Results 121 to 130 of about 3,414 (186)

Breakup of strong cratonic lithosphere causes extensive magmatism at continental margins. [PDF]

Sci Rep
Wang S, Leng W.
europepmc   +1 more source

Magmatic domes and the initiation of oceanic processes at the Norwegian margin. [PDF]

Sci Rep
Peron-Pinvidic G.
europepmc   +1 more source

Paleoarchean deep crustal hydration and oxidation induced by subduction-driven water recycling. [PDF]

Sci Adv
Zhou D, Ge R, Wilde SA, Collins WJ, Kemp AIS, Lian D, Cai P, Wang X.   +7 more
europepmc   +1 more source

Origin of continental crust on early Earth. [PDF]

Natl Sci Rev
Zheng YF.
europepmc   +1 more source

Deciphering grain-size reduction as a driver of mid-lithosphere discontinuity formation. [PDF]

Sci Adv
Liu M, Gerya TV, Li ZH, Chen L, Connolly JAD.   +4 more
europepmc   +1 more source

Comment on Baas, J.H., Hewitt, W., Lokier, S. and Hendry, J. (2025) Coming to light: How effective are sediment gravity flows in removing fine suspended carbonate from reefs? The Depositional Record, 11, 583–598. doi: 10.1002/dep2.319

The Depositional Record, Volume 12, Issue 3, June 2026.
John J. G. Reijmer, Arnoud Slootman, Max de Kruijf   +2 more
wiley   +1 more source

Early Archaean subduction and intracrustal processes: experimental evidence from the East Pilbara Terrane, Australia. [PDF]

Nat Commun
Hastie AR, Law S, Young LA, Kemp AIS.
europepmc   +1 more source

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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
openaire   +1 more source

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   +1 more source

Chemical alteration of the oceanic crust

Geologische Rundschau, 1989
The alteration of the upper oceanic crust through sea water-basement rock interaction produces different and distinct alteration zones with increasing depth. The zonation generally shows a consistent worldwide pattern.
openaire   +2 more sources