Results 31 to 40 of about 1,408 (194)
Cenozoic Uplift and Volcanism of Hangai Dome, Central Mongolia Triggered by Lower Mantle Upwellings
The mechanisms of surface uplift of Hangai Dome (>2 km) and formation of Cenozoic intraplate volcanism in central Mongolia remain vigorously debated.
Yingkai Wu, Xuewei Bao
doaj +1 more source
The interaction between magmatic and tectonic processes in ocean intraplate volcanism yields insights into the ascent and transport of magmas. Many oceanic intraplate studies lack a temporal component and do not consider changes in tectonic regime and/or
René H. W. Romer +3 more
doaj +1 more source
Plume-induced post-spreading intraplate volcanism within and around the South China Sea
This dataset contains the manually picked surface wave dispersion data and the final inverted 3-D Vs model data for our research paper "Plume-induced post-spreading intraplate volcanism within and around the South China Sea"
Zhen Guo +5 more
core +1 more source
Tectonic significance of changes in post-subduction Pliocene-Quaternary magmatism in the south east part of the Carpathian-Pannonian Region [PDF]
The south-eastern part of the Carpathian–Pannonian region records the cessation of convergence between the European platform/Moesia and the Tisza–Dacia microplate.
Downes, H. +8 more
core +1 more source
A subduction and mantle plume origin for Samoan volcanism
The origin of Samoan volcanism in the southwest Pacific remains enigmatic. Whether mantle melting is solely caused by a mantle plume is questionable because some volcanism, here referred to as non-hotspot volcanism, defies the plume model and its linear ...
Vincent Strak, Wouter P. Schellart
doaj +1 more source
The occurrence of mantle-derived peridotite xenoliths in phonolitic melts is a rare phenomenon, and is commonly ascribed to a mantle origin of the phonolite.
Andreas Klügel +2 more
doaj +1 more source
Extreme intensity of fluid-rock interaction during extensive intraplate volcanism [PDF]
The compositional variability in large igneous provinces has mainly been attributed to changes in the melting regime and shallow crus- tal processes and commonly ranges from depleted tholeiitic basaltic to enriched alkaline lavas. Large igneous provinces
Stefan H. Krumm +14 more
core +1 more source
Although previous findings support an origin of the Shatsky Rise igneous plateau (Northwest Pacific) through interaction of a mantle plume with a mid‐ocean ridge triple junction, the evidence for the involvement of a mantle plume is equivocal.
Antje Dürkefälden +7 more
doaj +1 more source
The distribution of intraplate volcanism in the Pacific Ocean basin: a spectral approach [PDF]
Summary. Although the major linear island chains in the Pacific Ocean basin have been extensively studied, relatively little attention has been given to the origin of the numerous seamounts and oceanic islands that are concentrated in the western Pacific.
Ribe, N, Watts, A
openaire +2 more sources
The extensive and well-preserved lava fields, “harrats” in Arabic, of western Saudi Arabia stretch for 3000 km south to north and cover an area of more than 120.000 km2 in total. The alkalic volcanism initiated at ca.
Hansteen, Thor +6 more
core +1 more source

