Results 71 to 80 of about 38,766 (189)
The Geochemistry of the Arabian Lithospheric Mantle--a Source for Intraplate Volcanism? [PDF]
DANISH LITHOSPHERE CENTRE, STER VOLDGADE 10, COPENHAGEN, 1350K, DENMARK DEPARTMENT OF GEOLOGY, ROYAL HOLLOWAY UNIVERSITY OF LONDON, EGHAM TW20 0EX, UK SCHOOL OF EARTH SCIENCES, VICTORIA UNIVERSITY OF WELLINGTON, PO BOX 600, WELLINGTON, NEW ZEALAND DEPARTMENT OF EARTH SCIENCES, OREGON STATE UNIVERSITY, CORVALLIS, OR97331-5506, USA DEPARTMENT OF EARTH ...
J. E. Shaw +4 more
openaire +1 more source
Scaling the Swell: Plume‐Lithosphere Interaction and Its Signal in Dynamic Seafloor Topography
Abstract Hotspot swells provide key constraints for understanding plume‐lithosphere interaction. However, quantitative relationships between plume properties and swell morphology remain poorly constrained. Here, we use 3D regional geodynamic models with composite diffusion‐dislocation creep rheology to investigate plume‐lithosphere interaction for ...
Ziqi Ma +2 more
wiley +1 more source
Intraplate Lithospheric Deformation Forms Large Volcanic Regions
Large igneous systems form either in areas of thin lithosphere at or near plate boundaries or by mantle-melting anomalies in intraplate settings with comparatively thicker lithosphere. Decompression melting or flux melt dominate at plate boundaries. Intraplate magmatism relates to thermal or compositional anomaly in the mantle.
César R. Ranero +8 more
openaire +2 more sources
Following the termination of seafloor spreading in the South China Sea (SCS) basin, abundant intraplate volcanism widely spreads in the Indochina block, SCS basin, and Leiqiong area, forming the Southeastern Asian Basalt Province (SABP).
Xingli Fan +5 more
doaj +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
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
Segmented Moho Uplift and Implications for Magmatic Underplating Beneath the Datong Basin
Abstract Understanding how the deep crust responds to coupled tectonic and magmatic processes is essential for deciphering intracontinental rifting. We apply high‐resolution passive‐source reverse time migration to teleseismic P‐wave receiver functions recorded by a dense seismic array to image the Moho beneath the Datong Basin. Our observations reveal
Chunlong Li +6 more
wiley +1 more source
Abstract Large intraplate earthquakes are paradoxical because they occur far from active plate boundaries. Northern Hainan Island (South China) hosts the 1605 Qiongbei M7.5 earthquake within a volcanic province linked to the Hainan mantle plume. New shear‐wave velocity images reveal two shallow low‐velocity zones extending to ∼10 km depth: a stronger ...
Lue Yang +9 more
wiley +1 more source
Short-lived and discontinuous intraplate volcanism in the South Pacific: Hot spots or extensional volcanism? [PDF]
South Pacific intraplate volcanoes have been active since the Early Cretaceous. Their HIMU-EMI-EMII mantle sources can be traced back into the West Pacific Seamount Province (WPSP) using plate tectonic reconstructions, implying that these distinctive ...
Staudigel, Hubert +3 more
core +2 more sources
Evidence for long-lived (>100 Myr) continental intraplate volcanism: Mongolia since the last ocean closure [PDF]
Since the closure of the Mongol-Okhotsk Ocean in the Mesozoic, Mongolia has been in an intraplate tectonic setting; the nearest plate boundary being ∼3,000 km to the east, at the active Pacific subduction front.
Barry, Tiffany +9 more
core +3 more sources

