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Subduction zones
Subduction zones are where sediments, oceanic crust, and mantle lithosphere return to and
reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's …
reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's …
Continental collision zones are primary sites for net continental crust growth—A testable hypothesis
The significance of the continental crust (CC) on which we live is self-evident. However, our
knowledge remains limited on its origin, its way and rate of growth, and how it has acquired …
knowledge remains limited on its origin, its way and rate of growth, and how it has acquired …
[HTML][HTML] Subduction zone geochemistry
Crustal recycling at convergent plate boundaries is essential to mantle heterogeneity.
However, crustal signatures in the mantle source of basaltic rocks above subduction zones …
However, crustal signatures in the mantle source of basaltic rocks above subduction zones …
Tectonic evolution of convergent plate margins and its geological effects
Oceanic lithosphere is generated at divergent plate boundaries and disappears at
convergent plate boundaries. Seafloor spreading and plate subduction together constitute …
convergent plate boundaries. Seafloor spreading and plate subduction together constitute …
The global range of subduction zone thermal models
We model 56 segments of subduction zones using kinematically defined slabs based on
updated geometries from Syracuse and Abers (2006) to obtain a comprehensive suite of …
updated geometries from Syracuse and Abers (2006) to obtain a comprehensive suite of …
Serpentinization of the forearc mantle
A wide range of geophysical and geological data indicate that extensive serpentinization in
the forearc mantle is both expected and observed. Large volumes of aqueous fluids must be …
the forearc mantle is both expected and observed. Large volumes of aqueous fluids must be …
Chemical geodynamics of mafic magmatism above subduction zones
The geochemical signatures of subducting crust have been identified in various types of
mafic igneous rocks at convergent plate boundaries, where island arc basalts (IAB) and …
mafic igneous rocks at convergent plate boundaries, where island arc basalts (IAB) and …
Contribution of syncollisional felsic magmatism to continental crust growth: a case study of the Paleogene Linzizong volcanic succession in southern Tibet
The Linzizong volcanic succession (~ 65–45 Ma) and the coeval batholiths (~ 60− 40 Ma) of
andesitic to rhyolitic composition represent a magmatic response to the India–Asia …
andesitic to rhyolitic composition represent a magmatic response to the India–Asia …
[كتاب][B] Global tectonics
P Kearey, KA Klepeis, FJ Vine - 2009 - books.google.com
The third edition of this widely acclaimed textbook provides a comprehensive introduction to
all aspects of global tectonics, and includes major revisions to reflect the most significant …
all aspects of global tectonics, and includes major revisions to reflect the most significant …
[كتاب][B] Energy in nature and society: general energetics of complex systems
V Smil - 2007 - books.google.com
A comprehensive, systematic, analytically unified, and interdisciplinary treatment of energy
in nature and society, from solar radiation and photosynthesis to our fossil fuelled civilization …
in nature and society, from solar radiation and photosynthesis to our fossil fuelled civilization …