全文获取类型
收费全文 | 768篇 |
免费 | 321篇 |
国内免费 | 59篇 |
专业分类
测绘学 | 117篇 |
大气科学 | 58篇 |
地球物理 | 594篇 |
地质学 | 243篇 |
海洋学 | 64篇 |
天文学 | 13篇 |
综合类 | 25篇 |
自然地理 | 34篇 |
出版年
2023年 | 4篇 |
2022年 | 16篇 |
2021年 | 23篇 |
2020年 | 39篇 |
2019年 | 43篇 |
2018年 | 28篇 |
2017年 | 37篇 |
2016年 | 37篇 |
2015年 | 50篇 |
2014年 | 52篇 |
2013年 | 56篇 |
2012年 | 46篇 |
2011年 | 46篇 |
2010年 | 34篇 |
2009年 | 46篇 |
2008年 | 62篇 |
2007年 | 41篇 |
2006年 | 53篇 |
2005年 | 59篇 |
2004年 | 34篇 |
2003年 | 28篇 |
2002年 | 37篇 |
2001年 | 36篇 |
2000年 | 23篇 |
1999年 | 36篇 |
1998年 | 27篇 |
1997年 | 18篇 |
1996年 | 23篇 |
1995年 | 18篇 |
1994年 | 18篇 |
1993年 | 15篇 |
1992年 | 12篇 |
1991年 | 8篇 |
1990年 | 3篇 |
1989年 | 13篇 |
1988年 | 10篇 |
1987年 | 2篇 |
1986年 | 1篇 |
1985年 | 2篇 |
1982年 | 1篇 |
1980年 | 3篇 |
1978年 | 3篇 |
1977年 | 2篇 |
1954年 | 3篇 |
排序方式: 共有1148条查询结果,搜索用时 109 毫秒
31.
《Comptes Rendus Geoscience》2015,347(1):13-23
We estimate using gravity data the thickness of post-glacial unconsolidated sediment filling two major glacial valleys in northern Pyrenees: the Gave de Pau valley between Pierrefitte-Nestalas and Lourdes, and the Garonne valley between Saint-Béat and Barbazan. One hundred and eighty-four new gravity data complete 74 measurements obtained from the International Gravimetric Bureau database. Negative residual anomalies resulting from the presence of small-density unconsolidated sediment approach 4 mgal in both the Gave de Pau and the Garonne valleys. Estimating the sediment thickness requires knowing the density contrast between Quaternary sediments and the underlying bedrock. Supposing this density contrast is 600 kg/m3, the maximum estimated thickness of post-glacial sediment is ∼ 230 and 300 meters, and the volume of sediment is 2.1 and 3.2 km3 in the Gave de Pau and Garonne valleys, respectively. In both valleys, the depth of Quaternary sediment suddenly increases at the confluence between two major glacial valleys (Gave de Pau – Gave de Cauterets, and Garonne – Pique confluences). Overdeepened basins are less deep downstream when approaching terminal moraines (Lourdes and Barbazan area), illustrating that the efficiency of glacial erosion depends on the ice flux flowing through valleys. 相似文献
32.
夏季青藏高原低涡的切向流场及波动特征分析 总被引:4,自引:0,他引:4
从大气动力学原理出发,将高原低涡视为受热源强迫的边界层内涡旋,建立了柱坐标下满足梯度风平衡的低涡控制方程组,分析高原低涡切向流场的基本特征.在此基础上,通过求解线性化涡旋模式,得出高原低涡中各类波动的频散关系及其特征,同时定性讨论了热力作用对混合波动的影响以及混合波动与高原低涡流场特征的联系.使用中尺度数值模式WRF分... 相似文献
33.
34.
Gary J. Barnes John M. Lumley Phill I. Houghton Richard J. Gleave 《Geophysical Prospecting》2011,59(1):176-187
Noise levels in marine and airborne full tensor gravity gradiometer surveys together with conventional land, marine and airborne gravity surveys are estimated and analysed in gridded form, resulting in relations that detail how these different survey systems can be compared analytically. After defining survey parameters including line spacing, speed and instrument bandwidth, the relations estimate the noise levels that result on either grids of gravity (gz) or gravity gradient (Gzz) as a function of the spatial filtering often applied during geological interpretation. Such comparisons are believed to be a useful preliminary guide for survey selection and planning. 相似文献
35.
给出了时变参数PGM(1,1)模型的数值解法,比较了其与GM(1,1)、PGM(1,1)模型的预测精度,分析了灰区间作为预测结果的可靠性。 相似文献
36.
