Results 211 to 220 of about 62,454 (271)
Water Versus Land on Temperate Rocky Planets. [PDF]
Guimond CM +8 more
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<i>In situ</i> microseismicity reveals lithospheric accretion at the ultraslow-spreading Gakkel Ridge, Arctic Ocean. [PDF]
Yu Z +10 more
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Slab tearing and segmented subduction termination driven by transform tectonics. [PDF]
Shuck B +14 more
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Basal mantle structure regenerated through supercontinents. [PDF]
Peng P +8 more
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Constraints of middle-late Permian granites in Eastern Inner Mongolia on the final subduction of the Paleo Asian Ocean. [PDF]
Zhao C, Yu Y, Liu Y, Cai H, He J, Gao X.
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The location of compression-induced subduction initiation controlled by structural versus thermal inheritance. [PDF]
Oravecz É, Gerya T, Balázs A.
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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
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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
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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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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
openaire +1 more source
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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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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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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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
openaire +1 more source

