IN Bindeman - Reviews in Mineralogy and Geochemistry, 2021 - pubs.geoscienceworld.org
This Chapter considers triple oxygen isotope variations and their 4 Gyr temporal evolution in bulk siliciclastic sedimentary rocks and in granites. The d18O and∆′ 17O values provide …
The history of the growth of continental crust is uncertain, and several different models that involve a gradual, decelerating, or stepwise process have been proposed,,–. Even more …
M Agostini, K Altenmüller, S Appel, V Atroshchenko… - Physical Review D, 2020 - APS
This paper presents a comprehensive geoneutrino measurement using the Borexino detector, located at Laboratori Nazionali del Gran Sasso (LNGS) in Italy. The analysis is the …
S Dytłow, B Górka-Kostrubiec - Environmental geochemistry and health, 2021 - Springer
Geochemical background data are used to distinguish between the sources of heavy metal (natural or anthropogenic) and to categorize the level of heavy metal pollution. In this study …
Resolving the geochemical discrepancies between the bulk continental crust and its building blocks, basaltic arc magmas, can provide insights into the processes by which the …
Calcium stable isotopes were analyzed in well-characterized saprolite samples developed on a Mesozoic metadiabase dike near Cayce, South Carolina, to determine the degree and …
This study was carried out on a negligible anthropogenically impacted Indo-Bangla transboundary river basin (Atrai, Bangladesh) to elicit radionuclides' and elemental …
The transition from mafic to felsic upper continental crust (UCC) is crucial to habitability of Earth, and may be related to the onset of plate tectonics. Thus, defining when this crustal …
MP Ptáček, N Dauphas, ND Greber - Earth and Planetary Science Letters, 2020 - Elsevier
The nature of emerged continents through time is highly debated. Several studies relying on trace element data concluded that the Archaean crust was predominantly mafic, while Ti …