Integrated Geophysical Investigations at the Greek Kamarina Site (Southern Sicily,Italy)     

Salvatore Scudero  Raffaele Martorana  Patrizia Capizzi  Antonino Pisciotta  Antonino D’Alessandro  Carla Bottari  Giovanni Di Stefano 《Surveys in Geophysics》2018,39(6):1181-1200

Kamarina, located in southern Sicily (Italy), was an important Greek colony since its foundation in the sixth century BC. Archaeological excavations, carried out since the twentieth century, uncovered only limited portions of the site so far. Despite the importance of the Greek colony, the presence of remarkable buildings that archaeologists expected to bring to light has not found fully correspondence in the archaeological excavations. Consequently, the integrated geophysical prospection carried out in the study area is aimed to support and address the future archaeological investigations. After the photographic and thermographic survey obtained by an unmanned aerial vehicle, we performed a systematic survey through ground magnetic and GPR methods over an area of 6200 m². The acquisition procedures have been optimized in order to get the best results combining high resolution and elevated speed of acquisition. The results derived from the three geophysical techniques have been conveniently combined by means of a cluster analysis, allowing us to clearly identify a series of buried archaeological features. Because of their geometrical characteristics, often in good agreement with the spatial arrangement of the archaeological remains at the surface, these buried archaeological features can be interpreted as roads, walls, or buildings foundations in which the various construction phases of the city can be clearly recognized. The integrated approach has proven to be essential for a robust interpretation of the archaeogeophysical investigation.  相似文献   

Decoupled kinematics of two neighbouring permafrost creeping landforms in the Eastern Italian Alps     

Roberto Seppi  Luca Carturan  Alberto Carton  Thomas Zanoner  Matteo Zumiani  Federico Cazorzi  Aldo Bertone  Carlo Baroni  Maria Cristina Salvatore 《地球表面变化过程与地形》2019,44(13):2703-2719

An overall acceleration of rock glacier displacement rates in the Alps has been observed in recent decades, with several cases of destabilization leading to potential geomorphological hazards. This behaviour has been attributed to the rising permafrost temperature, induced by atmospheric warming and regulated by thermo-hydrological processes. Landforms derived from the interaction of glacier remnants and permafrost are widespread in mountain areas, but are less studied and monitored than talus rock glaciers. This work presents a comparative study of a talus rock glacier and a glacial-permafrost composite landform (GPCL) in the Eastern Italian Alps. The two landforms are only 10 km apart, but have rather different elevation ranges and main slope aspects. The kinematics and ground thermal conditions were monitored from 2001 to 2015 along with geomorphological surveys, analyses of historical maps and remote sensing data. The dynamic behaviour of the rock glacier was similar to the majority of monitored rock glaciers in the Alps, with an acceleration after 2008 and a velocity peak in 2015. In contrast, the GPCL had a nearly unchanged displacement rate during the observation period. Statistical analyses of kinematic vs. nivo-meteorological variables revealed a dynamic decoupling of the two landforms after 2008 that corresponds with increased winter snow accumulation. Although the kinematics of both landforms respond to ground surface temperature variations, the collected evidence suggests a different reaction of ground surface temperature to variations in the precipitation regime. This different reaction is likely due to local topo-climatic conditions that affect snow redistribution by wind. The different reactions of the two systems to the same climatic forcing is likely a legacy of their different origins. GPCL dynamics result from interaction of permafrost and residual glacial dynamics that are associated with possible peculiarities in the internal/basal meltwater circulation, whose future response is uncertain and requires improved understanding. © 2019 John Wiley & Sons, Ltd. © 2019 John Wiley & Sons, Ltd.  相似文献   

Evolution of landscapes on the double mountain fork of the brazos river,West Texas: Implications for preservation and visibility of the archaeological record     

Michael D. Blum  James T. Abbott  Salvatore Valastro 《Geoarchaeology》1992,7(4):339-370

