Results 121 to 130 of about 265 (177)

Gravity modeling finds a large magma body in the deep crust below the Gulf of Naples, Italy. [PDF]

Sci Rep, 2018
Fedi M, Cella F, D'Antonio M, Florio G, Paoletti V, Morra V.   +5 more
europepmc   +1 more source

Geochemical baseline values and spatial distribution of major, trace, and rare earth elements in unpolluted soils of the Sicily region (Italy). [PDF]

Environ Geochem Health
Lo Medico F, Varrica D, Zuccolini MV, Miola M, Scopelliti G, Alaimo MG.   +5 more
europepmc   +1 more source

Rapid crystallization during recycling of basaltic andesite tephra: timescales determined by reheating experiments. [PDF]

Sci Rep, 2017
Deardorff N, Cashman K.
europepmc   +1 more source

The Crystal Chemistry and Topology of Modular Structures. III. 2D and 3D Zeolites Containing Tetrahedral Layers with the Apophyllite-Type Topology. [PDF]

Molecules
Aksenov SM, Chukanov NV, Rastsvetaeva RK, Pushcharovsky DY, Deyneko DV, Kalashnikova GO, Tananaev IG, Burns PC.   +7 more
europepmc   +1 more source

Xylogenesis reveals the genesis and ecological signal of IADFs in Pinus pinea L. and Arbutus unedo L. [PDF]

Ann Bot, 2018
Balzano A, Cufar K, Battipaglia G, Merela M, Prislan P, Aronne G, De Micco V.   +6 more
europepmc   +1 more source

Annotated checklist of Dermaptera and Zoraptera (Insecta) of Singapore, with redescriptions of several species. [PDF]

Zookeys
Kamimura Y, Cheah S, Wang WY, Lam WN.
europepmc   +1 more source

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An image of Mt. Vesuvius obtained by 2D seismic tomography

Journal of Volcanology and Geothermal Research, 1998
A high-resolution seismic tomography of Mt.Vesuvius was started in May 1994, with the aim of reconstructing the detailed shallow crustal structure underneath the volcano and define its feeding system. The first phase of the experiment was to perform a 2D profile, using three underground explosions as active sources.
Giuseppe De Natale, Giovanni Iannaccone, Paolo Capuano   +2 more
exaly   +6 more sources

The seismicity of Mt. Vesuvius

Tectonophysics, 1996
Abstract Over the last years, in order to improve the quality of the determination of earthquake locations as well as the reliability of the fault-plane solutions, three-component digital stations were temporarily added to the permanent seismic network of the Osservatorio Vesuviano operating in the Vesuvius area.
G. Vilardo, G. De Natale, G. Milano, U. Coppa   +3 more
openaire   +1 more source

Seismic Monitoring of Mt. Vesuvius by Array Methods

Seismological Research Letters, 2014
Mt. Vesuvius is a worldwide known active volcano located in Southern Italy, east of the city of Napoli. Its last eruption occurred in 1944, ending a continuous open‐conduit activity that lasted for more than three centuries. After then the volcano entered into a quiescent phase. Nonetheless, the explosive style of its past activity and its proximity to
LA ROCCA, MARIO, GALLUZZO D.
openaire   +3 more sources

3D Scattering Image of Mt. Vesuvius

Bulletin of the Seismological Society of America, 2009
In this article we apply a passive scattering-imaging method, derived from the method developed by Nishigami (1991) to data from the coda of the local volcano-tectonic (VT) earthquakes of Mt. Vesuvius. This method provides the space distribution of the strong scatterers together with a rough estimate of their strength.
A. Tramelli, E. Del Pezzo, M. C. Fehler
openaire   +1 more source