Heavy oxygen recycled into the lithospheric mantle. [PDF]
AbstractMagmas in volcanic arcs have geochemical and isotopic signatures that can be related to mantle metasomatism due to fluids and melts released by the down-going oceanic crust and overlying sediments, which modify the chemistry and mineralogy of the mantle wedge.
Dallai L +4 more
europepmc +5 more sources
Lithospheric mantle buoyancy: the role of tectonic convergence and mantle composition. [PDF]
AbstractPlate subduction and delamination, two key processes driving plate tectonics, are thought to be controlled by the buoyancy of the lithospheric mantle relative to the underlying asthenosphere. Most mantle delamination models consider a lithospheric density higher than the asthenosphere to ensure negative buoyancy (slab pull).
Boonma K +4 more
europepmc +5 more sources
The role of an oxidized lithospheric mantle in gold mobilization. [PDF]
Phanerozoic orogenic gold mineralization at craton margins is related to the metasomatism of the lithospheric mantle by crustal material. Slab subduction transfers Au from the crust to the metasomatized mantle and oxidizes the latter to facilitate the mobilization of Au into mantle melts. The role of volatiles in the mobilization of Au in the mantle is
Qiu KF +10 more
europepmc +5 more sources
Modeling of the Arabian/Nubian shield’s geothermal structure: a multi-parametric analysis using geophysical and geological tools [PDF]
The Arabian-Nubian Shield (ANS) is a complex Neoproterozoic tectonic mosaic whose lithospheric structure and geothermal regime remain poorly constrained.
Menna Haggag +5 more
doaj +2 more sources
Breakup of strong cratonic lithosphere causes extensive magmatism at continental margins [PDF]
Extensive magmatism and Large Igneous Provinces (LIPs) may form at continental margins during continental breakup. While high mantle temperatures and geochemical fertility (such as plume activity) are typically considered the causes of magmatic ...
Shi Wang, Wei Leng
doaj +2 more sources
The subantarctic lithospheric mantle [PDF]
Abstract We present a summary of peridotite in the Subantarctic (46–60° S) surrounding the Antarctic Plate. Peridotite xenoliths occur on the Kerguelen Islands and Auckland Islands. The Kerguelen Islands are underlain by a plume, whereas the Auckland Islands are part of continental Zealandia, which is a Gondwana-rifted fragment. Small amounts
Guillaume Delpech +13 more
openaire +5 more sources
Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion [PDF]
Tectonic plate convergence is accommodated across the continental lithosphere via discrete lithospheric subduction or distributed shortening and thickening.
Xi Xu +14 more
doaj +2 more sources
The Accuracy Assessment of Lithospheric Density Models
The Earth’s synthetic gravitational and density models can be used to validate numerical procedures applied for global (or large-scale regional) gravimetric forward and inverse modeling.
Robert Tenzer, Wenjin Chen
doaj +1 more source
Imaging a Decratonized Lithosphere: A Case of the Eastern North China Craton
During decratonization, the cratonic lithosphere mantle experienced composition transformation and thinning, which have been extensively studied in the North China Craton.
Hongqiang Li +4 more
doaj +1 more source
Joint modeling of lithosphere and mantle dynamics elucidating lithosphere‐mantle coupling [PDF]
We provide new insights into the lithosphere‐mantle coupling problem through a joint modeling of lithosphere dynamics and mantle convection and through comparison of model results with the high resolution velocity gradient tensor model along the Earth's plate boundary zones.
A. Ghosh +4 more
openaire +1 more source

