continental-crust

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Examples of continental crust

  • Mixing calculations illustrate the possible effects of bulk assimilation of continental crust.

  • The derivation from or contamination with crustal material explains the observed similarity of the multi-element patterns to typical upper continental crust.

  • It is therefore likely that generation of the widespread intermediate-silicic magmas represents an early stage in the formation of continental crust.

  • This finding has important implications for the growth of the continental crust.

  • The larger modelled upper continental crust component is also consistent with the relative abundance of detrital mica of possible extra-basinal origin.

  • This is in agreement with return to more mafic detritus and the proposed increased upper continental crust contribution, together at the expense of felsic detritus.

  • Inevitably then, over the course of time, the volume of continental crust builds up.

  • The origin and accretionary history of the continental crust has long been debated by earth scientists.

  • Unshaded areas enclosed by solid lines are submerged continental crust.

  • One of these sources must be in the mantle and the other(s) in the continental crust.

  • The data confirm the interpretation of partial melting of, or considerable contamination by, old continental crust during magma generation and evolution.

  • This controls the way the continental crust responds to plate collision, earthquakes and aseismic slip in subduction zones, and mantle convection.

  • The partial melting conditions are similar to those assumed when basaltic continental crust partially melts to form active margin batholiths.

  • Cooling and contamination of mafic and ultramafic magmas during ascent through continental crust.

  • The crustal component could be provided by partial melting at the base of continental crust or by contamination of more mafic magma with crustal material.

Meaning of continental crust

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