The Double Mountain Fork of the Brazos River is an ephemeral stream that flows across the western Rolling Plains of West Texas. Intensive pedestrian archaeological survey, covering some 8700 acres of the drainage, produced a site inventory with a general paucity of identifiable Paleoindian and Early to Middle Archaic components, whereas Late Archaic and Late Prehistoric sites were widespread and found in a diversity of landscape positions. Geoarchaeological investigations were conducted in conjunction with this survey and later testing activities, and suggested that much of this temporally and spatially skewed archaeological record may be attributable to the evolution of landscapes during the late Pleistocene and Holocene time period, rather than original occupation intensities. Most of the landscape in the study area has been subject to erosional stripping, but in selected localities late Pleistocene and Holocene depositional landform-sediment assemblages of fluvial, alluvial/colluvial fan, and eolian origin are preserved. With few exceptions, however, depositional contexts or stable geomorphic surfaces more than 3000 years old are erosionally truncated, completely absent, or deeply buried. As a result, a bias is imposed that renders older cultural records either poorly preserved or deeply buried and of low visibility to traditional survey techniques. Similar natural formation processes are likely at other locations on the western Rolling Plains, and should be considered during interpretation of prehistoric population dynamics in the area. The biases imposed by such natural formation processes on the western Rolling Plains are slightly different from other areas in the Southern Great Plains of the United States, but in most cases the known archaeological record corresponds with opportunities for preservation and visibility provided by geologic trajectories, and may reflect little on spatial and temporal discontinuities in prehistoric cultural activity.  相似文献   

On a unique behavior of freshwater bacteria   总被引：1，自引：1，他引：0  

Salvatore BELLINI 《中国海洋湖沼学报》2009,27(1):3-5

Magnetic sensitivity has been found in bacteria from freshwater sites around Pavia, Italy.  相似文献   

Distribution and spatial structure of pelagic fish schools in relation to the nature of the seabed in the Sicily Straits (Central Mediterranean)     

Marta D'Elia  Bernardo Patti  Attilio Sulli  Giorgio Tranchida  Angelo Bonanno  Gualtiero Basilone  Giovanni Giacalone  Ignazio Fontana  Simona Genovese  Cástor Guisande  & Salvatore Mazzola 《Marine Ecology》2009,30(S1):151-160

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Validation of macroscopic maturity stages according to microscopic histological examination for European anchovy   总被引：1，自引：0，他引：1  

Rosalia Ferreri  Gualtiero Basilone  Marta D'Elia  Anna Traina  Francisco Saborido-Rey  & Salvatore Mazzola 《Marine Ecology》2009,30(S1):181-187

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Ballistic representation for kinematic access     

Salvatore Alfano 《Celestial Mechanics and Dynamical Astronomy》2011,109(1):45-58

This work uses simple two-body orbital dynamics to initially determine the kinematic access for a ballistic vehicle. Primarily this analysis was developed to assess when a rocket body might conjunct with an orbiting satellite platform. A family of access opportunities can be represented as a volume for a specific rocket relative to its launch platform. Alternately, the opportunities can be represented as a geographical footprint relative to aircraft or satellite position that encompasses all possible launcher locations for a specific rocket. A thrusting rocket is treated as a ballistic vehicle that receives all its energy at launch and follows a coasting trajectory. To do so, the rocket’s burnout energy is used to find its equivalent initial velocity for a given launcher’s altitude. Three kinematic access solutions are then found that account for spherical Earth rotation. One solution finds the maximum range for an ascent-only trajectory while another solution accommodates a descending trajectory. In addition, the ascent engagement for the descending trajectory is used to depict a rapid access scenario. These preliminary solutions are formulated to address ground-, sea-, or air-launched vehicles.  相似文献   

Modelling the long‐term deformation of the sedimentary substrate of Mt. Etna volcano (Italy)          下载免费PDF全文

Salvatore Scudero  Giorgio De Guidi  Sebastiano Imposa  Gilda Currenti 《地学学报》2015,27(5):338-345

This study investigates in detail the deformation events that have affected the sedimentary successions forming the substrate of Mt. Etna volcano (Italy). Based on the geometric reconstruction of a buried sedimentary marker, we have been able to identify and quantify the effects of three different mechanisms of deformation that have affected the area in the last 600 ka. Numerical results from Finite Element Method (FEM) applied to model viscoelastic deformation suggest the occurrence of a crustal doming process originating at the mantle‐crust transition (~16 km). We propose that the source of deformation is related to the diapiric uprise of hydrothermal material originating in altered ocean‐like crust and its emplacement at a shallower level in the crust. This process has great relevance in the volcanic system and should be considered for the full assessment of its origin and evolution.  相似文献   

Atmospheric Background Measurement in the 300–400 nm Band with a Balloon Borne Experiment During a Nocturnal Flight     

Giovanni La Rosa  Gaetano Agnetta  Benedetto Biondo  Osvaldo Catalano  Filippo Celi  Renato Di Raffaele  Salvatore Giarrusso  Angelo Mangano  Francesco Russo  John Linsley  Angelo Lo Bue 《Astrophysics and Space Science》2001,276(1):219-226

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Recent developments in hydrologic analysis     

Salvatore Grimaldi 《Advances in water resources》2007

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