Results 201 to 210 of about 379,430 (254)
Zinc isotope evidence for extensive carbonate recycling in the Arctic asthenosphere. [PDF]
Zhang WQ +11 more
europepmc +1 more source
ABSTRACT Reconstructing the pressure–temperature–time (P–T–t) evolution of (ultra)high‐pressure rocks is essential for constraining subduction and collisional dynamics. Subduction zones are often investigated using basic eclogites, whereas nonbasic high‐pressure rocks remain comparatively understudied, potentially hindering a comprehensive ...
Otavio S. G. Silva +7 more
wiley +1 more source
Seismic and mineralogical evidence for an iron-rich mega-ultralow-velocity zone beneath Hawai'i. [PDF]
Kim D +3 more
europepmc +1 more source
Quantifying crustal stress in the Sinai Peninsula caused by gravitational potential energy and its tectonic implications. [PDF]
Jallouli C, Abdelfattah AK, Alzahrani H.
europepmc +1 more source
The mantle source of REE-rich alkaline silicate magmas can be enriched by continent-derived sediment subduction. [PDF]
Qiu KF +8 more
europepmc +1 more source
Basal mantle structure regenerated through supercontinents. [PDF]
Peng P +8 more
europepmc +1 more source
Missing molybdenum and the composition of the continental crust inferred from molybdenum isotopes. [PDF]
Tian Y +5 more
europepmc +1 more source
Modern arc-like water content in the source of 3.1-billion-year-old volcanic rocks. [PDF]
Vandenburg ED +6 more
europepmc +1 more source
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Diamonds and the Geology of Mantle Carbon
Reviews in Mineralogy and Geochemistry, 2013### Introduction Earth’s carbon, derived from planetesimals in the 1 AU region during accretion of the Solar System, still retains similarities to carbon found in meteorites (Marty et al. 2013) even after 4.57 billion years of geological processing.
Graham Pearson +2 more
exaly +3 more sources
Pure and Applied Geophysics, 1998
A brief outline is given on experimental studies carried out in the Minnesota Mineral and Rock Physics Laboratory of microstructural evolution and rheology of mantle mineral aggregates or their analogues, using a simple shear deformation geometry.
Shun-Ichiro Karato +2 more
exaly +3 more sources
A brief outline is given on experimental studies carried out in the Minnesota Mineral and Rock Physics Laboratory of microstructural evolution and rheology of mantle mineral aggregates or their analogues, using a simple shear deformation geometry.
Shun-Ichiro Karato +2 more
exaly +3 more sources

