Results 211 to 220 of about 62,454 (271)

Water Versus Land on Temperate Rocky Planets. [PDF]

open access: yesSpace Sci Rev
Guimond CM   +8 more
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Slab tearing and segmented subduction termination driven by transform tectonics. [PDF]

open access: yesSci Adv
Shuck B   +14 more
europepmc   +1 more source

Basal mantle structure regenerated through supercontinents. [PDF]

open access: yesNat Commun
Peng P   +8 more
europepmc   +1 more source
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Ophiolites and oceanic crust

Nature, 1974
OPHIOLITES consist of a pseudostratiform sequence, of harzburgite, tectonite, ultramafic and mafic cumulates sometimes including gabbro and quartz diorite (plagiogranite) intrusions, dolerite dyke swarms, pillow lava1, and deep-sea sediments2–4. This assemblage occurs in all Phanerozoic mountain systems and is interpreted as fossil oceanic crust and ...
E. M. MOORES, E. D. JACKSON
openaire   +3 more sources

Oceanic Crust: ABSTRACT

AAPG Bulletin, 1979
The model presented is based on the interpretation of marine geophysical data, studies of dredged rocks, theoretical modeling, geologic investigations of ophiolite complexes on the continents, and results of deep-sea crustal drilling by JOIDES/IPOD. Along the axis of the midoceanic ridge system a zone of upwelling asthenosphere extends from the base of
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Pacific ocean crust

1991
The Pacific Ocean basin comprises about one third of the earth’s surface, or 49.8% by area of our planet’s oceans and seas. It includes the earth’s largest and fastest moving plate, the Pacific plate, in addition to the smaller Nazca, Cocos, Rivera, Juan de Fuca, Gorda and Explorer plates, three so-called microplates (Galapagos, Easter and Juan ...
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Density of the ocean crust

Nature, 1984
The density structure and average density of the oceanic crust have implications for various geological and geophysical problems, including interpretations of gravity data, the variation of lithospheric bouyancy in relation to age, and role and fate of the crust in subduction.
R. L. Carlson, G. S. Raskin
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