Zobrazeno 1 - 7
of 7
pro vyhledávání: '"M. E. van Zalinge"'
Autor:
M. E. van Zalinge, D. F. Mark, R. S. J. Sparks, M. M. Tremblay, C. B. Keller, F. J. Cooper, A. Rust
Publikováno v:
Van Zalinge, M E, Mark, D F, Sparks, R S J, Tremblay, M, Keller, C B, Cooper, F J & Rust, A C 2022, ' Timescales for pluton growth, magma-chamber formation and super-eruptions ', Nature, vol. 608, no. 7921, pp. 87-92 . https://doi.org/10.1038/s41586-022-04921-9
Generation of silicic magmas leads to emplacement of granite plutons, huge explosive volcanic eruptions and physical and chemical zoning of continental and arc crust1,2,3,4,5,6,7. Whereas timescales for silicic magma generation in the deep and middle
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::83dcdf9cb9b3f5191e9309409092195c
https://hdl.handle.net/1983/821b4eec-a41a-4a35-a528-46f45f34aacd
https://hdl.handle.net/1983/821b4eec-a41a-4a35-a528-46f45f34aacd
Publikováno v:
Nature. 608(7921)
Generation of silicic magmas leads to emplacement of granite plutons, huge explosive volcanic eruptions and physical and chemical zoning of continental and arc crust
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::e887a3d95891b6fd546c053aaf815897
https://pubmed.ncbi.nlm.nih.gov/35922502
https://pubmed.ncbi.nlm.nih.gov/35922502
Publikováno v:
Van Zalinge, M E, Sparks, R S J, Cooper, F J & Condon, D J 2016, ' Early Miocene large-volume ignimbrites of the Oxaya Formation, Central Andes ', Journal of the Geological Society, vol. 173, no. 5, pp. 716-733 . https://doi.org/10.1144/jgs2015-123
During the early Miocene ignimbrite flare-up, significant parts of the Central Andes (17–20°S) were covered by large-volume ignimbrites. High-precision 206 Pb/ 238 U zircon dates constrain the flare-up in northern Chile at c. 18°S to a 3 myr peri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::15b71c4a5baec84ce9e090947e1edea2
https://doi.org/10.1144/jgs2015-123
https://doi.org/10.1144/jgs2015-123
Publikováno v:
van Zalinge, M E, Cashman, K V & Sparks, R S J 2018, ' Causes of fragmented crystals in ignimbrites : a case study of the Cardones ignimbrite, Northern Chile ', Bulletin of Volcanology, vol. 80, no. 3, 22 . https://doi.org/10.1007/s00445-018-1196-2
Broken crystals have been documented in many large-volume caldera-forming ignimbrites and can help to understand the role of crystal fragmentation in both eruption and compaction processes, the latter generally overlooked in the literature. This stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5706619c06cf38e7d8209a6e44e72de4
https://doi.org/10.1007/s00445-018-1196-2
https://doi.org/10.1007/s00445-018-1196-2
Publikováno v:
van Zalinge, M E, Sparks, R S J & Blundy, J D 2017, ' Petrogenesis of the large-volume cardones ignimbrite, Chile; development and destabilization of a complex magma-mush system ', Journal of Petrology, vol. 58, no. 10, pp. 1975-2006 . https://doi.org/10.1093/petrology/egx079
The 21.9 Ma Cardones ignimbrite, a member of the early Miocene Oxaya Formation in northernmost Chile, is a crystal-rich (c. 40 vol. %) rhyolite with an extra-caldera thickness up to 1000 m. Access to core from eight c. 1 km drill holes allowed sampli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::231644ff8d86c6c624f64ffc0b792391
https://hdl.handle.net/1983/2b443d86-44e0-4926-8b80-6778ebcd5c25
https://hdl.handle.net/1983/2b443d86-44e0-4926-8b80-6778ebcd5c25
Autor:
Laura Evenstar, J. Aslin, R. S. J. Sparks, M. E. van Zalinge, Daniel J. Condon, Frances J. Cooper
Publikováno v:
Van Zalinge, M, Sparks, S, Evenstar, L, Cooper, F, Aslin, J & Condon, D 2017, ' Using ignimbrites to quantify structural relief growth and understand deformation processes : Implications for the development of the Western Andean Slope, northernmost Chile ', Lithosphere, vol. 9, no. 1, pp. 29-45 . https://doi.org/10.1130/L593.1
LITHOSPHERE
LITHOSPHERE
Large-volume ignimbrites are excellent spatial and temporal markers for local deformation and structural relief growth because they completely inundate and bury the underlying paleotopography and leave planar surfaces with relatively uniform, low-gra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9ad9f8457c0b9c5f64812812a6411665
http://www.scopus.com/inward/record.url?scp=85013422849&partnerID=8YFLogxK
http://www.scopus.com/inward/record.url?scp=85013422849&partnerID=8YFLogxK
Publikováno v:
Applied Earth Science. 126:55-56
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b37d0360f796ebce016cddc6ee6b7fb
https://doi.org/10.1080/03717453.2017.1306247
https://doi.org/10.1080/03717453.2017.1306247