Results 221 to 230 of about 376,087 (268)

Weak mantle wedge causes mantle exhumation punctuated with discrete oceanic crust in the Tyrrhenian basin. [PDF]

Nat Commun
Su H, Leng W, Liao J, Brune S.
europepmc   +1 more source

Modern arc-like water content in the source of 3.1-billion-year-old volcanic rocks. [PDF]

Nat Commun
Vandenburg ED, Nebel O, Smithies RH, Cawood PA, Miller LA, Millet MA, Capitanio FA.   +6 more
europepmc   +1 more source

Enhanced erosion by continental arc volcanism as a driver of the Cambrian Explosion. [PDF]

Nat Commun
Wu Y, Tian H, Fan H, Pogge von Strandmann PAE, Zhao W, Li J, Sun H, Gu H, Lu C, Liu X, Li T, Ji S, Peng P.   +12 more
europepmc   +1 more source

The Emergence of an Urable Earth: How Early Planetary Evolution Shaped the Chemical Window for Life's Origin. [PDF]

Life (Basel)
Guo M, Meng Z, Liu S, Redfern SAT.
europepmc   +1 more source

Craton-margin lithosphere drives rare earth element ore-forming carbonatite magmatism. [PDF]

Nat Commun
Chen C, Wang Y, Shcheka SS, Förster MW, Jiang W, Chen Y, Foley SF, Jacob DE, Liu Y.   +8 more
europepmc   +1 more source

Geodynamic models of continental subduction and obduction of overriding plate forearc oceanic lithosphere on top of continental crust

Tectonics, 2015
Continental subduction takes place in the final stage of subduction when all oceanic lithosphere is consumed and continental passive margin is pulled into the mantle.
Joao C. Duarte, Wouter P. Schellart, Sarah J Edwards   +2 more
exaly   +2 more sources

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Fragmentation of continental subduction is ending the Himalayan orogeny

Science Bulletin, 2023
After two continents collide, plate convergence and orogenesis are sustained because subducted continental lithosphere continues pulling the surface plate. It remains controversial how, why, and when continental plate convergence and collision slow down and eventually cease.
Xiaofeng, Liang, Yang, Chu, Bo, Wan, Ling, Chen, Lin, Chen, Eric, Sandvol, Stephen P, Grand, Yibing, Li, Minling, Wang, Xiaobo, Tian, Yun, Chen, Tao, Xu, Yang, Li, Wei-Qiang, Ji   +13 more
openaire   +2 more sources

Continental Deep Subduction Versus Subduction Cessation: The Fate of Collisional Orogens

Tectonics, 2023
AbstractThe contrasting fates of collisional orogens, that is, continental deep subduction or subduction cessation, are widely recognized by petrological, paleomagnetic and geophysical observations. However, the mechanisms of such different collisional modes, especially the dynamics of continental deep subduction, are controversial.
Pengpeng Huangfu, Zhong-Hai Li
exaly   +2 more sources

Thermal regime of continental subduction: The record from exhumed HP–LT terranes (New Caledonia, Oman, Corsica)

Tectonophysics, 2013
Unlike the thermal structures of present-day subduction or collision zones, the variety of possible thermal evolutions (or “thermal regimes”) accompanying the transient stage of continental subduction (i.e., the shift from oceanic subduction to ...
Philippe Agard
exaly   +2 more sources