Results 201 to 210 of about 18,299,024 (255)
Petrogenesis and geodynamics of the Early Miocene Kashan granitoids in the central Urumieh-Dokhtar Magmatic Arc, Iran. [PDF]
Sci RepKou C, Zhang H, Zhu M.
europepmc +1 more source
Mantle Versus Crustal Contributions in Crustal-Scale Magmatic Systems (Sesia Magmatic System, Northern Italy) From Coupling Hf Isotopes and Numerical Modelling [PDF]
Contributions To Mineralogy and Petrology, 2021 The growth and evolution of crustal-scale magmatic systems play a key role in the generation of the continental crust, the largest eruptions on Earth, and the formation of metal resources vital to our society.
Silvano Sinigoi +2 more
exaly +4 more sources
Magmatic Sulfide Immiscibility at an Active Magmatic-Hydrothermal System: The Case of La Fossa (Vulcano, Italy) [PDF]
Journal of Volcanology and Geothermal Research, 2018 Magmatic sulfide minerals preserved in fresh volcanic rocks can be used to trace sulfur and chalcophile element evolution in magmatic systems and to constrain the potential magmatic contribution to ore-forming fluids.
Federico Di Traglia +2 more
exaly +2 more sources
Anatomy of an Extinct Magmatic System Along a Divergent Plate Boundary: Alftafjordur, Iceland
Geophysical Research Letters, 2015 Recent rifting episodes highlight the role of magmatic systems with propagating dikes on crustal spreading. However, our knowledge of magmatic systems is usually limited to surface observations and geophysical data.
Massimiliano Porreca +2 more
exaly +2 more sources
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Journal of the Virtual Explorer, 2010
The Ivrea-Verbano Zone (IVZ) and Serie dei Laghi (SdL) of northwest Italy, are two lithostratigraphic units that constitute the deep- and the middle- to upper-crustal components, respectively, of a tilted and exposed section through the pre-Alpine crust of northwest Italy.
Silvano Sinigoi +3 more
openaire +3 more sources
The Ivrea-Verbano Zone (IVZ) and Serie dei Laghi (SdL) of northwest Italy, are two lithostratigraphic units that constitute the deep- and the middle- to upper-crustal components, respectively, of a tilted and exposed section through the pre-Alpine crust of northwest Italy.
Silvano Sinigoi +3 more
openaire +3 more sources
Volatiles in Magmatic-Volcanic Systems
Elements, 2005The abundance and flux of volatiles are important to the hazards associated with explosive volcanic eruptions. Volatiles in magmas can be determined from investigations of melt and fluid inclusions in combination with volatile solubility data. A comparison of the newly determined solubilities of H2O, SO2, and Cl in a molten Vesuvius phonolite with the ...
DE VIVO, BENEDETTO +2 more
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Elements, 2006
An intimate physical and chemical interplay between crystals and melt in magmatic systems gives rise to a vast diversity of igneous rocks and the very structure of terrestrial planets. Yet the actual physical means by which this happens is unclear. The long-standing notion of crystals nucleating, growing, and settling ad infinitum from the interior of ...
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An intimate physical and chemical interplay between crystals and melt in magmatic systems gives rise to a vast diversity of igneous rocks and the very structure of terrestrial planets. Yet the actual physical means by which this happens is unclear. The long-standing notion of crystals nucleating, growing, and settling ad infinitum from the interior of ...
openaire +1 more source
Subduction systems and magmatism
Geological Society, London, Special Publications, 1994Abstract Most published subduction modelling and much palaeotectonic speculation incorporate the false assumption that subducting oceanic plates slide down fixed slots. In fact, hinges roll back into oceanic plates and slabs sink more steeply than the inclinations of the Benioff zones which define transient ...
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Experiments on Magmatic Model Systems
2020Experimental investigations in high-temperature quenching furnaces have provided invaluable contributions to our understanding of the parameters that control the crystallisation of minerals, mineral assemblages and rocks, especially from silicate liquids.
Martin Okrusch, Hartwig E. Frimmel
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