Results 131 to 140 of about 65,526 (293)
Geological evidence, including the presence of two passive margin platforms, juxtaposed and mismatched deformation between North America and more outboard terranes, as well as the lack of rift deposits, suggest that North America was the lower plate during both the Sevier and Laramide events and that subduction dipped westward beneath the Cordilleran ...
openaire +2 more sources
Sea-level stability over geological time owing to limited deep subduction of hydrated mantle
Nestor G. Cerpa +2 more
openalex +2 more sources
Physical and chemical properties of mantle sulfide and its geological implications [PDF]
Zhou Zhang
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Reconstruction of the Exhumed Mantle Across the North Iberian Margin by Crustal‐Scale 3‐D Gravity Inversion and Geological Cross Section [PDF]
Antonio Pedrera +6 more
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Oceanic igneous rocks throughout the Altai-Sayan Fold Belt (ASFB) in central-southern Siberia are often considered to be late Precambrian–early Paleozoic accreted elements of oceanic crust – often of uncertain paleogeographic or geodynamic origin.
Mongush Andrey Alexandrovich +1 more
doaj +1 more source
Length of day variations due to mantle dynamics at geological timescale [PDF]
M. Greff‐Lefftz
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Buffering of mantle conditions through water cycling and thermal feedbacks maintains magmatism over geologic time [PDF]
Johnny Seales +2 more
openalex +1 more source

