Results 251 to 260 of about 7,532,149 (298)

Advances in the analytical methods of metal sulfide Re-Os isotope dating

open access: yesActa Petrologica Sinica, 2022
Over the past 30 years, the analytic technique of Re-Os isotope of geological samples has been developed and improved constantly, including sample digestion, chemical separation, mass spectrometry determination and micro region analysis methods, and Re ...
SUN ShengLing   +3 more
openaire   +2 more sources

The Re‐Os Isotopic System: A Review of Analytical Techniques

Geostandards Newsletter, 2002
Over the past twenty years, successive technological advances have transformed the Re‐Os isotopic system into one of the most powerful tools in isotope geochemistry. We present here a brief historical review of these advances and then describe and compare the methods most commonly used today.
Reisberg, Laurie, Meisel, Thomas
openaire   +2 more sources

Interpreting ages from Re–Os isotopes in peridotites

Lithos, 2009
Abstract Since the first application of the 187Re–187Os isotope system to determine the timing of melt extraction from peridotites twenty years ago, a plethora of studies have demonstrated its usefulness in dating melt depletion, hence, lithosphere formation in continental settings. However, these studies have also highlighted issues that affect this
Roberta L. Rudnick, Richard J. Walker
openaire   +1 more source

Re–Os elemental and isotopic systematics in crude oils

Geochimica et Cosmochimica Acta, 2007
Analysis of 12 worldwide oil samples show that Re and Os abundances are positively correlated with the asphaltene content of oil. Light oils with 83%), with
David Selby   +2 more
openaire   +1 more source

Microwave Digestion for Re-Os Isotope Measurements in Geological Samples

open access: yesAtomic Spectroscopy
In this study, we present the novel use of a microwave digestion system (CEM BLADE) to digest geological materials for Re-Os isotopic analysis. This technique employs quartz digestion vessels that are easy to clean and reusable, avoid the complicated ...
Mao, Guohua   +4 more
openaire   +2 more sources

The Aguablanca Ni-Cu Deposit: A Re-Os Isotope Study

International Geology Review, 2008
The Aguablanca Ni-Cu ore deposit is hosted by subvertical magmatic breccia bodies in which fragments of pyroxenite are cemented by sulfides. It is located within the Aguablanca Stock, which includes diorite, gabbro, norite and gabbronorite. Re-Os isotope data of magmatic pyrrhotite, chalcopyrite, and pentlandite and hydrothermal pyrite show that the Os
Ryan Mathur   +2 more
openaire   +1 more source

Re‐Os Isotopic Measurements at the Femtomole Level in Natural Samples

Geostandards Newsletter, 1997
Here we describe a new chemical separation method for Os and an improved mass spectrometric procedure for Re and Os. This technique is based on the selective extraction of OsO4 from aqueous solution in liquid bromine. Among other advantages, this procedure avoids the cumbersome distillation procedure for Os and uses only commercial “off the shelf” PFA ...
Jean Louis Birck   +2 more
openaire   +1 more source

Re-Os isotopic evidence for early differentiation of the Martian mantle

Geochimica et Cosmochimica Acta, 2000
Variations in the short-lived systems of 182Hf-182W and 146Sm-142Nd in the SNC meteorites indicate an early isolation of, and subsequent inefficient mixing between, mantle reservoirs in Mars. Correlations of eW and e142Nd with initial γOs are consistent with the Re-Os isotopic systematics of these meteorites being set during the earliest ...
A.D. Brandon   +3 more
openaire   +1 more source

Re-Os isotope systematics of sediments of the Brahmaputra River system

Geochimica et Cosmochimica Acta, 2003
Re-Os analyses were performed on suspended loads and coarser grained bank sediments of the Brahmaputra River system. Re and Os concentrations of these sediments vary from 7 to 1154 ppt and from 3 to 173 ppt, respectively. 187Os/188Os ratios range from 0.178 to 6.8, and thus vary from nearly mantle to very radiogenic crustal values.
Singh, Sunil   +2 more
openaire   +2 more sources

Re–Os isotopic evidence for a lower crustal origin of massif-type anorthosites

Nature, 2000
Massif-type anorthosites are large igneous complexes of Proterozoic age. They are almost monomineralic, representing vast accumulations of plagioclase with subordinate pyroxene or olivine and Fe-Ti oxides--the 930-Myr-old Rogaland anorthosite province in southwest Norway represents one of the youngest known expressions of such magmatism.
, Schiellerup   +5 more
openaire   +2 more sources

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