全文获取类型
收费全文 | 56篇 |
免费 | 4篇 |
国内免费 | 4篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 3篇 |
地球物理 | 13篇 |
地质学 | 23篇 |
天文学 | 24篇 |
出版年
2023年 | 1篇 |
2022年 | 1篇 |
2021年 | 1篇 |
2020年 | 5篇 |
2019年 | 4篇 |
2018年 | 4篇 |
2017年 | 1篇 |
2016年 | 3篇 |
2015年 | 2篇 |
2014年 | 3篇 |
2013年 | 5篇 |
2012年 | 4篇 |
2011年 | 2篇 |
2010年 | 1篇 |
2009年 | 6篇 |
2008年 | 1篇 |
2007年 | 2篇 |
2006年 | 3篇 |
2005年 | 1篇 |
2004年 | 3篇 |
2003年 | 3篇 |
2002年 | 2篇 |
2001年 | 1篇 |
2000年 | 2篇 |
1998年 | 2篇 |
1973年 | 1篇 |
排序方式: 共有64条查询结果,搜索用时 109 毫秒
41.
42.
Cristiano Collettini Massimiliano Barchi Cristina Pauselli Costanzo Federico Giampaolo Pialli 《Journal of Geodynamics》2000,29(3-5)
This paper deals with the geometry and kinematics of the active normal faults in northern Umbria, and their relationship with the seismicity observed in the area. In particular, we illustrate the contribution of seismic reflection data (a network of seismic profiles, NNW–SSE and WSW–ENE trending) in constraining at depth the geometry of the different active fault systems and their reciprocal spatial relationships. The main normal fault in the area is the Alto Tiberina fault, NNW trending and ENE dipping, producing a displacement of about 5 km, and generating a continental basin (Val Tiberina basin), infilled by up to 1500 m with Upper Pliocene–Quaternary deposits. The fault has a staircase trajectory, and can be traced on the seismic profiles to a depth of about 13 km. A set of WSW-dipping, antithetic faults can be recognised on the profiles, the most important of which is the Gubbio fault, bordering an extensional Quaternary basin and interpreted as an active fault based on geological, geomorphologic and seismological evidence. The epicentral distribution of the main historical earthquakes is strictly parallel to the general trend of the normal faults. The focal mechanisms of the major earthquakes show a strong similarity with the attitude of the extensional faults, mapped at the surface and recognised on the seismic profiles. These observations demonstrate the connection between seismicity in the area and the activity of the normal faults. Moreover, the distribution of the instrumental seismicity suggests the activity of the Alto Tiberina fault as the basal detachment for the extensional tectonics of the area. Finally, the action of the Alto Tiberina fault was simulated using two dimensional finite element modelling: a close correspondence between the concentration of shear stresses in the model and the distribution of the present earthquakes was obtained. 相似文献
43.
de Medeiros Felipe Jeferson de Oliveira Cristiano Prestrelo Santos e Silva Cludio Moiss de Arajo Joo Medeiros 《Climate Dynamics》2020,54(9):4043-4057
Climate Dynamics - Large domains in regional climate models are known to provide a better representation of the mesoscale circulation and hence the precipitation field. To evaluate the model... 相似文献
44.
Cristiano Nicosia Roger Langohr Florias Mees Antonia Arnoldus‐Huyzendveld Jacopo Bruttini Federico Cantini 《Geoarchaeology》2012,27(2):105-122
Archaeological excavations at the Biblioteca Magliabechiana, which is part of the Uffizi gallery complex in Florence (Tuscany, central Italy), exposed Dark Earth deposits between alluvial sediments of the nearby Arno River. The term Dark Earth refers to thick, dark colored, and seemingly homogeneous deposits occurring in urban settings throughout Europe, broadly dated to the post‐Roman period. The stratigraphic sequence of the Biblioteca Magliabechiana was investigated by integrating geomorphological, chronological, and archaeological information with micromorphological and soil analytical data. This combination of approaches resulted in the identification of an early phase of Dark Earth formation (7th century A.D.) during which the area was characterized by the accumulation of manure or night soil in wet peri‐fluvial conditions. After a phase of abandonment, Dark Earth accretion resumed (10th to early 11th century A.D.), at this stage due primarily to the dumping of domestic waste. Subsequent progressive abandonment of the area was followed by the deposition of alluvium, probably during the major flood of November 4, 1177. The present study demonstrates that Dark Earth is the outcome of strong bioturbation and human reworking acting on anthropogenic deposits and possibly on alluvial sediments. 相似文献
45.
Caio A. S. Coelho Cristiano Prestrelo de Oliveira Tércio Ambrizzi Michelle Simões Reboita Camila Bertoletti Carpenedo José Leandro Pereira Silveira Campos Ana Carolina Nóbile Tomaziello Luana Albertani Pampuch Maria de Souza Custódio Lívia Marcia Mosso Dutra Rosmeri P. Da Rocha Amanda Rehbein 《Climate Dynamics》2016,46(11-12):3737-3752
46.
