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This, combined with the young age of the oceanic crust, explains why few craters are likely to be found in the oceans.
The detached amphibolitized oceanic crust may then return to shallow depths as a result of its positive buoyancy against the denser surrounding mantle.
The basement is thought to be oceanic crust, generated either at a mid-ocean ridge or by back-arc spreading dependent on the favoured model.
The progressive contraction of oceanic crust caused the uplift of previously rifted continental margin and platforms and the formation of foredeep flysch basins.
Recycling of hydrated basalt of the oceanic crust and growth of early continents.
Fortunately, some portions of oceanic crust are occasionally preserved as ophiolites.
The progressive contraction of oceanic crust caused the uplift of previously rifted continental margin and platforms, and formation of foredeep flysch basins.
The majority of the oceanic crust formed today is created at intermediate- to fast-spreading ocean ridges.
This book contains a wealth of new data and new thinking on the whole problem of ophiolites and oceanic crust and upper mantle.
The students, whilst acknowledging excellent texts in igneous petrology or igneous geochemistry, felt the lack of a multi-disciplinary text specifically covering the generation and evolution of the oceanic crust.
Bioalteration of basaltic glass in the oceanic crust.
These pressures are equivalent to 57-46 km depth beneath an oceanic crust-mantle hanging-wall, a much greater thickness than can be accounted for by the thickness of the ophiolite.
Partial melting of subducting oceanic crust.
The evidence of hornblende crystallization implies that the ultramafites and associated gabbros were emplaced at depth in a crust considerably thicker than typical oceanic crust as represented by ophiolites.
The oceanic crust as a bioreactor.