全文获取类型
收费全文 | 1542篇 |
免费 | 90篇 |
国内免费 | 61篇 |
专业分类
测绘学 | 927篇 |
大气科学 | 44篇 |
地球物理 | 218篇 |
地质学 | 114篇 |
海洋学 | 62篇 |
天文学 | 3篇 |
综合类 | 166篇 |
自然地理 | 159篇 |
出版年
2024年 | 4篇 |
2023年 | 7篇 |
2022年 | 52篇 |
2021年 | 99篇 |
2020年 | 105篇 |
2019年 | 87篇 |
2018年 | 65篇 |
2017年 | 136篇 |
2016年 | 137篇 |
2015年 | 138篇 |
2014年 | 129篇 |
2013年 | 138篇 |
2012年 | 87篇 |
2011年 | 98篇 |
2010年 | 59篇 |
2009年 | 62篇 |
2008年 | 49篇 |
2007年 | 48篇 |
2006年 | 51篇 |
2005年 | 31篇 |
2004年 | 26篇 |
2003年 | 25篇 |
2002年 | 16篇 |
2001年 | 12篇 |
2000年 | 10篇 |
1999年 | 4篇 |
1998年 | 1篇 |
1997年 | 3篇 |
1996年 | 1篇 |
1995年 | 1篇 |
1994年 | 2篇 |
1993年 | 3篇 |
1992年 | 2篇 |
1991年 | 1篇 |
1990年 | 3篇 |
1979年 | 1篇 |
排序方式: 共有1693条查询结果,搜索用时 31 毫秒
251.
激光雷达(LiDAR):获取高精度古地震探槽信息的一种新技术 总被引:8,自引:4,他引:4
激光雷达技术是近几十年新发展起来的一种测量技术,已被广泛应用于工程测量、文物保护及地形测量等方面,近几年来活动构造的研究中也已逐步引入。作为活动构造研究的最基础的古地震研究一直还采用传统的地质素描技术进行探槽信息获取,数码照相技术的引入虽然解决了一些问题,但由于照相技术本身的限制,很难克服获取信息的变形和扭曲。激光雷达扫描系统的高信息量、高精度、便捷、安全和易操作等性能,为古地震研究开辟了获取数据信息的新手段和新技术。 相似文献
252.
253.
Granitic coastal geomorphology: applying integrated terrestrial and bathymetric LiDAR with multibeam sonar to examine coastal landscape evolution 下载免费PDF全文
Coasts composed of resistant lithologies such as granite are generally highly resistant to erosion. They tend to evolve over multiple sea level cycles with highstands acting to remove subaerially weathered material. This often results in a landscape dominated by plunging cliffs with shore platforms rarely occurring. The long‐term evolution of these landforms means that throughout the Quaternary these coasts have been variably exposed to different sea level elevations which means erosion may have been concentrated at different elevations from today. Investigations of the submarine landscape of granitic coasts have however been hindered by an inability to accurately image the nearshore morphology. Only with the advent of multibeam sonar and aerial laser surveying can topographic data now be seamlessly collected from above and below sea level. This study tests the utility of these techniques and finds that very accurate measurements can be made of the nearshore thereby allowing researchers to study the submarine profile with the same accuracy as the subaerial profile. From a combination of terrestrial and marine LiDAR data with multibeam sonar data, it is found that the morphology of granite domes is virtually unaffected by erosion at sea level. It appears that evolution of these landscapes on the coast is a very slow process with modern sea level acting only to remove subaerially weathered debris. The size and orientation of the joints determines the erosional potential of the granite. Where joints are densely spaced (<2 m apart) or the bedrock is highly weathered can semi‐horizontal surfaces form. Copyright © 2014 John Wiley & Sons, Ltd. 相似文献
254.
The town of Zafferana Etnea, located on the southeastern slope of Mt. Etna volcano (Italy), has been repeatedly threatened
by lava flows in recent centuries. The last serious threat occurred during the 1991–1993 eruption, when the lava front came
to a halt only 1.7 km from the centre of town. Morphostructural data derived from light detection and ranging (LiDAR) surveys
carried out on Etna in 2005 have enabled us to evaluate the risk of lava invasion in a section (16 km2) of the Zafferana Etnea territory. Qualitative and quantitative results are obtained combining the information derived from
LiDAR analysis with geological, morphological and structural data using geographic information systems technology (GIS). The
study quantifies in unprecedented detail the areal extent and volume of forested and urban areas and its degree of exposure
to different levels of hazard from future lava invasion. Nearly 52% of the urban texture fall into areas of moderate to high
risk from lava invasion. Future land use planning should take these findings into account and promote new development preferentially
in areas of lower risk. 相似文献
255.