Davi C. D. Melo Jamil A. A. Anache Cristiano das N. Almeida Jaqueline V. Coutinho Geraldo M. Ramos Filho Lívia M. P. Rosalem 《水文科学杂志》2020,65(8):1262-1280
ABSTRACT
In-situ
hydrological monitoring is essential for a proper decision-making process and modelling. Efforts have been made in Brazil to carry out field activities at the basin scale, but how complete and comprehensive are those studies? Where are they located? How long have they been carried out? What are the main findings? To answer these questions, an overview of experimental monitoring basins in Brazil is presented, listing their geographical locations, monitored variables, operational status, monitoring periods and main publications. We identified 60 monitored sites, spread across most Brazilian biomes, with an average monitoring period of 12 years. However, some publications from these monitoring studies are not fully accessible to the international community. Field hydrology activities in Brazil contribute to a better understanding of hydrological processes in humid and semi-arid regions and inform us about the impacts of land-use change on water quality and quantity. 相似文献47.
Francisco António Pereira Neto George Sand França Cristobal Condori Giuliano Sant’Anna Marotta Cristiano Naibert Chimpliganond 《Journal of Seismology》2018,22(5):1113-1126
This work describes the development of the Angolan earthquake catalog and seismicity distribution in the Southwestern African Plate, in Angola. This region is one of the least seismically active, even for stable continental regions (SCRs) in the world. The maximum known earthquake had a magnitude of 6.0 Ms, while events with magnitudes of 4.5 have return period of about 10 years. Events with magnitude 5 and above occur with return period of about 20 years. Five seismic zones can be confirmed in Angola, within and along craton edges and in the sedimentary basins including offshore. Overall, the exposed cratonic regions tend to have more earthquakes compared to other regions such as sedimentary basins. Earthquakes tend to occur in Archaic rocks, especially inside preexisting weakness zones and in tectonic-magmatic reactivation zones of Mesozoic and Meso-Cenozoic, associated with the installation of a wide variety of intrusive rocks, strongly marked by intense tectonism. This fact can be explained by the models of preexisting weakness zones and stress concentration near intersecting structures. The Angolan passive margin is also a new region where seismic activity occurs. Although clear differences are found between different areas along the passive margin, in the middle near Porto Amboim city, seismic activity is more frequent compared with northwestern and southwestern regions. 相似文献
48.
Léo A. Hartmann Mariana Werle Cassiana R.L. Michelin Cristiano Lana Gláucia N. Queiroga Marco P. Castro Karine R. Arena 《地学前缘(英文版)》2019,10(4):1623-1633
Proto-Adamastor ocean bathed Rodinia and successor continental fragments from 1.0–0.9 Ga up to 0.75 Ga, and evolved into world Adamastor Ocean at 0.75–0.60 Ga. Mesoproterozoic oceanic crust is poorly preserved on continents, only indirect evidence registered in Brasiliano Orogen. We report first evidence of ophiolite originated in proto-Adamastor. We use multi-technique U-Pb-Hf zircon and δ11B tourmaline isotopic and elemental compositions. The host tourmalinite is enclosed in metaserpentinite, both belonging to the Bossoroca ophiolite. Zircon is 920 Ma-old, ?Hf(920 Ma) = +12, HfTDM = 1.0 Ga and has ‘oceanic’ composition (e.g., U/Yb < 0.1). Tourmaline is dravite with δ11B = +1.8‰ (Tur 1), 0‰ (Tur 2), ?8.5‰ (Tur 3). These characteristics are a novel contribution to Rodinia and associated world ocean, because a fragment of proto-Adamastor oceanic crust and mantle evolved at the beginning of the Brasiliano Orogen. 相似文献
49.
Federico Manzini Raoul Behrend Lorenzo Comolli Virginio Oldani Cristiano B. Cosmovici Roberto Crippa Cesare Guaita Gottfried Schwarz Josep Coloma 《Astrophysics and Space Science》2012,337(2):531-542
Extensive observations of comet C/2004 Q2 (Machholz) were carried out between August 2004 and May 2005. The images obtained
were used to investigate the comet’s inner coma features at resolutions between 350 and 1500 km/pixel. 相似文献
50.
Support Vector Machines for Landslide Susceptibility Mapping: The Staffora River Basin Case Study, Italy 总被引:4,自引:0,他引:4
The aim of this study is the application of support vector machines (SVM) to landslide susceptibility mapping. SVM are a set
of machine learning methods in which model capacity matches data complexity. The research is based on a conceptual framework
targeted to apply and test all the procedural steps for landslide susceptibility modeling from model selection, to investigation
of predictive variables, from empirical cross-validation of results, to analysis of predicted patterns. SVM were successfully
applied and the final susceptibility map was interpreted via success and prediction rate curves and receiver operating characteristic
(ROC) curves, to support the modeling results and assess the robustness of the model. SVM appeared to be very specific learners,
able to discriminate between the informative input and random noise. About 78% of occurrences was identified within the 20%
of the most susceptible study area for the cross-validation set. Then the final susceptibility map was compared with other
maps, addressed by different statistical approaches, commonly used in susceptibility mapping, such as logistic regression,
linear discriminant analysis, and naive Bayes classifier. The SVM procedure was found feasible and able to outperform other
techniques in terms of accuracy and generalization capacity. The over-performance of SVM against the other techniques was
around 18% for the cross-validation set, considering the 20% of the most susceptible area. Moreover, by analyzing receiver
operating characteristic (ROC) curves, SVM appeared to be less prone to false positives than the other models. The study was
applied in the Staffora river basin (Lombardy, Northern Italy), an area of about 275 km2 characterized by a very high density of landslides, mainly superficial slope failures triggered by intense rainfall events. 相似文献