Results 111 to 120 of about 1,147,354 (242)
Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
In many basaltic eruptions, observations show that the effusion rate of magma has a typical dependence on time: the effusion rate curves show first a period of increasing and later a decreasing phase by a maximum value. We present a model to explain this
Antonello Piombo +2 more
doaj +1 more source
The shallow magma chamber of Stromboli Volcano (Italy)
In this work, we integrate artificial and natural seismic sources data to obtain high‐resolution images of the shallow inner structure of Stromboli Volcano. Overall, we used a total of 21,953 P readings from an active seismic experiment and an additional
D. Patanè +8 more
doaj +1 more source
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
Deccan Trap flood basalt volcanism reached its peak 65.5(±1)millionyears ago, giving rise to a 2.7km thick lava pile that formed the Western Ghats range near Mumbai.
Wolff, John A. +4 more
core +1 more source
THE SHALLOW MAGMA CHAMBER OF STROMBOLI
AbstractIn this work, we integrate artificial and natural seismic sources data to obtain high‐resolution images of the shallow inner structure of Stromboli Volcano. Overall, we used a total of 21,953 P readings from an active seismic experiment and an additional 2731 P and 992 S readings deriving from 269 local events.
Araceli García-Yeguas +9 more
openaire +1 more source
Merensky-type platinum deposits and a reappraisal of magma chamber paradigms. [PDF]
Chistyakova S +3 more
europepmc +1 more source

