Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Jarek Trela"'
Autor:
Esteban Gazel, Jarek Trela, Michael Bizimis, Alexander Sobolev, Valentina Batanova, Cornelia Class, Brian Jicha
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 8, Pp 2764-2779 (2018)
Abstract Mantle plume‐derived melts provide a unique glimpse into the chemical heterogeneity of the deep mantle. However, the exact processes involved in forming and sampling lower mantle heterogeneities remain unresolved and thus, require further
Externí odkaz:
https://doaj.org/article/b5782454466741de938e2763413eb905
Publikováno v:
Goldschmidt2022 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34556af551b6b9e4711b9e845e521065
https://doi.org/10.46427/gold2022.12740
https://doi.org/10.46427/gold2022.12740
Autor:
Juliane Gross, Jarek Trela, Eric C. Ferré, Justin Filiberto, B. L. Jolliff, Victoria E. Hamilton, P. K. Carpenter, Arya Udry, Andrea L. Meado, Axel Wittmann, Sarah C. Penniston-Dorland, Richard D. Ash, K. M. Cannon
Publikováno v:
Journal of Geophysical Research: Planets. 123:1823-1841
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3cc43cd4f5e90977c94b87ac4036f93
https://doi.org/10.1029/2018je005635
https://doi.org/10.1029/2018je005635
Autor:
Michael Bizimis, Valentina Batanova, Brian R. Jicha, Jarek Trela, Esteban Gazel, L. Moore, Alexander V. Sobolev
Publikováno v:
Nature Geoscience. 10:451-456
Earth’s mantle has cooled since the Archaean. Geochemical identification of anomalously hot lavas formed above the Galapagos Plume 89 million years ago, however, implies that a hot mantle reservoir may have persisted for billions of years.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad57c56a6d264bbd8fcfa9e867ec5cb8
https://doi.org/10.1038/ngeo2954
https://doi.org/10.1038/ngeo2954
Publikováno v:
The Mountain Geologist. 54:69-85
The Aycross Formation is the basal unit of the Absaroka Volcanic Supergroup in the southern Absaroka Range and consists of volcanic sandstone, mudstone, breccia, tuff and conglomerate. The Aycross was deposited during the waning stages of the Laramid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25ed5bcf1d7e5344b24ad3f6f901165b
https://doi.org/10.31582/rmag.mg.54.2.69
https://doi.org/10.31582/rmag.mg.54.2.69
Autor:
Jeffrey G. Ryan, C. Cannatelli, Sarah E. Mazza, Z. D. Atlas, Federico Lucchi, Benedetto De Vivo, Denis Zamboni, Esteban Gazel, Jarek Trela
Publikováno v:
Geochemistry, Geophysics, Geosystems. 17:2034-2053
The complex geodynamic evolution of Aeolian Arc in the southern Tyrrhenian Sea resulted in melts with some of the most pronounced along the arc geochemical variation in incompatible trace elements and radiogenic isotopes worldwide, likely reflecting
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b78977d822eecabc1ba20846a4e1e28a
https://doi.org/10.1002/2016gc006301
https://doi.org/10.1002/2016gc006301
Publikováno v:
Tectonophysics. 660:107-116
The magmatic processes responsible for accretion of new oceanic plutonic crust at fast-spreading centers remain unclear. Expedition 312, at Ocean Drilling Program Hole 1256D, on the eastern flank of the East Pacific Rise, barely drilled through the u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a6b536229a0ad1319c2078bc72358b6c
https://doi.org/10.1016/j.tecto.2015.08.023
https://doi.org/10.1016/j.tecto.2015.08.023
Autor:
Valentina Batanova, Jarek Trela, Esteban Gazel, Alexander V. Sobolev, Federico Lucchi, Denis Zamboni, Benedetto De Vivo, C. Cannatelli
Publikováno v:
Lithos
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
Artículos CONICYT
CONICYT Chile
instacron:CONICYT
The Aeolian arc (Italy) is characterized by some of the strongest along-the-arc geochemical variations in the planet, making it an ideal location to study the effect of subducting components in modifying the mantle source of island arc melts. Here, w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a3c5d9675f653ee222d6be803d1a23b
Publikováno v:
American Mineralogist. 99:601-606
Meteorite Northwest Africa (NWA) 6963 was classified as a basaltic shergottite based on mineralogy, but here we show that it is a gabbroic rock with a quartz-alkali feldspar intergrowth that represents a late-stage granitic melt. NWA 6963 contains cl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::341ab02cd30785d1291f27e118d55030
https://doi.org/10.2138/am.2014.4638
https://doi.org/10.2138/am.2014.4638