Zobrazeno 1 - 10
of 278
pro vyhledávání: '"M, Brenan"'
Publikováno v:
Geochimica et Cosmochimica Acta. 339:127-138
Publikováno v:
Geochimica et Cosmochimica Acta. 316:253-272
Several field-based studies have proposed that late-stage magmatic aqueous brines may be responsible for the transportation and redistribution of platinum-group elements (PGE) in mafic–ultramafic igneous systems. We experimentally studied the solub
Publikováno v:
Geochimica et Cosmochimica Acta. 316:230-252
We performed experiments to determine the solubility of Au and Pd in magmatic aqueous fluids as a function of oxygen fugacity (ƒO2), temperature (T), pH and total chloride concentration (Cltotal). Experiments were conducted at 800–1000 °C and 200
Publikováno v:
Science of The Total Environment. 887:163943
Autor:
H Wilson, M Brenan, H Rai, N Blake, H Mccann, G Blake, R Colleran, C Hanratty, N Begossi, R A Byrne
Publikováno v:
European Journal of Cardiovascular Nursing. 21
Funding Acknowledgements Type of funding sources: None. Background Patient-reported experience metric (PREM) questionnaires are an important tool for evaluating patient experience. Purpose Validated PREM tools may help to identify areas of quality im
Publikováno v:
Economic Geology. 115:1827-1833
There has been vigorous debate for several decades about whether the extreme enrichments of platinum group elements (PGEs) in some magmatic sulfide deposits could have resulted from simple equilibration of sulfide liquid with silicate melt. Key examp
Autor:
Bryan J. Maciag, James M. Brenan
Publikováno v:
Geochimica et Cosmochimica Acta. 276:198-218
This study applies X-ray absorption near edge structure (XANES) and extended X-ray absorption fine structures (EXAFS) spectroscopy at the K-edge to determine the speciation of arsenic and antimony in a suite of basaltic glasses synthesized over a ran
Autor:
Roisin Colleran, Gavin Blake, M Brenan, N Blake, Himanshu Rai, C Hanratty, Robert A. Byrne, H McCann, H Wilson
Publikováno v:
General posters.
Publikováno v:
Nature Geoscience. 12:701-706
The Moon accreted meteoritic material towards the end of Solar System formation. Quantification of this late accretion requires an estimation of the abundance of highly siderophile, or iron-loving, elements in the lunar mantle. As lunar mantle sample
Autor:
James M. Brenan, Natashia Drage
Publikováno v:
Goldschmidt2021 abstracts.