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Identification of tsunami deposits and liquefaction features in the Gargano area (Italy):paleoseismological implication
tsunami liquefaction Gargano 1627 earthquake
2015/9/16
The Gargano region (Southeastern Italy) was hit by a M = 6.8 earthquake and inundated by a subsequent tsunami in 1627. To better define the hazard in the region, we searched for evidence of this and p...
Surface roughness of pyroclastic deposits at Mt. Etna by 3D laser scanning
surface roughness pyroclastic deposits Laser 3D
2015/9/1
The terrestrial 3D Laser Scanning technique has been applied to analyse the surface roughness of pyroclastic deposits on volcanic surfaces at Mt. Etna. This technique allowed the construction of high ...
Paleomagnetic dating of tectonically influenced Plio-Quaternary fan-system deposits from the Apennines (Italy)
Quaternary breccias Central Italy Paleomagnetism
2015/8/14
The Roveto Valley is a narrow, elongated, NW-trending depression filled with continental Plio-Quaternary deposits that outcrop at different topographic elevations. A morpho-lithostratigraphic successi...
New insights on the occurrence of peperites and sedimentary deposits within the silicic volcanic sequences of the Paraná Magmatic Province, Brazil
peperites and sedimentary deposits silicic volcanic sequences the Parana Magmatic Province Brazil
2015/1/6
The PMP (Paraná Magmatic Province) is characterized by lava flows of the Early Cretaceous Serra Geral Formation which covers about 75% of the Paraná Basin (southern and southeastern Brazil), composed ...
Lithospheric-scale structures in New Guinea and their control on the location of gold and copper deposits
Lithospheric-scale structures New Guinea location of gold copper deposits
2015/1/6
The locations of major gold and copper deposits on the island of New Guinea are considered by many to be controlled by a series of transfer faults that strike N–S to NE–SW, perpendicular to the long a...
Crustal 3-D geometry of the Kristineberg area (Sweden) with implications on VMS deposits
Kristineberg area Crustal 3-D geometry
2015/1/5
Structural analysis of the Palaeoproterozoic volcanogenic massive sulfide (VMS) hosting Kristineberg area, Sweden, constrained by existing magnetotelluric (MT) and seismic reflection dat...
Krakatau caldera deposits: revisited and verification by geophysical means
Krakatau caldera Parasitic cones Caldera deposit Drillings at calderas S-wave attenuation Vp/Vs ratio
2015/8/18
One of the differences between volcanic craters and calderas is that the latter bottoms are flatways filled with caldera deposit with lower density in comparison to country rocks. The 1883 Krakatau er...
A simple semi-empirical approach to model thickness of ash-deposits for different eruption scenarios
semi-empirical approach model thickness ash-deposits different eruption scenarios
2011/1/19
The impact of ash-fall on people, buildings, crops, water resources, and infrastructure depends on several factors such as the thickness of the deposits, grain size distribution and others. Preparedne...
Comment on Diamond Genesis,Ore Deposits and Ring Structures
Comment Diamond Genesis Ore Deposits Ring Structures
2009/6/15
Comment on Diamond Genesis,Ore Deposits and Ring Structures.
SURGING VERSUS CONTINUOUS TURBIDITY CURRENTS: FLOW DYNAMICS AND DEPOSITS IN AN EXPERIMENTAL INTRASLOPE MINIBASIN
SURGING VERSUS CONTINUOUS TURBIDITY CURRENTS FLOW DYNAMICS DEPOSITS EXPERIMENTAL INTRASLOPE MINIBASIN
2014/4/8
Small intraslope basins (; 100 km2), or ‘‘minibasins,’’such as those found on the continental slope of the Gulf of Mexico,have been filled predominantly by turbidity currents. Each minibasin is the re...