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- W84404554 abstract "The Moho is defined by an abrupt change in seismic velocity, which is often attributed to the petrological crust-mantle boundary. However, other types of transitions may explain observed pronounced seismic reflections, such as metamorphic changes in iso-chemical rocks from granulitic lower crustal rocks to eclogitic facies, pronounced shear zones, or magmatic intrusions. Therefore, it is of crucial importance to have high-resolution models of the seismic velocity around the Moho. Further, the seismic reflectivity in normal-incidence and wide-angle may provide valuable constraints on the structure at the crust-mantle boundary. In areas influenced by strong magmatism with mantle source, e.g. at rift zones and other extended regions, the resulting transition between crust and mantle may assume several forms." @default.
- W84404554 created "2016-06-24" @default.
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- W84404554 date "2010-05-01" @default.
- W84404554 modified "2023-09-23" @default.
- W84404554 title "Moho and magmatism in extensional settings" @default.
- W84404554 hasPublicationYear "2010" @default.
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