Results 111 to 120 of about 74,269 (283)
The Mobility of Major and Trace Elements in EOC Minerals on Parent Chondrite Bodies
The combined EPMA and SIMS study of the geochemical features of olivine, low-Ca pyroxene and plagioclase in equilibrated ordinary chondrites (EOCs) has revealed the effect of thermal metamorphism on trace element concentrations in EOC silicate minerals ...
Kristina Sukhanova, Sergey Skublov
doaj +1 more source
The anticipated performance of calorimeter crystals in the environment expected after the planned High-Luminosity upgrade of the Large Hadron Collider (HL-LHC) at CERN has to be well understood, before informed decisions can be made on the need for ...
Dissertori, G. +7 more
core +2 more sources
The geologic study of the Apulian Tavoliere plain (Apulia region, southern Italy) is extremely difficult due to the scarcity of outcrops and fauna that could be used for dating. The survey in progress of the 1:50,000 scale geological sheet no.
Caldara, Massimo +3 more
core +1 more source
The two largest deposits of Russia – Yaregskoye and Pizhemskoye belong to the same genetic type; hydrothermal-metamorphic indigenous deposits. They are located in the same Timan structure at a distance of no more than 230 km from each other. According to
A. B. Makeyev +4 more
doaj +1 more source
Geochemistry, Sm-Nd isotopes and SHRIMP U-Pb geochronology of the Morro do Coco Granite (RJ, Brazil): another piece of the post-collisional magmatism of the Ribeira Belt [PDF]
Fellippe Roberto Alves Bione +3 more
openalex +1 more source
Effect of Re-impacting Debris on the Solidification of the Lunar Magma Ocean
Anorthosites that comprise the bulk of the lunar crust are believed to have formed during solidification of a Lunar Magma Ocean (LMO) in which these rocks would have floated to the surface.
Abe +120 more
core +1 more source
Inferences of Source Lithologies for Chicxulub Microtektites Using a Bayesian Approach
The Chicxulub impact on the Yucatán Peninsula at the Cretaceous‐Paleogene boundary (KPB) was a likely contributor to the end‐Cretaceous mass extinction.
Jack Carter +5 more
doaj +1 more source
The palingenic calc-alkaline granitoid massifs of the Olekminsky complex form a magmatic belt stretching within the Western-Stanovoy terrane in the northeastern direction for more than 700 km.
S. I. Dril +6 more
doaj +1 more source
Is the gold standard tarnished? – understanding the limitations of high volume resolution U-Pb geochronology [PDF]
Martin J. Whitehouse
openalex +1 more source

