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Terrinha Pedro Pueyo Emilio L. Aranguren Aitor Kullberg José Carlos Kullberg Maria Carla Casas-Sainz Antonio Azevedo Maria do Rosário 《International Journal of Earth Sciences》2018,107(5):1807-1833
International Journal of Earth Sciences - The geometry and emplacement of the ~ 96 km2, Late Cretaceous Sintra Igneous complex (SIC, ca. 80 Ma) into the West Iberian passive... 相似文献
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The prediction of rockfall trajectories below a rock cliff is essential in susceptibility, hazard and risk maps, particularity
close to populated areas. The Monte da Lua hill area in Portugal, a tourist destination close to the historic city of Sintra
(UNESCO World Heritage), is a typical granite boulder chaos landscape where from time to time rockfalls occur, the last such
event having occurred on 29 January 2002. This area is therefore suitable to develop a rockfall study in order to provide
hazard and risk maps a basis for mitigation measures. A preliminary investigation of the area leads to the identification
of 188 potentially dangerous boulders. Detailed locations and geotechnical characteristics in terms of geometry, strength
and context were sampled for each boulder. Digital elevations at 1 × 1 m resolution, known rockfall trajectory and building
locations are provided in a GIS project for the study together with the spatial database of boulder characteristics. The modelling
approach was conducted in two steps: (1) discrimination of the boulders in terms of static and dynamic mobility behaviour
with multivariate analysis; (2) stochastic simulation of rockfall trajectories. The rockfall trajectory algorithm proposed
is straightforward and is only dependent on elevation data, initial location of boulders and a friction angle. Due to the
slope of the area, it assumes that rockfall is always of the rolling or sliding type. The friction angle was calibrated on
the basis of the rockfall travel distance recorded on 29 January 2002 and generates simulated “realistic” trajectories. A
smaller friction angle increases all simulated trajectories, leading to more “pessimistic” scenarios. The combined analysis
of trajectories and potential damage to buildings and discrimination in terms of static and dynamic behaviour provides a final
table in which all 188 sampled boulders are classified in one of the five risk grades. 相似文献
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Triassic stretching directions in Iberia and North Africa inferred from magnetic fabrics 总被引:1,自引:0,他引:1
Ruth Soto Antonio M. Casas‐Sainz Beln Oliva‐Urcia Cristina García‐Lasanta Esther Izquierdo‐Llavall Bennacer Moussaid Jos Carlos Kullberg Teresa Romn‐Berdiel Yolanda Snchez‐Moya Alfonso Sopea Sara Torres‐Lpez Juan Jos Villalaín Hamidou El‐Ouardi Inmaculada Gil‐Pea Ann M. Hirt 《地学学报》2019,31(5):465-478
During the Triassic, Iberia and western North Africa displayed a unique situation in relation with the Central and North Atlantic opening and westward expansion of the Tethys. Unravelling the stretching direction in Triassic deposits of the studied area can help in our understanding of this scenario. The tectonic setting is characterized by localized basins with strong thickness variations greatly influenced by previous post‐Variscan mechanical discontinuities. In this work, we revise and compile magnetic fabric data from eight Triassic depocentres in terms of defining the stretching direction (i.e. magnetic lineation), resulting from extensional deformation of this period. Data show the importance of the opening of the Atlantic rift as the leading process during the Triassic. Dextral transtension can explain the deflection of the extensional direction observed in most studied depocentres that is caused by the activity of previous major oblique faults. 相似文献
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