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pro vyhledávání: '"Tara Louise Stephens"'
Previous studies have suggested a link between rates of sea-level variation and eruptions globally [McGuire et al., 1997], with Satow and coauthors [2021] presenting the first detailed comparison between sea-level change and eruptive history for a si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1156eea06b226d397ac720a54628fde
https://doi.org/10.31223/x5961n
https://doi.org/10.31223/x5961n
Autor:
Catherine Greenfield, Richard Walker, Simon P.A. Gill, David Healy, Sam Poppe, Tara Louise Stephens
Publikováno v:
Volcanica, 4 (2
Volcanica, Vol 4, Iss 2, Pp 189-201 (2021)
Volcanica, Vol 4, Iss 2, Pp 189-201 (2021)
Inferences about sheet intrusion emplacement mechanisms have been built largely on field observations of intrusion tip zones: magmatic systems that did not grow beyond their observed state. Here we use finite element simulation of elliptical to super
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d4bd5624687959797e95e59eda50c5c1
https://doi.org/10.31223/x5c32m
https://doi.org/10.31223/x5c32m
Autor:
Ken McCaffrey, Richard Walker, Natalie Farrell, K.A. Wright, Richard England, Alodie Bubeck, Thomas G. Blenkinsop, David Healy, T.M. Kawanzaruwa, Tara Louise Stephens
Publikováno v:
Geological Society of America bulletin, 2017, Vol.129(9-10), pp.1052-1070 [Peer Reviewed Journal]
Igneous sills can facilitate significant lateral magma transport in the crust; therefore, it is important to constrain controls on their formation and propagation. Close spatial association between sills and dikes in layered (sedimentary) host rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d9e416f239fde140e208ecbaa2c815f6
Autor:
Richard England, Tara Louise Stephens, Richard Walker, Ken McCaffrey, Alodie Bubeck, David Healy
Publikováno v:
Earth and planetary science letters, 2017, Vol.478, pp.159-174 [Peer Reviewed Journal]
Sill emplacement is typically associated with horizontally mechanically layered host rocks in a near-hydrostatic far-field stress state, where contrasting mechanical properties across the layers promote transitions from dykes, or inclined sheets, to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a7eacdd360a6e790fe718fb3919abf6d