Zobrazeno 1 - 10
of 85
pro vyhledávání: '"Ian D. Bastow"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 3, Pp n/a-n/a (2023)
Abstract Constraints on chemical heterogeneities in the upper mantle may be derived from studying the seismically observable impedance contrasts that they produce. Away from subduction zones, several causal mechanisms are possible to explain the inte
Externí odkaz:
https://doaj.org/article/94630b23c99c46bcbd4c083a5eb94605
Autor:
Thomas A. J. Merry, Ian D. Bastow, Rita Kounoudis, Christopher S. Ogden, Rebecca E. Bell, Laurence Jones
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 9, Pp n/a-n/a (2021)
Abstract The eastern Mediterranean hosts, within the span of a few hundred kilometers, extensional, strike‐slip, and collision tectonics above a set of fragmenting subducting slabs. Slab roll‐back, toroidal flow, and lithospheric dripping/delamin
Externí odkaz:
https://doaj.org/article/92ebd5ebc12b4ffba8a3f91a0a43efe6
Publikováno v:
Basin Research. 35:483-486
Publikováno v:
Rooney, T O, Brown, E L, Bastow, I D, Arrowsmith, J R & Campisano, C J 2023, ' Magmatism during the continent – ocean transition ', Earth and Planetary Science Letters, vol. 614, 118189 . https://doi.org/10.1016/j.epsl.2023.118189
As continents break apart, the dominant mechanism of extension transitions from faulting and lithospheric stretching to magma intrusion and oceanic crust formation in a new ocean basin. A common feature of this evolution preserved at magmatic rifted
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b259e641411ccd102ea427f6a0050a85
https://pure.au.dk/portal/da/publications/magmatism-during-the-continent--ocean-transition(7bb31bc2-888c-4d99-977e-517fb1f220f9).html
https://pure.au.dk/portal/da/publications/magmatism-during-the-continent--ocean-transition(7bb31bc2-888c-4d99-977e-517fb1f220f9).html
Autor:
Gareth L. Hurman, Derek Keir, Jonathan M. Bull, Lisa C. McNeill, Adam D. Booth, Ian D. Bastow
Magmatic intrusion and faulting both accommodate crustal extension in magma-rich rifts. However, quantitative constraints on the contribution of faulting to total extension and along-rift variations of faulting during the final stages of break-up are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f89998dc268520e3fd5aad9351535314
https://eprints.soton.ac.uk/477965/
https://eprints.soton.ac.uk/477965/
Continental breakup involves a transition from rapid, fault-controlled syn-rift subsidence to relatively slow, post-breakup subsidence induced by lithospheric cooling. Yet the stratigraphic record of many rifted margins contain syn-breakup unconformi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d73297d398e2354960963a7bd9465e3
The subdued topography of the Turkana Depression separates the elevated Ethiopian and Kenyan Plateaus in East Africa. Mechanisms to explain its topography are debated because constraints on upper m...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f83e94900a7fed035656a01ad7febf2
https://doi.org/10.1002/essoar.10508941.1
https://doi.org/10.1002/essoar.10508941.1
The eastern Mediterranean hosts, within the span of a few hundred kilometers, extensional, strike-slip, and collision tectonics above a set of fragmenting subducting slabs. Slab roll-back, toroidal flow, and lithospheric dripping/delamination process
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b34be6ca7c0873366f58b7ab2ca87cdc
http://hdl.handle.net/10044/1/90935
http://hdl.handle.net/10044/1/90935
Autor:
Cynthia Ebinger, Ian D. Bastow, M. Musila, R. Kounoudis, Atalay Ayele, B. A. Kibret, C. S. Ogden, Rebecca Bendick, Nicholas Mariita, G. Wigham, G. Kianji
The Turkana Depression, a topographically-subdued, broadly-rifted zone between the elevated East African and Ethiopian plateaus, disrupts the N–S, fault-bounded rift basin morphology that characterizes most of the East African Rift. The unusual bre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::73661577720d27ae70b8c7d558e1ffbe
http://hdl.handle.net/10044/1/90652
http://hdl.handle.net/10044/1/90652
Autor:
Hersh Gilbert, Thomas J. Owens, Melissa V. Bernardino, Ian D. Bastow, W. Levandowski, Craig H. Jones
Publikováno v:
Geosphere. 15:2018-2042
The Isabella anomaly, a prominent upper-mantle high-speed P-wave anomaly located within the southern Great Valley and southwestern foothills of the Sierra Nevada, has been interpreted either as foundering sub-Sierran lithosphere or as remnant oceanic