Combining active and passive multi-channel analysis of surface waves to improve reliability of \hbox {V}_\mathrm{S,30} estimation using standard equipment     

Francisco Humire  Esteban Sáez  Felipe Leyton  Gonzalo Yañez 《Bulletin of Earthquake Engineering》2015,13(5):1303-1321

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Parametric model for capacity curves     

Luis G. Pujades  Yeudy F. Vargas-Alzate  Alex H. Barbat  José R. González-Drigo 《Bulletin of Earthquake Engineering》2015,13(5):1347-1376

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Quantifying Water Pollution Sources in a Small Tile‐drained Agricultural Watershed          下载免费PDF全文

Petr Fučík  Tomáš Hejduk  Jana Peterková 《洁净——土壤、空气、水》2015,43(5):698-709

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Contribution of Methane Benthic and Atmospheric Fluxes of an Experimental Area (Sitka Stream)          下载免费PDF全文

Adam Bednařík  Lubomír Čáp  Vítězslav Maier  Martin Rulík 《洁净——土壤、空气、水》2015,43(8):1136-1142

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The Varre-Sai chondrite,a Brazilian fall: petrology and geochemistry     

Caio Vinícius Gabrig Turbay Rangel  Marcos Tadeu D’Azeredo Orlando  Cláudio De Morisson Valeriano  Alexandre de Oliveira Chaves 《International Geology Review》2017,59(15):1966-1973

The Varre-Sai meteorite fell along the border of the states of Espirito Santo and Rio de Janeiro, Brazil; on 19 June 2010 at 5:40 pm. Petrography and X-ray powder diffraction (XRD) indicate that the rock is an L5 S4 chondrite, with blastoporphyritic texture that has not been previously described. Geochemical data based on major and rare-earth elements (REEs) show that Varre-Sai is highly similar to the other L chondrites. In Harker diagrams, Varre-Sai, L, and LL chondrites form a single group, suggesting no significant chemical differences between them and contributing to the long-standing debate of whether LL chondrites form a distinct group or whether they are a subset of the L group. Harker diagrams also define a trend from E to H and L/LL chondrites, similar to the cosmochemical trends suggested by other authors. The behaviour of Fe₂O_3t and NiO indicates a relationship with Fe-Ni alloys, and their trend in the diagram suggests some chemical differentiation in the ordinary chondrite parental bodies. The REE content in Varre-Sai, normalized to C chondrites, falls in the field of L chondrites and others, but with slight REE enrichment. The chemical differences in chondrites, mainly in REEs, Fe₂O_3t and NiO could be alternatively interpreted as variations in the inherited agglutinated materials as chondrules, Ca–Al-rich inclusions and Fe–Ni nodules.  相似文献   

Flood risk assessment in a coastal lagoon under present and future scenarios: Ria de Aveiro case study     

Carina L. Lopes  Fátima L. Alves  João M. Dias 《Natural Hazards》2017,86(3):1307-1332

Iranian strong motion records as well as detailed conditions of their instrument sites and the characteristics of their causative seismic sources are compiled and processed. The dataset consists of 2286 three-component records from 461 Iranian earthquakes with at least two high-quality records having moment magnitude from 3.9 to 7.3. These records are about 20% of the Iranian database and are suitable for seismic hazard analysis and engineering applications. Perhaps for the first time in the literature, the distance to the surface projection of the fault is reported for a great number of records corresponding to earthquakes with M > 6.0. The raw accelerations are processed using the wavelet de-noising method. Having corrected and filtered these raw data, the pseudospectral accelerations are calculated for each of the three components of time series, separately. In addition to the ground motion parameters, a large and comprehensive list of metadata characterizing the recording conditions of each record is also developed. Moreover, careful revision of the characteristics of the earthquakes such as location, magnitude, style of faulting and fault rupture plane geometry, if available, is carried out using the best available information in a scientifically sound manner. Finally, we also focus on special ground motion records including records with peak ground acceleration (PGA) >300 cm/s² and distances less than 30 km. These are “exceptional” records in the Iranian dataset and include less than 2% of the selected dataset.  相似文献   

Numerical simulation of the 30–45 ka debris avalanche flow of Montagne Pelée volcano,Martinique: from volcano flank collapse to submarine emplacement     

Brunet  Morgane  Moretti  Laurent  Le Friant  Anne  Mangeney  Anne  Fernández Nieto  Enrique Domingo  Bouchut  Francois 《Natural Hazards》2017,85(2):1189-1208

Natural Hazards - In November 2015, China government announced that the national carbon emissions trading market is expected to start in 2017. Carbon emission trading system is a raising concern...  相似文献   

Evolution of borate minerals from contact metamorphic to hydrothermal stages: Ludwigite-group minerals and szaibélyite from the Vysoká – Zlatno skarn,Slovakia     

Bilohuščin  Vladimír  Uher  Pavel  Koděra  Peter  Milovská  Stanislava  Mikuš  Tomáš  Bačík  Peter 《Mineralogy and Petrology》2017,111(4):643-658

Mineralogy and Petrology - Borate minerals of the ludwigite group (LGM) and szaibélyite in association with hydroxylclinohumite, clinochlore, a serpentine mineral, magnesian magnetite, spinel,...  相似文献   

Platiniferous gold–tourmaline aggregates in the gold–palladium belt of Minas Gerais,Brazil: implications for regional boron metasomatism     

Cabral  Alexandre Raphael  Tupinambá  Miguel  Zeh  Armin  Lehmann  Bernd  Wiedenbeck  Michael  Brauns  Michael  Kwitko-Ribeiro  Rogerio 《Mineralogy and Petrology》2017,111(6):807-819

Mineralogy and Petrology - The platiniferous gold–palladium belt of Minas Gerais, Brazil, forms an approximately 240-km-long, roughly north–south-trending domain that includes numerous...  相似文献   

Using very long-range terrestrial laser scanner to analyze the temporal consistency of the snowpack distribution in a high mountain environment     

Juan I. López-Moreno  Jesús Revuelto  E. Alonso-González  Alba Sanmiguel-Vallelado  Steven R. Fassnacht  Jeffrey Deems  Enrique Morán-Tejeda 《山地科学学报》2017,14(5):823-842

This study demonstrated the usefulness of very long-range terrestrial laser scanning (TLS) for analysis of the spatial distribution of a snowpack, to distances up to 3000 m, one of the longest measurement range reported to date. Snow depth data were collected using a terrestrial laser scanner during 11 periods of snow accumulation and melting, over three snow seasons on a Pyrenean hillslope characterized by a large elevational gradient, steep slopes, and avalanche occurrence. The maximum and mean absolute snow depth error found was 0.5-0.6 and 0.2-0.3 m respectively, which may result problematic for areas with a shallow snowpack, but it is sufficiently accurate to determine snow distribution patterns in areas characterized by a thick snowpack. The results indicated that in most cases there was temporal consistency in the spatial distribution of the snowpack, even in different years. The spatial patterns were particularly similar amongst the surveys conducted during the period dominated by snow accumulation (generally until end of April), or amongst those conducted during the period dominated by melting processes (generally after mid of April or early May). Simple linear correlation analyses for the 11 survey dates, and the application of Random Forests analysis to two days representative of snow accumulation and melting periods indicated the importance of topography to the snow distribution. The results also highlight that elevation and the Topographic Position index (TPI) were the main variables explaining the snow distribution, especially during periods dominated by melting. The intra- and inter-annual spatial consistency of the snowpack distribution suggests that the geomorphological processes linked to presence/absence of snow cover act in a similar way in the long term, and that these spatial patterns can be easily identified through several years of adequate monitoring.  相似文献