Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Michael J. Vollinger"'
Publikováno v:
Geochimica et Cosmochimica Acta. 185:182-197
Geochemical analyses of stratigraphic sequences of lava flows are necessary to understand how a volcano works. Typically one sample from each lava flow is collected and studied with the assumption that this sample is representative of the flow compos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9580879c92addb87a05973b6d09198f9
https://doi.org/10.1016/j.gca.2016.01.015
https://doi.org/10.1016/j.gca.2016.01.015
Autor:
T. Boucher, Chloe H Anderson, J. Michael Rhodes, E. A. Breves, Sarah Byrne, Stephen Giguere, Caleb I. Fassett, Richard W. Murray, M. Darby Dyar, Michael J. Vollinger, K. H. Lepore
Publikováno v:
Applied spectroscopy. 71(4)
Obtaining quantitative chemical information using laser-induced breakdown spectroscopy is challenging due to the variability in the bulk composition of geological materials. Chemical matrix effects caused by this variability produce changes in the pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b40a47b7083747f630f019029ad48393
https://pubmed.ncbi.nlm.nih.gov/28374610
https://pubmed.ncbi.nlm.nih.gov/28374610
Autor:
Michael J. Vollinger, Dominique Weis, J. P. Marske, Michael O. Garcia, John M. Eiler, Andrew R. Greene, Aaron J. Pietruszka
Publikováno v:
Geochemistry, Geophysics, Geosystems. 14:4849-4873
[1] Geochemical time series analysis of lavas from Kīlauea's ongoing Pu‘u ‘Ō‘ō eruption chronicle mantle and crustal processes during a single, prolonged (1983 to present) magmatic event, which has shown nearly two-fold variation in lava eff
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7d19ae6dacd0aa2580032cbcf4e39ed
https://doi.org/10.1002/ggge.20285
https://doi.org/10.1002/ggge.20285
Autor:
J. M. Rhodes, Michael J. Vollinger
Publikováno v:
Geochemistry, Geophysics, Geosystems. 5
[1] This paper presents major and trace element compositions of lavas from the entire 3098 m stratigraphic section sampled by phase-2 of the Hawaii Scientific Drilling Project. The upper 245 m are lavas from Mauna Loa volcano, and the lower 2853 m ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cf6350fbda0565f41808c404b21d6e8
https://doi.org/10.1029/2002gc000434
https://doi.org/10.1029/2002gc000434