Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Lucía Pérez Díaz"'
Cretaceous to earliest Oligocene plate motions between Greenland and North America are only modellable at high resolution from a short-lived (61-42 Ma) sequence of magnetic isochrons in the Labrador Sea. Understanding them at other times is hampered
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bcca706bd0ad7662b4b6e140bea38440
https://doi.org/10.5194/egusphere-egu22-6077
https://doi.org/10.5194/egusphere-egu22-6077
Publikováno v:
Geology
Geology, Geological Society of America, 2020, 48 (12), pp.1169-1173. ⟨10.1130/G47859.1⟩
EPIC3Geology
Geology, 2020, 48 (12), pp.1169-1173. ⟨10.1130/G47859.1⟩
Geology, Geological Society of America, 2020, 48 (12), pp.1169-1173. ⟨10.1130/G47859.1⟩
EPIC3Geology
Geology, 2020, 48 (12), pp.1169-1173. ⟨10.1130/G47859.1⟩
It has been suggested that plume arrival at the base of the lithosphere introduces a push force that overwhelms the balance of torques driving plate circuits, leading to plate-tectonic reorganizations. Among the most compelling evidence in support of
Publikováno v:
Solid Earth, Vol 11, Pp 889-897 (2020)
Digital.CSIC. Repositorio Institucional del CSIC
instname
Digital.CSIC. Repositorio Institucional del CSIC
instname
In the geosciences, data are acquired, processed, analysed, modelled and interpreted in order to generate knowledge. Such a complex procedure is affected by uncertainties related to the objective (e.g. the data, technologies and techniques employed)
Publikováno v:
Nature Geoscience. 15:246-247
The processes that accommodated plate divergence between Greenland and North America are most confidently interpretable from a short-lived (61-42 Ma) sequence of magnetic isochrons in the Labrador Sea. Understanding of the preceding and following per
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c74cf971627ad1ced8b577ce1b20f419
https://doi.org/10.21203/rs.3.rs-840254/v1
https://doi.org/10.21203/rs.3.rs-840254/v1
Models of Cenozoic plate motions between Greenland and North America often use magnetic anomalies in the Labrador Sea and Baffin Bay regions. The crustal origin of some of the older magnetic signatures, (pre C24, Paleocene) is questioned, and these m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::132992c42906fcf2c400b9c49707735d
https://doi.org/10.5194/egusphere-egu21-2372
https://doi.org/10.5194/egusphere-egu21-2372
Plate reconstruction studies show that the Neotethys Ocean was closing due to convergence of Africa and Eurasia towards the end of the Cretaceous. The period around 75 Ma reflects the onset of cont...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5aa6d15e7a758b4315fcb71a77a5939a
https://doi.org/10.1002/essoar.10503298.2
https://doi.org/10.1002/essoar.10503298.2
Publikováno v:
Solid Earth, Vol 11, Pp 397-417 (2020)
EPIC3Solid Earth, Copernicus Publications, 11, pp. 397-417
EPIC3Solid Earth, Copernicus Publications, 11, pp. 397-417
Plate tectonic modellers often rely on the identification of “break-up” markers to reconstruct the early stages of continental separation. Along the Iberian-Newfoundland margin, so-called break-up markers include interpretations of old magnetic a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::567ece7831d35c9ffe1fdab2f8a1a771
https://www.solid-earth.net/11/397/2020/
https://www.solid-earth.net/11/397/2020/
Observations of the apparent links between plate speeds and the global distribution of plate boundary types have led to the suggestion that subduction may provide the largest component in the balance of torques maintaining plate motions. This would i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09ab74790dac73265173cae02cf70da1
https://doi.org/10.5194/egusphere-egu2020-5076
https://doi.org/10.5194/egusphere-egu2020-5076
The Iberian-Newfoundland conjugate margins are one of the most extensively studied non-volcanic rifted margins in the world. In recent years, researchers have focused their efforts at better understanding the earliest stages of continental rifting, o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ab48a2578b6915353ad92753df206b2
https://doi.org/10.5194/egusphere-egu2020-11068
https://doi.org/10.5194/egusphere-egu2020-11068