Results 181 to 190 of about 17,487 (279)
Early Archaean subduction and intracrustal processes: experimental evidence from the East Pilbara Terrane, Australia. [PDF]
Hastie AR, Law S, Young LA, Kemp AIS.
europepmc +1 more source
Abstract Seafloor basalt samples recovered from the Caroline Basin (CB), the Parece Vela Basin (PVB), and the Western Philippine Sea Plate (WPSP) are analyzed for whole‐rock major and trace elements (including H2O), Sr‐Nd‐Pb‐Hf isotopes and 40Ar‐39Ar age‐dating.
Guo‐Liang Zhang +3 more
wiley +1 more source
The Mantle Fe<sup>3+</sup>/ΣFe Ratio Has Doubled Since the Early Archean. [PDF]
Zhu XX +4 more
europepmc +1 more source
Abstract Rifting is a tectonic process that leads to extensive magmatic activity, continental breakup, and the formation of new oceanic crust. The interplay between rifting and dynamic mantle flow driven by thermal heterogeneity in the mantle along the rift‐axis can influence magmatism and deformation beyond the rift zone.
Min‐Seok Jang, Byung‐Dal So
wiley +1 more source
Isotopic evidence for volatile loss driven by South Pole-Aitken basin-forming impact. [PDF]
Tian HC +9 more
europepmc +1 more source
Abstract The cratonic lithospheric mantle records complex metasomatic processes and is frequently tapped by alkaline magmatism, offering a unique opportunity to trace the progressive evolution of the mantle. In the present contribution, we investigate a newly identified calc‐alkaline lamprophyre field from the Neoarchean Jonnagiri Schist Belt, Eastern ...
Sourav Naskar +6 more
wiley +1 more source
Revisiting the scale of mantle plume-induced hot spot swells. [PDF]
Liu L +5 more
europepmc +1 more source
Abstract We present a comprehensive multidisciplinary investigation of the Healy submarine volcano in the southern Kermadec arc, northeast of New Zealand. We show the first results of sidescan‐sonar data collected at a submarine arc volcano by an Autonomous Underwater Vehicle (AUV).
A. Bagnasco +6 more
wiley +1 more source
Upper mantle low-velocity layer tied to volatile-charged carbonate melts. [PDF]
Huang Y +6 more
europepmc +1 more source
Abstract The origin of orthogonally spreading ridge segments separated by oceanic transform faults, versus obliquely spreading ridge segments without transform faults (TFs), is a long‐standing enigma of plate tectonics. We address this problem using three‐dimensional (3D) geodynamic models that simulate axial magmatic intrusions along two ridge ...
Garrett Ito +5 more
wiley +1 more source

