Andere Kunden interessierten sich auch für
![Evolution of Archean Crust and Early Life]( "Evolution of Archean Crust and Early Life")
Evolution of Archean Crust and Early Life79,99 €![Fluids in the Crust]( "Fluids in the Crust")
Fluids in the Crust153,99 €![Seismic response of the crust to stress changes]( "Seismic response of the crust to stress changes")
Seismic response of the crust to stress changes46,99 €![Anisotropy magnetic and density tomography subsoil and Earth crust]( "Anisotropy magnetic and density tomography subsoil and Earth crust")
Anisotropy magnetic and density tomography subsoil and Earth crust18,99 €![Faults in the Circumpolar Arctic crust]( "Faults in the Circumpolar Arctic crust")
Faults in the Circumpolar Arctic crust40,99 €![Evolution of Archean Crust and Early Life]( "Evolution of Archean Crust and Early Life")
Evolution of Archean Crust and Early Life74,99 €![The TRANSMED Atlas. The Mediterranean Region from Crust to Mantle]( "The TRANSMED Atlas. The Mediterranean Region from Crust to Mantle")
The TRANSMED Atlas. The Mediterranean Region from Crust to Mantle37,99 €
The continental crust is the layer of igneous, sedimentary, and metamorphic rocks which form the continents and the areas of shallow seabed close to their shores, known as continental shelves. This layer is sometimes called sial due to more felsic, or granitic, bulk composition, which lies in contrast to the oceanic crust, called sima due to its mafic, or basaltic rock.