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In some areas of continental collision, the lower part of the thickened crust that results is interpreted to flow laterally, such as in the
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is the mainly lateral movement of material within the lower part of the
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flow mechanism. It is thought to be an important process during both
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Brune, S.; Heine, C.; Pérez-Gussinyé, M.; Sobolev, S.V. (2014).
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The tendency of the lower crust to flow is controlled by its
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Chen, L.; Capitanio, F.A.; Liu, L.; Gerya, T.V. (2017).
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240:Husson, L.; Sempere, T. (2003).
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297:-related article is a
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36:continental collision
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40:continental break-up
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100:Bolivian
68:dioritic
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