Zobrazeno 1 - 10
of 58
pro vyhledávání: '"Charlotte E. Keen"'
Publikováno v:
Tectonics. 37:1955-1972
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7c838c4f2f910ab0e46a69475d0e2e5c
https://doi.org/10.1029/2017tc004924
https://doi.org/10.1029/2017tc004924
Publikováno v:
Marine and Petroleum Geology. 89:443-463
Studies of the structural deformation and the nature of the ocean-continent transition zone at the rifted continental margin, offshore central Labrador, and its conjugate off West Greenland have been conducted over several decades and helped to defin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6264336675c2849040c881c78efd3e3c
https://doi.org/10.1016/j.marpetgeo.2017.10.012
https://doi.org/10.1016/j.marpetgeo.2017.10.012
Publikováno v:
Basin Research. 29:233-254
The stratigraphic, subsidence and structural history of Orphan Basin, offshore the island of Newfoundland, Canada, is described from well data and tied to a regional seismic grid. This large (400 by 400 km) rifted basin is part of the non-volcanic ri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f24b897e8986247519910d943507cb5a
https://doi.org/10.1111/bre.12147
https://doi.org/10.1111/bre.12147
Publikováno v:
Tectonics. 33:1133-1153
A mid-Cretaceous to Late Cretaceous volcanic province, named here the Charlie-Gibbs Volcanic Province, is described near the western termination of the Charlie-Gibbs Fracture Zone, against the rifted continental margin northeast of Newfoundland. We u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebc6679ab06404e507b4fd0fea24d601
https://doi.org/10.1002/2014tc003547
https://doi.org/10.1002/2014tc003547
Publikováno v:
Marine and Petroleum Geology. 28:1663-1675
The Labrador continental margin provides a rich source of data with which to study the relationships between stratigraphy, tectonics and paleoenvironment. We have completed a regional seismic interpretation and integrated this with new biostratigraph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c93457065ef19aad89bf584fe848dde2
https://doi.org/10.1016/j.marpetgeo.2011.05.009
https://doi.org/10.1016/j.marpetgeo.2011.05.009
Autor:
Charlotte E. Keen, R. R. Boutilier
Publikováno v:
Journal of Geophysical Research: Solid Earth. 105:13375-13387
We have explored the idea that observations of large igneous crustal thickness at volcanic rifted continental margins may be explained by the interaction of rift-driven flow in the lithosphere with an underlying, sublithospheric hot plume sheet. This
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25ad3b75e2de504a0257c3171c523301
https://doi.org/10.1029/2000jb900027
https://doi.org/10.1029/2000jb900027
Autor:
R. R. Boutilier, Charlotte E. Keen
Publikováno v:
Journal of Geophysical Research: Solid Earth. 104:7389-7403
This paper explores the suggestion that observations of large igneous crustal thickness at rifted volcanic margins may in part be explained by small-scale convection in the upper mantle. This may increase the delivery of magma to the overlying lithos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5c675d46008faff7d4d7c811812b09a1
https://doi.org/10.1029/1998jb900076
https://doi.org/10.1029/1998jb900076
Publikováno v:
Basin Research. 9:243-261
A two-layer lithospheric stretching model that includes the effects of decompression melting was used to estimate the deformation and thermal evolution of the Queen Charlotte Basin, British Columbia. The basin contains up to 6 km of Tertiary fill and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71285fe77b914949deb46add4dc31ba2
https://doi.org/10.1046/j.1365-2117.1997.00043.x
https://doi.org/10.1046/j.1365-2117.1997.00043.x