Results 31 to 40 of about 110,450 (295)

Using perovskite to determine the pre-shallow level contamination magma characteristics of kimberlite [PDF]

open access: yes, 2014
It remains difficult to obtain reliable geochemical signatures of uncontaminated kimberlite magma from bulk rock studies due to the combined effects of crustal assimilation and element mobility during post-emplacement alteration processes.
Hawkesworth, Chris J.   +2 more
core   +2 more sources

Research Progress on the Application of Strontium Isotope Analysis Techniques in Geology: A Review

open access: yesYankuang ceshi
Strontium (Sr) isotopes have unique geochemical properties, such as time dependence and environmental sensitivity. With the development of testing technology and theoretical systems, using Sr isotopes has become a key technique in geoscience research ...
Wuhui JIA   +4 more
doaj   +1 more source

Sr-isotope analysis of speleothems by LA-MC-ICP-MS: High temporal resolution and fast data acquisition [PDF]

open access: yes, 2017
Speleothems are well established climate archives. A wide array of geochemical proxies, including stable isotopes and trace elements are present within speleothems to reconstruct past climate variability.
Breitenbach, Sebastian   +5 more
core   +3 more sources

Sr-Nd-Pb isotope systematics of fine sediments from the modern rivers in SW Japan: Implications for sediment provenance of the Northwest Pacific

open access: yesJournal of Asian Earth Sciences: X, 2020
As reference data for comprehensive provenance analyses of deep-sea sediments in the Northwest Pacific region, we present Sr-Nd-Pb isotopic compositions of fine sediments sampled from 48 rivers in southwest Japan.
Yu Saitoh   +2 more
doaj   +1 more source

Comparison and Optimization of Sr Isotope Analysis in Carbonate Rocks by Multiple-step Leaching Method

open access: yesYankuang ceshi, 2023
BACKGROUNDMarine sedimentary carbonate rock is an important carrier for recording seawater information. The Sr isotope composition (87Sr/86Sr) of carbonate rocks can reflect the relative contribution of the continental crust and mantle to the Sr isotope ...
Xu PAN   +6 more
doaj   +1 more source

Уран-свинцевий ізотопний вік гранітів Вознесенського масиву (Інгульський мегаблок Українського щита) [PDF]

open access: yes, 2016
Уран-свинцевим ізотопним методом датовано монацити із гранітів Вознесенського масиву. Вік монациту, а отже і гранітів, становить 2034,6 ± 6,6 млн років.
Бондаренко, С.М.   +5 more
core   +2 more sources

Determination of strontium isotope ratios in plant samples by wet ashing digestion

open access: yesResults in Earth Sciences
Strontium isotope provenance analysis has been widely applied across multiple disciplines, including archaeology, food science, and forensics. The establishment of bioavailable ⁸⁷Sr/⁸⁶Sr maps, known as isoscapes, which rely on a substantial number of ...
Wenyan Cheng   +3 more
doaj   +1 more source

Conservation of 87Sr/86Sr During Wine-Making of White Wines: A Geochemical Fingerprint of Geographical Provenance and Quality Production

open access: yesFrontiers in Environmental Science, 2020
The measuring of 87Sr/86Sr in wine, grape, and bioavailable soil fraction samples with the same uncertainty of geological materials allows fully comparing the whole wine-production chain with the peculiar geochemical isotope signature of any geographic ...
Ines Tescione   +7 more
doaj   +1 more source

The IRHUM (Isotopic Reconstruction of Human Migration) database – bioavailable strontium isotope ratios for geochemical fingerprinting in France [PDF]

open access: yesEarth System Science Data, 2014
Strontium isotope ratios (87Sr / 86Sr) are a key geochemical tracer used in a wide range of fields including archaeology, ecology, food and forensic sciences.
M. Willmes   +9 more
doaj   +1 more source

Accurate spectroscopy of Sr atoms

open access: yes, 2005
We report the frequency measurement with an accuracy in the 100 kHz range of several optical transitions of atomic Sr : $^1S_0- ^3P_1$ at 689 nm, $^3P_1- ^3S_1$ at 688 nm and $^3P_0- ^3S_1$ at 679 nm.
28   +39 more
core   +3 more sources

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