Results 31 to 40 of about 2,889,255 (157)
The rhyolitic ignimbrite and K‐feldspar granite porphyry from the Wangmushan mining district, northern Fujian yield ages of 173.8 ± 0.8 and 102.6 ± 0.4 Ma, respectively. Geochemical data, zircon trace elements, whole‐rock Sr–Nd–Pb isotope data, and zircon Hf isotopic compositions indicate that the rhyolitic ignimbrite originated from partial remelting ...
Wei Shaogang +7 more
wiley +1 more source
ABSTRACT The Fiorano quarry paleosol developed within the Colli Albani volcanic district (Italy) in the time interval bracketed by the deposition of the Pozzolanelle pyroclastic‐flow unit (365 ± 4 ka) and the emplacement of the Capo di Bove lava flow (277 ± 2 ka).
Eduardo Di Marcantonio +4 more
wiley +1 more source
Pyroclastic currents: observation and impact
A state-of-the-art and perspectives on the physical volcanology of pyroclastic currents and explosive eruptions (observation and impact) are given in this lecture for the Iceland Summer School 2021, EUROVOLC ...
Doronzo, Domenico
core +1 more source
An Open Database of Lunar Regolith and Simulants Properties
ABSTRACT Lunar regolith, the layer of unconsolidated material covering the Moon's surface, is central to the science and technology developed for the Moon, notably related to in‐situ science investigations, resource utilization, surface infrastructure, and mobility systems.
Léonie Gasteiner +2 more
wiley +1 more source
ABSTRACT Although central Brazil hosts significant ion‐adsorption rare earth element (REE) deposits associated with A‐type granites, their coeval volcanic counterparts have been largely overlooked as exploration targets. This study demonstrates that acidic metavolcanic rocks of the Araí Group share strong radiometric, geochemical and mineralogical ...
Yuri Ribeiro +3 more
wiley +1 more source
Effect of particle entrainment on the runout of pyroclastic density currents [PDF]
AbstractPyroclastic density currents (PDCs) can erode soil and bedrock, yet we currently lack a mechanistic understanding of particle entrainment that can be incorporated into models and used to understand how PDC bulking affects runout. Here we quantify how particle splash, the ejection of particles due to impact by a projectile, entrains particles ...
Fauria, Kristen E +2 more
openaire +3 more sources
ABSTRACT During the Middle Miocene Badenian Salinity Crisis (BSC), extensive evaporites formed across different tectonic settings in the Central Paratethys. Limited age constraints hamper evaporite correlation and identification of driving mechanisms. Here, we use U–Pb dating of zircon by LA‐ICP‐MS from tephra overlying the Tuzla Basin evaporites.
Nevena Andrić‐Tomašević +5 more
wiley +1 more source
Dynamics of pyroclastic density currents and submarine eruptions [PDF]
Density gradients are fundamental drivers of volcanic flows. Pyroclastic density currents propagate because they are more dense than the ambient fluid and pyroclasts can rise through water as a result of their buoyancy.
Fauria, Kristen
core +1 more source
Interactions between pyroclastic density currents : insights from analog experiments [PDF]
During some explosive volcanic eruptions, multiple pyroclastic density currents have been produced within a short time span of each other and flowed through the same area.
O'Donnell, Sean Bryan
core +1 more source
Investigation of variable aeration of monodisperse mixtures: implications for pyroclastic density currents [PDF]
The high mobility of dense pyroclastic density currents (PDCs) is commonly attributed to high gas pore pressures. However, the influence of spatial and temporal variations in pore pressure within PDCs has yet to be investigated. Theory suggests that variability in the fluidisation and aeration of a current will have a significant control on PDC flow ...
Rowley, Pete +3 more
openaire +4 more sources

