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

Madison

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Strength

Rifted Continental Margin off Mid-Norway, km wide rift lone. Uplift of the cen tral rift led to massive subaerial volcanism during breakup. Modeling of the margin history of vertical Illotion Illust consider large melt volumes eillplaced during hreakup, presently constituting lower crust;tI high-velocity bodies.

使迷醉

ELATE

Book 1995sional stresses thatmay cause break-up. One part of the book is dedicated to currentknowledge of the structure and evolution of various Atlantic margins.After a brief incursion into the Mediterranean, succeeding articlesreport on the transform and active margins of the Ivory Coast-Ghanatransform margin and the Sea of Japan. .

生來(lái)

Book 1995ecific margins around the world.Special emphasis is placed on the structure and evolution of variousAtlantic margins. .After an introduction to volcanic margin concepts, the first articlesreport the results of numerical models of the mechanics of riftpropagation, melt generation and sources of exten

富饒

FIS

propose

Volcanic Margin Concepts,ing and after continental breakup. Whether a volcanic margin develops or not, i.e. the relative magnitude of magmatism during breakup, depends on the temperature and fluid content of the asthenosphere along the incipient plate boundary and the dynamic history of the lithosphere during the syn-rift p

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Lithosphere-Asthenosphere Interactions Below Rifts,nsequences of extension within the solid upper lithosphere. The flow is calculated using a two-dimensional, time-dependent formulation of the Navier -Stokes equations for an incompressible viscous fluid. The viscosity depends on temperature, pressure and strain-rate. Velocity boundary conditions on

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Finite Duration Rifting, Melting and Subsidence at Continental Margins,the a nhydrous manl le solidus. The qu antity of melt generated depends on four principal factors: the degree of lilhospheric thinning; the potential temperature of the asthenospheric mantle; the thickness of the lithosphere prior to rifting; and t he duration of rifting. Subsidence at rifted contin