Zobrazeno 1 - 10
of 41
pro vyhledávání: '"JAMES E. QUICK"'
Autor:
Lorenzo Tavazzani, Stefano Peres, Silvano Sinigoi, Gabriella Demarchi, James E. Quick, Rita C. Economos, Urs Klötzli
Construction of granitic magma chambers is recognized as a pivotal intermediate stage in the ascent of silicic magmas (SiO in excess of 65 wt%) through continental crust. However, the mechanisms by which large volumes (> 100 km ) of these highly crys
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::661e15156300e1e341de5bb8567c8c9e
http://hdl.handle.net/11368/2927977
http://hdl.handle.net/11368/2927977
Publikováno v:
Professional Paper. :461-488
During the ongoing eruption at Mount St. Helens, Washington, lava has extruded continuously at a rate that decreased from ~7-9 m 3 /s in October 2004 to 1-2 m 3 /s by December 2005. The volume loss in the magma reservoir estimated from the geodetic d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f95f2ade7b180026abdd126460989ccb
https://doi.org/10.3133/pp175022
https://doi.org/10.3133/pp175022
Publikováno v:
Journal of Petrology. 48:1185-1218
The Ivrea^Verbano Zone in the western Italian Alps contains one of the world’s classic examples of ponding of mantle-derived, mafic magma in the deep crust. Within it, a voluminous, composite mafic pluton, the Mafic Complex, intruded lower-crustal,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d9b4d9d077e130e96740230691475cef
https://doi.org/10.1093/petrology/egm014
https://doi.org/10.1093/petrology/egm014
Publikováno v:
International Geology Review. 47:203-214
The Trinity peridotite represents a rare opportunity to examine a relatively fertile plagioclase peridotite that was exhumed and later subjected to intrusive events in a seafloor environment, followed by its emplacement and incorporation into a conti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c76bf2868444207f984ec027f95f193
https://doi.org/10.2747/0020-6814.47.2.203
https://doi.org/10.2747/0020-6814.47.2.203
Publikováno v:
Earth and Planetary Science Letters. 166:31-45
A 1 to 1.5 km-thick, high-temperature shear zone is localized in wall rocks subparallel to the eastern intrusive contact of the Permian Mafic Complex of the Ivrea–Verbano zone (IVZ), Italy. The shear zone is characterized by concentrated ductile de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95cdca376b8638112e0a5fa82f033c73
https://doi.org/10.1016/s0012-821x(98)00280-5
https://doi.org/10.1016/s0012-821x(98)00280-5
Publikováno v:
The Journal of Geology. 106:609-622
The southern Ivrea‐Verbano Zone of the western Italian Alps contains a huge complex of mafic to intermediate plutonic rocks that intruded the lower continental crust during the Permian. Recent geologic mapping of the complex has characterized the e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4882962f62fca4d38f9c55cce59aac3e
https://doi.org/10.1086/516045
https://doi.org/10.1086/516045
Autor:
Urs Klötzli, Gabriella Demarchi, Kei Sato, Colombo Celso Gaeta Tassinari, Zekerias Günes, James E. Quick, Silvano Sinigoi
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
Advection of heat by the intrusion of mantle-derived magma is frequently invoked as the driver of high-temperature metamorphic events in the deep crust. One of the best places worldwide to study and evaluate this process is the deep crustal section o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2395308ff465c6e381b1144ab13d980a
Publikováno v:
Geological field trips 6 (2014). doi:10.3301/GFT.2014.05
info:cnr-pdr/source/autori:Mazzucchelli M.; Quick J. E.; Sinigoi S.; Zanetti A.; Giovanardi T./titolo:Igneous evolutions across the Ivrea crustal section: the Permian Sesia Magmatic System and the Triassic Finero intrusion/doi:10.3301%2FGFT.2014.05/rivista:Geological field trips/anno:2014/pagina_da:/pagina_a:/intervallo_pagine:/volume:6
info:cnr-pdr/source/autori:Mazzucchelli M.; Quick J. E.; Sinigoi S.; Zanetti A.; Giovanardi T./titolo:Igneous evolutions across the Ivrea crustal section: the Permian Sesia Magmatic System and the Triassic Finero intrusion/doi:10.3301%2FGFT.2014.05/rivista:Geological field trips/anno:2014/pagina_da:/pagina_a:/intervallo_pagine:/volume:6
The famous deep crustal section of the Ivrea-Verbano Zone (IVZ, western Alps, Fig. A) has received enormous attention over the last three decades as one of the best examples of continental "magmatic underplating". Recent investigations, comprising st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2845018234b3dad4b5d39a3d9940698
https://hdl.handle.net/11380/1054114
https://hdl.handle.net/11380/1054114
Publikováno v:
Bulletin of Volcanology. 57:44-51
Condensate samples were collected in 1992 from a high-temperature (300° C) fumarole on the floor of the Halemaumau Pit Crater at Kilauea. The emergence about two years earlier of such a hot fumarole was unprecedented at such a central location at Ki
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17926c598fb02b49fd08ab689ae784f6
https://doi.org/10.1007/bf00298706
https://doi.org/10.1007/bf00298706
Autor:
James E. Quick, Robert T. Gregory
Publikováno v:
The Journal of Geology. 103:187-198
The ascent of basaltic melts through the upper mantle results in chemical disequilibrium between the melts and the pyroxene and plagioclase of the wall-rock peridotite. Phase and cryptic variations in ophiolitic peridotites demonstrate that the resul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5eba038800117db4a19be6673ab2fc96
https://doi.org/10.1086/629735
https://doi.org/10.1086/629735