical Geology special issue stems from oral presentations given at two symposia held in 2007; Accessory minerals as tracers of crustal processes, at The Goldschmidt Conference in Koln, 19–24 August, 2007, and Internal textures, and trace element and isotope geochemistry in accessory minerals: Advances in imaging and in situ microanalysis, at ...
Gerdes, Axel   +3 more
openaire   +3 more sources

Sulfur-bearing Magmatic Accessory Minerals

open access: yesReviews in Mineralogy and Geochemistry, 2011
Almost all magmas contain sulfide- or sulfate-bearing phases. In most natural samples the sulfur-bearing phase is a sulfide, which typically is pyrrhotite (Fe1− x S) or pyrite (FeS2) although chalcopyrite (CuFeS2), pentlandite ((Fe,Ni)9S8), sphalerite (ZnS) or molybdenite (MoS2) may be present as well.
Parat, Fleurice   +2 more
openaire   +2 more sources

Home - About - Disclaimer - Privacy