Shoshonitic enclaves in the high Sr/Y Nyemo pluton, southern Tibet: Implications for Oligocene magma mixing and the onset of extension of the southern Lhasa terrane [PDF]
, 2020 Post-collisional potassic and high Sr/Y magmatism in the Lhasa terrane provides critical constraints on the timing and mechanism of subduction of Indian lithosphere and its role in the uplift of the Tibetan Plateau.
Asimow, Paul D. +8 more
core
Geology and metallogeny of the upper mantle rocks from the Serranía de Ronda
, 2020 This research has been financially supported by the Spanish projects CGL201681085R, RTI2018-099157-A-I00, RYC-2015-17596 to JMGJ and the the research group (RNM 131) of the Junta de Andalucía. Additional funding for the edition of the printed version of the manuscript has been provided by the “Sociedad Española de Mineralogía (SEM)”.
Gervilla, Fernando +4 more
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Length of day variations due to mantle dynamics at geological timescale [PDF]
, 2011 M. Greff‐Lefftz
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, 2008 [1] Variations in the seismic velocity structure of the Himalayan collision zone include significant differences between its north and south portions, with transitions in physical properties across the Greater Himalaya.
G. Monsalve +3 more
semanticscholar +1 more source
Sea-level stability over geological time owing to limited deep subduction of hydrated mantle
, 2022 Nestor G. Cerpa +2 more
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Neogene plate tectonic reconstructions and geodynamics of North Island sedimentary basins: Implications for the petroleum systems [PDF]
, 2006 Although the modern Australia-Pacific plate boundary through New Zealand is relatively straight, there have been significant changes in its geometry during the Neogene. Within the North Island sector there has been a fundamental transition from an Alpine
Furlong, Kevin P., Kamp, Peter J.J.
core +1 more source
Olivine hydration in the deep upper mantle: Effects of temperature and silica activity
, 2006 Although water controls the biology and geology of the surface, hydrogen is perhaps the most poorly constrained compositional variable in the bulk Earth.
J.R Smyth +4 more
semanticscholar +1 more source
Geoscience Canada, 2014 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 ...
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Significance and Petrochemistry of Upper Mantle–mantle Transition Zone Metaperidotites and Oceanic Crust Metagabbros within the Kazdağı Metaophiolite: Implications for the Geological Evolution of the Izmir–Ankara–Erzincan Ocean, Northwestern Turkey [PDF]
, 2019 Ender Sarıfakıoğlu +3 more
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Constraining mantle density structure using geological evidence of surface uplift rates: The case of the African Superplume [PDF]
, 2000 Michael Gurnis +3 more
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