Results 41 to 50 of about 2,155,550 (190)
Our petrochemical studies on ~1.2 Ga granitoids of the Natal Metamorphic Belt, South Africa, do not suggest any property similar to Phanerozoic‐style subduction‐related granitoids. Plot of Kotongweni Tonalite in Y versus Sr diagram (after Moyen 2011), note that most samples have Sr/Y < 50.
Palesa Leuta +2 more
wiley +1 more source
Large‐volume lateral magma transport from the
AbstractLong‐distance lateral magma transport within the crust has been inferred for various magmatic systems including oceanic island volcanoes, mid‐oceanic ridges, and large igneous provinces. However, studying the physical and chemical properties of active fissure systems is difficult.
Osamu Ishizuka +3 more
openaire +3 more sources
U–Pb isotope and trace element geochemistry of apatite from carbonatites of Peshawar Plain Alkaline Igneous Province, western Himalaya shows Permo‐Carboniferous magmatism, an additional magmatic pulse during Cretaceous, and post‐magmatic hydrothermal/metasomatism during Oligocene. ABSTRACT U–Pb isotope and trace element geochemistry of apatite combined
Mehboob ur Rashid +9 more
wiley +1 more source
Channelized melt flow in downwelling mantle: Implications for 226Ra-210Pb disequilibria in arc magmas [PDF]
We present the results of an analytical model of porous flow of viscous melt into a steadily dilating ‘‘channel’’ (defined as a cluster of smaller veins) in downwelling subarc mantle.
Koenders, M. A. +7 more
core +1 more source
This multi‐omics study identified genetic loci, gut microbiota, blood metabolites, and gray matter volumes of orbitofrontal cortex and cerebellum that were potentially relevant to alerting in healthy Chinese adults. Subsequent two‐step one‐sample Mendelian randomization further revealed a serial mediation pathway: Bacteroides intestinalis influences ...
Hongru Li +8 more
wiley +1 more source
Insights on the state of stress in the mantle beneath Pahala, Hawai‘i
Magma supply rates from the mantle to Hawaiian volcanoes serve as an important control on eruptive behavior at the surface. The Pa ̄hala Sill Complex, a collection of magma-bearing, seismogenic structures at 40 km depth beneath Hawai‘i, presents an ...
John D. Wilding, Zachary E. Ross
doaj +1 more source
Image-based modelling of lateral magma flow: the Basement Sill, Antarctica [PDF]
The McMurdo Dry Valleys magmatic system, Antarctica, provides a world-class example of pervasive lateral magma flow on a continental scale. The lowermost intrusion (Basement Sill) offers detailed sections through the now frozen particle microstructure of
Nick Petford, Seyed Mirhadizadeh
doaj +1 more source
Time scales of magma transport and mixing at Kīlauea Volcano, Hawai’i [PDF]
Modeling of volcanic processes is limited by a poor knowledge of the time scales of storage, mixing and final ascent of magmas into the shallowest portions of volcanic ‘plumbing’ systems immediately prior to eruption. It is impossible to measure these timescales directly; however, micro-analytical techniques provide indirect estimates based on the ...
Rae, ASP +6 more
openaire +5 more sources
Amino‐silane treatment improves the basalt fiber–PA6 interface, enhancing composite performance. ABSTRACT Basalt fiber‐reinforced polymer (BFRP) composites have emerged as sustainable alternatives to glass fiber (GF) composites, but their performance is often controlled by the quality of the fiber–matrix adhesion.
Mohammad Mezbah Ul Hoque +3 more
wiley +1 more source
Low Viscosity of Peridotite Liquid: Implications for Magma Ocean Dynamics
Transport properties of silicate melts control magma ocean dynamics on the early terrestrial planets and rocky exoplanets. Here we calculate the viscosity (transport of momentum) of peridotite liquid at potential magma ocean conditions (0–159 GPa, 2,200 ...
D. Huang, Y. Li, M. Murakami
doaj +1 more source

