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- W2027572634 abstract "Abstract On the basis of results of physical modelling and an analysis of the relevant geological and geophysical data, the mechanism and regularity of rifting are studied. As a rule, rifting develops in extensive and long-living “hot” regions characterized by a reduced thickness of lithosphere. Rifts develop due to regional extension of the lithosphere in the hot regions and are zones of localization of deformation (neckings). The style of deformation and faulting in a necking are studied experimentally. The plastic layers of low strength in the continental crust play an essential role in rifting. Those places favourable for the localization of plastic deformation are related to the parameters (expressiveness) of these layers in various parts of a hot region. The development of a necking (rifting) is accompanied by replacement of the lower crust by high-strength mantle (ultrabasic) material. When there is an interruption of the extension, this might cause an effective strengthening of the lithosphere in the rift zones and results in jumps when tension is renewed. Modelling has indicated that rifts can form angular junctions and branching in hot spots and older faulting zones. Various generations of rifts can converge and intersect in a hot spot. In contrast to this, “cold” lithospheric zones of higher strength are detoured by rifts. Basic magmatism, including plateau basalts, is often present in such zones." @default.
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- W2027572634 date "1991-12-01" @default.
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- W2027572634 title "Mechanism of rifting: considerations based on results of physical modelling and on geological and geophysical data" @default.
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- W2027572634 doi "https://doi.org/10.1016/0040-1951(91)90172-o" @default.
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