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Statements

Subject Item
dbr:Intraplate_deformation
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dbr:Lower_crustal_flow
Subject Item
dbr:Lower_crustal_flow
rdfs:label
Lower crustal flow
rdfs:comment
In geodynamics lower crustal flow is the mainly lateral movement of material within the lower part of the continental crust by a ductile flow mechanism. It is thought to be an important process during both continental collision and .
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dbc:Geodynamics
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62015206
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1101690662
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dbr:Quartz dbr:Continental_break-up dbr:Andes dbr:Rheology dbr:Continental_collision dbr:Continental_crust dbr:Ductility_(Earth_science) dbr:Granodiorite dbc:Geodynamics dbr:Strain_rate dbr:Plagioclase_feldspar dbr:Geothermal_gradient dbr:Altiplano dbr:Brittle–ductile_transition_zone dbr:Bolivia dbr:Geodynamics dbr:Tibetan_plateau dbr:Diorite
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In geodynamics lower crustal flow is the mainly lateral movement of material within the lower part of the continental crust by a ductile flow mechanism. It is thought to be an important process during both continental collision and .
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