Results 111 to 120 of about 5,658 (224)
Owing to their abundance and relative availability on Earth's seafloor, mid‐ocean ridge basalts (MORBs) have a well‐defined chemical element budget, reflected by the low standard deviation associated with typical normal MORB (N‐MORB) composition. However,
Thomas Duvernay +3 more
doaj +1 more source
The Ghansura Rhyolite Dome (GRD) is an integral part of the Bathani volcano-sedimentary sequence (BVSs), which in turn is a vital component of the Chotanagpur Granite Gneiss Complex (CGGC), eastern India.
Gogoi Bibhuti, Basumatary Pallabi
doaj +1 more source
Magma chamber evolution during the 1650 AD Kolumbo eruption provides clues about past and future volcanic activity. [PDF]
Konstantinou KI.
europepmc +1 more source
Monomineralic anorthosites in layered intrusions are indicators of the magma chamber replenishment by plagioclase-only-saturated melts. [PDF]
Latypov R +5 more
europepmc +1 more source
THE PHLEGRAEAN FIELDS - MAGMA EVOLUTION WITHIN A SHALLOW CHAMBER
A systematic petrological and chemical study of the volcanic products of the Phlegraean Fields has been accomplished based on the new stratigraphy described by Rosi et al. (this volume). The majority of Phlegraean rocks belong to the "potassic" series of
ARMIENTI, PIETRO +7 more
core +1 more source
The Pomici di Mercato (PdM, 8,010±40 a), also known in the literature as Pomici Gemelle or Pomici di Ottaviano, is one of the oldest Plinian eruptions of Somma- Vesuvius.
Orsi, G +3 more
core +1 more source
Centrifuge experiments with magmatic systems : from melt segregation to pluton emplacement
In this thesis, laboratory investigations have been conducted to investigate several processes occurring during the melt segregation (crystal settling and compaction processes), as well as during emplacement of plutons.
Forien, Mélanie
core
Merensky-type platinum deposits and a reappraisal of magma chamber paradigms. [PDF]
Chistyakova S +3 more
europepmc +1 more source
V V Gordienko, L Ya Gordienko
openaire +1 more source
Zoned magma chamber of the Osuzuyama acid rocks, southwest Japan
The Osuzuyama acid igneous complex comprises voluminous pyroclastic deposits and lavas with dacitic to rhyolitic compositions. They represent magma which erupted from a compositionally zoned magma chamber without a detectable cooling hiatus.
Setsuya Nakada
core