The Orange Basin records the development of the Late Jurassic to present day volcanic-rifted passive margin of Namibia. Regional extension is recorded by a Late Jurassic to Lower Cretaceous Syn-rift Megasequence, which is separated from a Cretaceous to present day post-rift Megasequence by the Late Hauterivian (ca. 130 Ma) break-up unconformity. The Late Cretaceous Post-rift evolution of the basin is characterized by episodic gravitational collapse of the margin. Gravitational collapse is recorded as a series of shale-detached gravity slide systems, consisting of an up-dip extensional domain that is linked to a down-dip zone of contraction domain along a thin basal detachment of Turonian age. The extensional domain is characterized by basinward-dipping listric faults that sole into the basal detachment. The contractional domain consists of landward-dipping listric faults and strongly asymmetric basinward-verging thrust-related folds. Growth stratal patterns suggest that the gravitational collapse of the margin was short-lived, spanning from the Coniacian (ca. 90 Ma) to the Santonian (ca. 83 Ma). Structural restorations of the main gravity-driven system show a lack of balance between up-dip extension (24 km) and down-dip shortening (16 km). Gravity sliding in the Namibian margin is interpreted to have occurred as a series of episodic short-lived gravity sliding between the Cenomanian (ca. 100 Ma) and the Campanian (ca. 80 Ma). Gravity sliding and spreading are interpreted to be the result of episodic cratonic uplift combined with differential thermal subsidence. Sliding may have also been favoured by the presence of an efficient detachment layer in Turonian source rocks. 相似文献
37.
在我国大陆开展的流动重力重复观测是监测地震前兆异常的主要技术手段之一。 对大地震前流动重力场观测资料研究结果表明, 区域性持续的重力场增加和减少与大地震发生有显著关系。 目前, 区域重力场变化监测已经成为一种常规前兆观测技术手段。 本文首先从三维倾斜台阶模型入手, 计算了理论重力异常, 并对异常进行变换, 找到了一种可以更好刻画其场源边界的方法, 并进一步应用空间相关系数法进行异常特征分析, 得到了从概率意义上估计危险区的方法。 最后, 本文尝试运用此方法对青藏高原东缘地区1998—2005年的四期流动重力测网资料进行处理和分析。 应用本文提出的异常处理技术, 可有效地圈定异常梯级带位置, 确定质源体边界形态, 并可以联合背景重力异常场等其他资料, 给出危险区发震概率的空间估计, 分析结果在年度震情会商中可以有效地对地震危险区的划定提供技术支持。 相似文献
38.
汶川MS8.0地震的“孕育”、发生和发展是深部物质分异、调整和运移的产物.为此,在四川中西部地区(松潘—甘孜,龙门山断裂系和四川盆地)应用重力布格异常场资料并通过两条典型剖面的地壳厚度(Moho界面深度)分布与依据Airy均衡理论给出的理论均衡地壳厚度做对比分析,探讨四川盆地、龙门山造山带、邛崃山等川西地域的地壳均衡状态,得到龙门山及其以西地带的深部地壳结构.龙门山造山带恰处于很不均衡的状态,即与其西北和东南部相比差异明显,故地壳处于不稳定状态.为探讨该区重力场均衡与强烈地震活动之间的关系,还必须进行新一轮的高精度观测,以对该区深部精细结构、重力场效应和均衡补偿深入研究.此外,本文研究结果有益于震后确定城镇布局和为不同类型建筑物重建选址提供深部要素. 相似文献
39.
考虑时变影响的拱坝坝肩空间变形场预测 总被引:1,自引:0,他引:1
坝肩变形是拱坝坝肩稳定状态的综合反映,在运行期呈小变形变化,监测点测值在空间上具有连续性,同时影响拱坝坝肩变形的各种因素具有时变性。通过融合统计回归和多层递阶方法的特点,建立了反映变形场空间和时变特性的空间时变分析模型。实例分析表明,该模型实用有效,预测精度高。考虑时变影响可以提高拱坝坝肩空间变形场的预测能力,对监控拱坝坝肩的实际工作状况有重要意义。 相似文献
40.
Lech Krysiński 《Pure and Applied Geophysics》2009,166(3):375-408
The paper describes a new method of gravity modelling of the density cross section along a DSS profile. We propose a systematic
procedure of gravity interpretation using structural information contained both in the velocity distribution of the seismic
model and the geometry of its layers. The procedure is based on the optimisation of the density parameters of the model. The
values of the parameters are limited by relationships between the seismic velocity and the density (optimisation with inequalities).
The formulation of the method allows for discussion of the presence of isostasy and the distribution of compensating masses.
The discussion is very important for the considered crust-lithosphere system. The presented calculations are done for one
Carpathian profile (CEL01). The analysis of the properties of the fitting procedure provides the characteristic depth of subcrustal
compensating density structures, the position of crucial tectonic boundaries along the profiles, locations of the crustal
areas having exceptional lithology, the regional density differences of subcrustal matter and the estimation of regional deviations
from the isostatic equilibrium. 相似文献