Voorbeelden van het gebruik van Continental crust in het Engels en hun vertalingen in het Nederlands
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On the continental crust this yields a row of volcanoes.
Always found as volcanic pipes over deep continental crust.
The felsic continental crust of today did not yet exist.
As you drive along, you're witnessing the growth of the continental crust.
The continental crust has an average composition similar to that of andesite.
The average composition of the continental crust is andesitic.
And if this has been going on for some considerable period of time, which we know it has, you can actually make very large amounts of continental crust in this way.
In contrast, the bulk of the continental crust is much older.
Partial melting of the Upper Mantle is held to have generated the continental crust.
The development of a continental crust eventually led to the formation of mountains.
Back-arcs can form on either oceanic crust or continental crust.
YouhavethePacificplate colliding with the continental crust and the Pacific plate is actually heavier and it slides underneath the continental crust.
Quartz is the second most abundant mineral in the Earth's continental crust, after feldspar.
The continental crust is typically from 30 km 20 mi to 50 km 30 mi thick and is mostly composed of slightly less dense rocks than those of the oceanic crust. .
The ultramafic ophiolite sequences which have been obducted onto continental crust are typically underlain by a mélange.
basaltic magma is trapped in the less dense continental crust, which is heated
are common in the continental crust but rare to absent in the oceanic crust. .
This small piece of continental crust was sandwiched in between the larger continents of Laurussia(to the north)
The Kaapvaal Craton formed and stabilised between 3.7 and 2.6 Ga by the emplacement of major granitoid batholiths that thickened and stabilised the continental crust during the early stages of an arc-related magmatism and sedimentation cycle.
These are rocks from the lower continental crust deformed and intruded by Variscan granites,