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- W589993485 endingPage "379" @default.
- W589993485 startingPage "325" @default.
- W589993485 abstract "The great variety of forms of continental extension zones, or rifts, may result from the interaction of a small number of processes. Observational and theoretical studies have helped constrain the relative importance of those processes. At the most basic level, either mountain building or intrusion of basaltic magma is needed to heat and weaken the lithosphere enough to allow extension at reasonable tectonic force levels. Controversies persist over what controls the form of rifting, including what controls the dip angle of extensional faults, whether rifting is generally symmetrical or asymmetrical, and why some rifts are narrow and some are wide. Increasing evidence indicates that massive magmatic events coincide with most rifts. Both the genesis of pulses of mantle melting and the effect of magma on the lithosphere are not well understood. The fact that continents split to change the pattern of plate tectonics and produce economically important basins should keep interest high in deepening understanding of extensional processes." @default.
- W589993485 created "2016-06-24" @default.
- W589993485 creator A5016261729 @default.
- W589993485 date "2015-01-01" @default.
- W589993485 modified "2023-10-03" @default.
- W589993485 title "The Dynamics of Continental Breakup and Extension" @default.
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