Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Ramon Espinasa Perena"'
Autor:
Andres Sandoval-Velasquez, Andrea Luca Rizzo, Alessandro Aiuppa, Susanne M. Straub, Arturo Gomez-Tuena, Ramon Espinasa-Perena
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The abundance of mantle-derived rocks and lavas, in combination with its tectonic evolution, render Mexico a perfect laboratory to investigate the chemical and the isotopic heterogeneity of the lithospheric mantle. New data on the composition of nobl
Externí odkaz:
https://doaj.org/article/39caff279dc74206acd642e8e81028df
Autor:
Susanne M Straub, Valentina Batanova, Alexander Sobolev, Arturo Gómez-Tuena, Ramon Espinasa-Perena, W. Lindsay Fleming, Ilya Bindeman, Finlay Stuart, Elisabeth Widom
Publikováno v:
Goldschmidt2022 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41e88410ede7dc1fbb1ec49ca1e21fa6
https://doi.org/10.46427/gold2022.10611
https://doi.org/10.46427/gold2022.10611
Autor:
Andres Sandoval Velasquez, Andrea Luca Rizzo, Alessandro Aiuppa, Maria Luce Frezzotti, Susanne M Straub, Arturo Gómez-Tuena, Ramon Espinasa Perena
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f4a5a496c3403438fe5a4d1a62c30019
https://hdl.handle.net/10281/428983
https://hdl.handle.net/10281/428983
Autor:
G. Gisbert, Hugo Delgado-Granados, Ramon Espinasa-Perena, Martin Mangler, Chiara Maria Petrone, Julie Prytulak
Publikováno v:
Journal of the Geological Society. 179
Popocatepetl is one of the most active volcanoes in North America. Its current predominantly mild activity is contrasted by a history of large effusive and explosive eruptions and sector collapse events, which was first summarised by Espinasa-Perena
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::54616703dd0f4d3ff8d6ad7b071aa098
https://doi.org/10.1144/jgs2021-022
https://doi.org/10.1144/jgs2021-022
Autor:
José G. Cavazos-Tovar, Ramon Espinasa-Perena, Mattia Parolari, Susanne M. Straub, Arturo Gómez-Tuena
Publikováno v:
Lithos. 322:52-66
The origin, evolution and long-term preservation of andesitic continents within the context of destructive plate boundaries are still enigmatic for geoscientists. Here we use U Pb zircon geochronology and whole-rock geochemical data of arc and forear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d20b2c402c4d738321062db498bc50a
https://doi.org/10.1016/j.lithos.2018.10.005
https://doi.org/10.1016/j.lithos.2018.10.005
Autor:
Andrea Luca Rizzo, Susanne M. Straub, Arturo Gómez-Tuena, Maria Luce Frezzotti, Alessandro Aiuppa, Andres Sandoval-Velasquez, Ramon Espinasa-Perena
The Ventura Espiritu Santo Volcanic Field (VESVF) and the Sierra Chichinautzin (SCN) are two monogenetic volcanic fields originated in different tectonic environments in the central portion of Mexico (continental rift and subduction). The VESVF is lo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee3ac8b74bf2e1b04d23728be07be380
https://doi.org/10.5194/egusphere-egu2020-17010
https://doi.org/10.5194/egusphere-egu2020-17010
Autor:
Philipp A. Brandl, Ramon Espinasa-Perena, Susanne M. Straub, Luigi Solari, Louise Bolge, Arturo Gómez-Tuena, Paola Vannucchi, Georg F. Zellmer, Ilya N. Bindeman, Finlay M. Stuart
Publikováno v:
Geochimica et Cosmochimica Acta. 166:29-52
Recycling of upper plate crust in subduction zones, or ‘subduction erosion’, is a major mechanism of crustal destruction at convergent margins. However, assessing the impact of eroded crust on arc magmas is difficult owing to the compositional si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::066aedaa1dee03304ae66b5366895be2
https://doi.org/10.1016/j.gca.2015.06.001
https://doi.org/10.1016/j.gca.2015.06.001
Autor:
Ana Lillian Martin-Del Pozzo, Finlay M. Stuart, Charles H. Langmuir, Georg F. Zellmer, Arturo Gómez-Tuena, Ramon Espinasa-Perena, Susanne M. Straub
Publikováno v:
Geological Society, London, Special Publications. 385:31-64
A fundamental question in the formation of orogenic andesites is whether their high melt SiO2 reflects the recycling of silicic melts from the subducted slab or the processing of basaltic mantle melts in the overlying crust. The latter model is widel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::35222ac021dfcaf0d3a95364838fc812
https://doi.org/10.1144/sp385.14
https://doi.org/10.1144/sp385.14
Autor:
Finlay M. Stuart, Charles H. Langmuir, Yue Cai, Ramon Espinasa-Perena, Arturo Gómez-Tuena, Ana Lillian Martin-Del Pozzo, G. T. Mesko, Susanne M. Straub, Georg F. Zellmer
Publikováno v:
Journal of Petrology. 54:1551-1554
LAMONT^DOHERTY EARTH OBSERVATORYAT THE COLUMBIA UNIVERSITY, 61 ROUTE 9W, PALISADES, NY 10964, USA CENTRO DE GEOCIENCIAS, UNIVERSIDAD NACIONAL AUTO¤ NOMA DE ME¤ XICO, QUERE¤ TARO 76230, ME¤ XICO INSTITUTE OF EARTH SCIENCES, ACADEMIA SINICA, 128 AC
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b6aa770c4073e3253f8af9d6f869c66
https://doi.org/10.1093/petrology/egt021
https://doi.org/10.1093/petrology/egt021
Autor:
Arturo Gómez-Tuena, Charles H. Langmuir, Finlay M. Stuart, Yue Cai, G. T. Mesko, Georg F. Zellmer, Ana Lillian Martin-Del Pozzo, Ramon Espinasa-Perena, Susanne M. Straub
Publikováno v:
Journal of Petrology. 54:665-701
Andesite petrogenesis is inextricably linked to plate processing at convergent margins. The details of andesite formation, however, remain poorly understood because the signatures of the initial arc mantle melts are often modified in the overlying cr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::094ed7c499a9692021ff71297e15b381
https://doi.org/10.1093/petrology/egs081
https://doi.org/10.1093/petrology/egs081