Results 181 to 190 of about 376,087 (268)
Mineralogical evidence for continental deep subduction
openaire +1 more source
Abstract Following continental collision, the distal European margin was overridden by the Alpine wedge and is now largely concealed beneath the mostly intact orogenic lid. Consequently, the geological evolution and nature of the hidden basement domains remain poorly constrained.
Bianca Heberer +11 more
wiley +1 more source
Linking carbonatites, rare earth ores, and subduction-fertilized mantle lithosphere. [PDF]
Spandler C, Merdith AS, Griffin A.
europepmc +1 more source
Marine Geophysical Investigation of a Fault Ruptured During the 2012 Mw 8.6 Wharton Basin Earthquake
Abstract The 2012 Mw 8.6 and 8.2 Wharton Basin earthquakes, within an intraplate deformation zone in the Indian Ocean, are the largest instrumentally recorded strike‐slip earthquakes on Earth that challenged the prevailing view that great earthquakes occur only at well‐defined plate boundaries.
Saksham Rohilla +10 more
wiley +1 more source
Convergent mantle flow and plate kinematics contribute to South China Sea rifting. [PDF]
Li S +9 more
europepmc +1 more source
Abstract Detrital zircon U–Pb geochronology from Triassic–Jurassic basins in the New England Orogen (NEO) constrains sediment provenance and episodic continental arc evolution along the eastern Gondwanan margin. Dominant zircon clusters at 270–230 Ma and 340–300 Ma in these basins were likely sourced from contemporaneous magmatism in the NEO ...
Yanxiong Zhang +2 more
wiley +1 more source
Metamorphic evolution of amphibolite from Proto-Tethys South Altyn orogen and its geological significance. [PDF]
Zhang S, Ma T, Gai Y, Liu L.
europepmc +1 more source
Abstract Magmatic output in continental arcs is often variable, with short‐lived flare‐ups separated by prolonged lulls. Flare‐ups commonly coincide with increased crustal thickness, which has been interpreted as both a cause and a consequence of elevated magmatism.
Sourav Karmakar +4 more
wiley +1 more source
Inboard advance of arc magmatism regulates mountain building in the Andes. [PDF]
Capaldi TN +4 more
europepmc +1 more source
Abstract Arc volcanism is commonly interpreted as the surface expression of subduction‐related magmatism and its spatial organization is often controlled by lithospheric structures. In arc‐back‐arc systems, slab retreat may promote the transition from compression to extension and the development of Subduction‐Transform Edge Propagator (STEP) faults ...
L. Cocchi +4 more
wiley +1 more source

