Zobrazeno 1 - 10
of 21
pro vyhledávání: '"B J, Collette"'
Autor:
J. Verhoef, B. J. Collette
Publikováno v:
Seamounts, Islands, and Atolls
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c77e4d58c2e3fda2bfc2f22b95227475
https://doi.org/10.1029/gm043p0391
https://doi.org/10.1029/gm043p0391
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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23 pages, 16 figures, 1 table
The data from a recent magnetic compilation by Verhoef et al. (1991) off west Africa were used in combination with data in the western Atlantic to review the Mesozoic plate kinematic evolution of the central North A
The data from a recent magnetic compilation by Verhoef et al. (1991) off west Africa were used in combination with data in the western Atlantic to review the Mesozoic plate kinematic evolution of the central North A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10e262835e8742188a8103100ee33af3
https://doi.org/10.1007/bf01674063
https://doi.org/10.1007/bf01674063
Autor:
J. M. Burgers, B. J. Collette
Publikováno v:
Selected Papers of J. M. Burgers ISBN: 9789401040884
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c91e2dd8b59a9db4d5a98c7108d545e
https://doi.org/10.1007/978-94-011-0195-0_27
https://doi.org/10.1007/978-94-011-0195-0_27
Autor:
B. J. Collette, Walter R. Roest
Publikováno v:
Journal of the Geological Society. 143:833-843
The Fifteen Twenty Fracture Zone offsets the Mid-Altantic Ridge over 195 km in a sinistral sense. It was surveyed in 1982 between 30 ° W and 60 ° , i.e. from anomaly 34 on the African plate to anomaly 34 on the American plate where it disappears as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1d1cbf5c1819f5f40492c840effb3408
https://doi.org/10.1144/gsjgs.143.5.0833
https://doi.org/10.1144/gsjgs.143.5.0833
Publikováno v:
Earth and Planetary Science Letters. 63:399-407
An analysis of the magnetic structure of Plato and Atlantis seamounts in the North Atlantic was made using the phase-shifting technique of Schouten [9]. The possibility of distinguishing the age of the seamounts from the age of their adjacent seafloo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7027fb22c5633ac5bfa0639d3c55f273
https://doi.org/10.1016/0012-821x(83)90113-9
https://doi.org/10.1016/0012-821x(83)90113-9
Autor:
Th. F. A. Mulder, B. J. Collette
Publikováno v:
Marine Geophysical Researches. 6:383-394
The basement topography and the free-air gravity along two profiles in the central North Atlantic between 16° and 25° N, crossing a number of fracture zones, were divided in three wavelength intervals. Two-dimensional modelling shows that the short
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b1ad51213bf6d63aee1b0acbe0bd5b8
https://doi.org/10.1007/bf00286251
https://doi.org/10.1007/bf00286251
Autor:
B. J. Collette
Publikováno v:
Journal of the Geological Society. 143:763-774
A morphology is presented for the typical cross-section of an inactive fracture zone in the Atlantic. Inactive fracture zones typically consist of an asymmetric valley to the young side of the fracture zone plane and a high wall or scarp to the old s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2056b7e2da7d29a3a8b3651fcda4d3f5
https://doi.org/10.1144/gsjgs.143.5.0763
https://doi.org/10.1144/gsjgs.143.5.0763
Publikováno v:
Nature. 308:527-531
Present-day spreading directions as represented by the active (transform fault) sections of fracture zones in the central North Atlantic do not fit a small circle pattern about a unique pole1–5, as recently confirmed by a ‘Gloria’ survey. Contr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::678b0c13814d79885fe21cf209bd2dac
https://doi.org/10.1038/308527a0
https://doi.org/10.1038/308527a0
Publikováno v:
Earth and Planetary Science Letters. 42:103-108
A clay model of the Mid-Atlantic Ridge between 12° and 15°N, based on a survey with 8-km line spacing, reveals the irregular character of the medium-scale ridge topography. The median valley is far from constant in cross-section, ranging from an as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e688ba468b476b0814ef1f8885d1a14
https://doi.org/10.1016/0012-821x(79)90194-8
https://doi.org/10.1016/0012-821x(79)90194-8
Publikováno v:
Geophysical Journal of the Royal Astronomical Society. 12:363-373
Summary Gravity measurements indicate that the post-Hercynian basins in the North Sea area are in isostatic equilibrium. This means that most probably the crust underwent a considerable thinning since the Permian. Part 1 describes the seismic program
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c09f175cc8b65d7e857aa845cd037d0
https://doi.org/10.1111/j.1365-246x.1967.tb03147.x
https://doi.org/10.1111/j.1365-246x.1967.tb03147.x