Results 121 to 130 of about 2,749 (215)
Paleoarchean deep crustal hydration and oxidation induced by subduction-driven water recycling. [PDF]
Zhou D +7 more
europepmc +1 more source
Fine‐root trait variation in temperate trees follows arc‐shape pattern along deep soil profiles
Root trait variation along the soil depth profile in four temperate tree species. Summary Roots are plants' interface with the soil, controlling access to water and nutrients. Yet, fine‐root trait variation along deep soil profiles and its functional implications remain poorly understood.
Katrin Pietig +3 more
wiley +1 more source
Unveiling the metallogenic continuum of an Archean craton. [PDF]
Demmer M, Ezad I, Fiorentini M.
europepmc +1 more source
ABSTRACT The Paleoproterozoic Talvivaara mudstone is a very large sulfidic Ni‐Co deposit that records enhanced organic matter accumulation during the global Shunga Event. Here, rock geochemistry and microscale S and Fe isotope composition of in situ pyrrhotites and pyrites are studied in well‐characterised, well‐preserved drill core samples.
Raimo Lahtinen +3 more
wiley +1 more source
Anatomy of a post-subduction collision. [PDF]
Şengül Uluocak E +3 more
europepmc +1 more source
The Seismic Expression of Core Complex‐Style Extensional Detachment Faults in Rifted Margins
ABSTRACT The identification of core complex‐style extensional detachment faults (CCDFs) in rifted margins is crucial for accurately restoring their stratigraphic and thermal histories. Yet recognising CCDFs in seismic reflection images is challenging due to their faint topographic expression; the lack of associated abrupt offset in seismic reflections;
Pauline Chenin +3 more
wiley +1 more source
Zinc isotope evidence for extensive carbonate recycling in the Arctic asthenosphere. [PDF]
Zhang WQ +11 more
europepmc +1 more source
Ductile Extrusion Triggered by Continental Collision in NE Brazil
ABSTRACT The Borborema Province in northeastern Brazil hosts one of the world's largest strike‐slip shear zone networks, active during the late Neoproterozoic assembly of West Gondwana. Whether these shear zones initiated during active continental collision or as a post‐orogenic response to far‐field stresses remains debated.
L. R. Tesser +6 more
wiley +1 more source

