Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Michal Camejo-Harry"'
Publikováno v:
Royal Society Open Science, Vol 11, Iss 5 (2024)
Intra-arc diversity in volcanic activity and composition is ubiquitous, but its underlying causes remain largely unresolved in many settings. In this work, we examine such variability in the Grenadines archipelago, southern Lesser Antilles arc. Here,
Externí odkaz:
https://doaj.org/article/3e249a8bdcde413695b4c1987c93e19e
Autor:
Elena Melekhova, Michal Camejo-Harry, Jon Blundy, Simon R Wallis, Catherine Annen, Barbara E Kunz, Frances E Jenner, Matthew Thirlwall
The Lesser Antilles volcanic arc is known for its magmatic diversity and unusually abundant plutonic xenoliths. Xenoliths from Petit St. Vincent (Grenadines’ archipelago) are particularly interesting because of their textural and petrogenetic range
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac096ce8f6b26e43bec1993a4478c21b
http://oro.open.ac.uk/82751/8/82751VOR.pdf
http://oro.open.ac.uk/82751/8/82751VOR.pdf
Publikováno v:
Journal of Volcanology and Geothermal Research. 373:1-22
Kick-'em-Jenny and Kick-'em-Jack are two submarine volcanoes located in the southern Lesser Antilles arc. We present data on the temporal and spatial compositional variations in lavas and melt inclusions from Kick-'em-Jenny and four lavas from Kick-'
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd6fba69f7bbe625618eef3b0c234208
https://doi.org/10.1016/j.jvolgeores.2019.01.023
https://doi.org/10.1016/j.jvolgeores.2019.01.023
Autor:
T. E. Christopher, Michal Camejo-Harry, Jon D Blundy, William Attridge, Richard Robertson, Elena Melekhova
Publikováno v:
Camejo-Harry, M, Melekhova, E, Blundy, J, Attridge, W, Robertson, R & Christopher, T 2018, ' Magma evolution beneath Bequia, Lesser Antilles, deduced from petrology of lavas and plutonic xenoliths ', Contributions to Mineralogy and Petrology, vol. 173, 77 . https://doi.org/10.1007/s00410-018-1504-z
Extrusive and intrusive igneous rocks represent different parts of a magmatic system and ultimately provide complementary information about the processes operating beneath volcanoes. To shed light on such processes, we have examined and quantified th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aef92b06757a73aa6cf9b0f2cc58917e
https://doi.org/10.1007/s00410-018-1504-z
https://doi.org/10.1007/s00410-018-1504-z