Abstract: Landslide research at the British Geological Survey (BGS) is carried out through a number of activities, including surveying, database development and real-time monitoring of landslides. Landslide mapping across the UK has been carried out since BGS started geological mapping in 1835. Today, BGS geologists use a combination of remote sensing and ground-based investigations to survey landslides. The development of waterproof tablet computers (BGS·SIGMAmobile), with inbuilt GPS and GIS for field data capture provides an accurate and rapid mapping methodology for field surveys. Regional and national mapping of landslides is carried out in conjunction with site-specific monitoring, using terrestrial LiDAR and differential GPS technologies, which BGS has successfully developed for this application. In addition to surface monitoring, BGS is currently developing geophysical ground-imaging systems for landslide monitoring, which provide real-time information on subsurface changes prior to failure events. BGS’s mapping and monitoring activities directly feed into the BGS National Landslide Database, the most extensive source of information on landslides in Great Britain. It currently holds over 14?000 records of landslide events. By combining BGS’s corporate datasets with expert knowledge, BGS has developed a landslide hazard assessment tool, GeoSure, which provides information on the relative landslide hazard susceptibility at national scale. 相似文献
256.
257.
移动通讯数字地图系统的数据采集及质量控制 总被引:1,自引:0,他引:1
对黑龙江移动通讯数字地图系统的数据结构进行了分析,叙述了各类数据的采集流程及其质量控制,可为通讯部门的数据采集提供参考。 相似文献
258.
Remote measurement of river morphology via fusion of LiDAR topography and spectrally based bathymetry 总被引:1,自引:0,他引:1
Carl J. Legleiter 《地球表面变化过程与地形》2012,37(5):499-518
This study developed and evaluated a hybrid approach to remote measurement of river morphology that combines LiDAR topography with spectrally based bathymetry. Comparison of filtered LiDAR point clouds with surveyed cross‐sections indicated that subtle features on low‐relief floodplains were accurately resolved by LiDAR but that submerged areas could not be detected due to strong absorption of near‐infrared laser pulses by water. The reduced number of returns made the active channel evident in a LiDAR point density map. A second dataset suggested that pulse intensity also could be used to discriminate land from water via a threshold‐based masking procedure. Fusion of LiDAR and optical data required accurate co‐registration of images to the LiDAR, and we developed an object‐oriented procedure for achieving this alignment. Information on flow depths was derived by correlating pixel values with field measurements of depth. Highly turbid conditions dictated a positive relation between green band radiance and flow depth and contributed to under‐prediction of pool depths. Water surface elevations extracted from the LiDAR along the water's edge were used to produce a continuous water surface that preserved along‐channel variations in slope. Subtracting local flow depths from this surface yielded estimates of the bed elevation that were then combined with LiDAR topography for exposed areas to create a composite representation of the riverine terrain. The accuracy of this terrain model was assessed via comparison with detailed field surveys. A map of elevation residuals showed that the greatest errors were associated with underestimation of pool depths and failure to capture cross‐stream differences in water surface elevation. Nevertheless, fusion of LiDAR and passive optical image data provided an efficient means of characterizing river morphology that would not have been possible if either dataset had been used in isolation. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
259.
LiDAR data were used to quantify and analyse a rockfall event which occurred in 2003 in the Western Dolomites (Italian Alps). In addition to previously existing airborne laserscanning (ALS) data, high resolution terrestrial laserscanning (TLS) data were collected. By using the original point clouds, the volume, axial ratio and runout length of single boulders as well as the surface roughness in the runout zone of the rockfall were derived. The total volume of the rockfall event of approximately 10 000 m³ was estimated by a reconstruction of the pre‐event surface at the detachment zone. The analysis of the laser scanning data of the accumulation zone revealed a power law scaling for boulder volumes larger than 8 m³. The dependence of runout length on boulder volume is complex; it is moderated by particle sphericity. In addition, we used ALS and TLS data to derive the spatial distribution of surface roughness on the talus cone. TLS allow for more accurate roughness mapping than ALS data, but for most applications the point density of ALS data seems to be sufficiently high to derive measures of roughness. Different sampling approaches for plane fitting on the scale of 5 m did not show significant effects besides the computational time. The results of our analyses provide important perspectives for rockfall modelling and process understanding with potential applications in both ‘applied’ (natural hazards) and ‘pure’ geomorphological research. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
260.