Results 111 to 120 of about 23,785 (261)
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
Modeling heat transfer from a convecting, crystallizing, replenished silicic magma chamber at an oceanic spreading center [PDF]
Lei Liu, R. P. Lowell
openalex +1 more source
Workshop on Magmatic Processes of Early Planetary Crusts: Magma Oceans and Stratiform Layered Intrusions [PDF]
The significance of the lunar highland pristine cumulate samples were reevaluated with the aid of the additional insights provided by geologically constrained terrestrial investigations.
Mccallum, I. S., Walker, D.
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Igneous Layering in Basaltic Magma Chambers
Layering is a common feature in mafic and ultramafic layered intrusions and generally consists of a succession of layers characterized by contrasted mineral modes and/or mineral textures, including grain size and orientation and, locally, changing mineral compositions.
Namur, Olivier +17 more
openaire +5 more sources
In situ probing of the present-day zircon-bearing magma chamber at Krafla, Northeastern Iceland [PDF]
Anastassia Y. Borisova +12 more
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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
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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
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Venus steep-sided domes: Relationships between geological associations and possible petrogenetic models [PDF]
Venus domes are characterized by steep sides, a circular shape, and a relatively flat summit area. In addition, they are orders of magnitude larger in volume and have a lower height/diameter ratio than terrestrial silicic lava domes.
Head, James W., III, Pavri, B.
core +1 more source

