Titlebook: Rifted Ocean-Continent Boundaries; E. Banda,M. Torné,M. Talwani Book 1995 Springer Science+Business Media Dordrecht 1995 Atlantic Ocean.Co

Adrenal-Glands

PALL

J. J. Da?obeitia,R. W. Hobbs,J. H. McBride,T. A. Minshull,J. Gallart

CHOIR

Jean-Claude Sibuet,Véronique Louvel,Robert B. Whitmarsh,Robert S. White,Susan J. Horsefield,Bertrand

MERIT

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Lithosphere-Asthenosphere Interactions Below Rifts,he convective flow. The most vigorous flows occur when the rift is narrow and the transition from extended to unextended regions is sharp. The rate of extension is relatively unimportant for the parameter ranges explored here. The strain-rate dependence of viscosity is an important factor in determi

OFF

Finite Duration Rifting, Melting and Subsidence at Continental Margins, We present results from a uniform pure-shear lithospheric stretching model for melt generation and for subsidence at continental margins rifted at realistic finite rates. Predict ions from the model are compared with observations of melt generation and Subsidence from the ‘nonvolcanic’ Galicia Bank

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Gravity Anomalies and the Thermal and Mechanical Structure of Rifted Continental Margins,than adjacent oceanic lithosphere. Why stretched lithosphere is weak is enigmatic but. the lack of evidence of any hot-spot activity suggests that it is caused by rheological effects related to crustal composillon. rather than by reheating of the lithosphere following rifting . Despite a region of w

Androgen

Nature of Thin Crust Across the Southwest Greenland Margin and its Bearing on the Location of the Othe southern Labrador Sea, their symmetry across the extinct ridge, and their correlation with seafloor spreading models, strongly argue for their formation by seafloor spreading. Such an interpretation is also consistent with the plate kinematic motions derived for the North American and Eurasian P

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Anisotropy Measurements and the Deep Structure of a Passive Margin: Southwestern Greenland,ampling) have prevented the use of a nisotropy as a constraint for the determination of lower crustal composition in favor of estimates on Poisson’s ratio. Therefore, we suggest that anisotropy estimates can place new and more relevant constraints on the different rock types present in the deep crus

tendinitis

The Edge Experiment and the U.S. East Coast Magnetic Anomaly,ing reflectors alone are responsible for the ECMA. The crustal section here represents the Initial Oceanic Crust which is thicker and possesses higher seismic velocities than normal oceanic crust. It should not be called “transitional crust,” “modified continental crust,” or “rift stage crus!.” The