全文获取类型
收费全文 | 5628篇 |
免费 | 1423篇 |
国内免费 | 1750篇 |
专业分类
测绘学 | 882篇 |
大气科学 | 958篇 |
地球物理 | 1378篇 |
地质学 | 3206篇 |
海洋学 | 1024篇 |
天文学 | 144篇 |
综合类 | 515篇 |
自然地理 | 694篇 |
出版年
2024年 | 52篇 |
2023年 | 162篇 |
2022年 | 387篇 |
2021年 | 533篇 |
2020年 | 405篇 |
2019年 | 491篇 |
2018年 | 447篇 |
2017年 | 400篇 |
2016年 | 392篇 |
2015年 | 413篇 |
2014年 | 392篇 |
2013年 | 427篇 |
2012年 | 479篇 |
2011年 | 444篇 |
2010年 | 415篇 |
2009年 | 441篇 |
2008年 | 321篇 |
2007年 | 319篇 |
2006年 | 292篇 |
2005年 | 247篇 |
2004年 | 206篇 |
2003年 | 147篇 |
2002年 | 162篇 |
2001年 | 161篇 |
2000年 | 127篇 |
1999年 | 112篇 |
1998年 | 72篇 |
1997年 | 54篇 |
1996年 | 45篇 |
1995年 | 34篇 |
1994年 | 40篇 |
1993年 | 31篇 |
1992年 | 25篇 |
1991年 | 24篇 |
1990年 | 19篇 |
1989年 | 19篇 |
1988年 | 22篇 |
1987年 | 8篇 |
1986年 | 9篇 |
1985年 | 2篇 |
1984年 | 4篇 |
1983年 | 1篇 |
1982年 | 4篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1979年 | 3篇 |
1978年 | 1篇 |
1958年 | 4篇 |
1957年 | 2篇 |
1954年 | 1篇 |
排序方式: 共有8801条查询结果,搜索用时 421 毫秒
991.
COSEISMIC DISPLACEMENT FIELD OF THE WENCHUAN EARTHQUAKE DERIVED FROM STRONG MOTION RECORDS AND APPLICATION IN SLIP INVERSION
下载免费PDF全文
![点击此处可从《地震地质》网站下载免费的PDF全文](/ch/ext_images/free.gif)
The development of high-rate GNSS seismology and seismic observation methods has provided technical support for acquiring the near-field real-time displacement time series during earthquake. But in practice, the limited number of GNSS continuous stations hardly meets the requirement of near-field quasi-real-time coseismic displacement observation, while the macroseismographs could be an important complement. Compared with high-rate GNSS, macroseismograph has better sensitivity, higher resolution(100~200Hz)and larger dynamic range, and the most importantly, lower cost. However, baseline drift exists in strong-motion data, which limits its widespread use. This paper aims to prove the feasibility and reliability of strong motion data in acquiring seismic displacement sequences, as a supplement to high-rate GNSS.
In this study, we have analyzed the strong-motion data of Wenchuan MS8.0 earthquake in Longmenshan fault zone, based on the automatic scheme for empirical baseline correction proposed by Wang et al., which fits the uncorrected displacement by polynomial to obtain the fitting parameters, and then the baseline correction is completed in the velocity sequence. Through correction processing and quadratic integration, the static coseismic displacement field and displacement time series are obtained. Comparison of the displacement time series from the strong motions with the result of high-rate GPS shows a good coincidence. We have worked out the coseismic displacement field in the large area of Wenchuan earthquake using GPS data and strong motion data. The coseismic displacement fields calculated from GPS and strong motions are consistent with each other in terms of magnitude, direction and distribution patterns. High-precision coseismic deformation can provide better data constraint for fault slip inversion. To verify the influence of strong-motion data on slip distribution in Wenchuan earthquake, we used strong motion, GPS and InSAR data to estimate the stress drop, moment magnitude and coseismic slip model, and our results agreed with those of the previous studies. In addition, the inversion results of different data are different and complementary to some extent. The use of strong-motion data supplements the slip of the fault in the 180km segment and the 270~300km segment, thus making the inversion results of fault slip more comprehensive.
From this result, we can draw the following conclusions:1)Based on the robust baseline correction method, the use of strong motion data, as an important complement to high-rate GNSS, can obtain reliable surface displacement after the earthquake. 2)The strong motion data provide an effective method to study the coseismic displacement sequence, the surface rupture process and quick seismogenic parameters acquisition. 3)The combination of multiple data can significantly improve the data coverage and give play to the advantages of different data. Therefore, it is suggested to combine multiple data(GPS, strong motion, InSAR, etc.)for joint inversion to improve the stability of fault slip model. 相似文献
992.
CHARACTERISTICS OF TECTONIC STRESS FIELD OF THE XIAOWAN RESERVOIR BEFORE AND AFTER THE IMPOUNDMENT
下载免费PDF全文
![点击此处可从《地震地质》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Using the seismic waveform data of Xiaowan seismic network and Yunnan seismic network, we determined the focal mechanisms of 36 earthquakes(ML ≥ 3.0)from Jun. 2005 to Dec. 2008 and 51 earthquakes(ML ≥ 2.5)from Jan. 2009 to Dec. 2015 by generalized polarity and amplitude technique.
We inverted tectonic stress field of the Xiaowan reservoir before impounding, using the focal mechanisms of 36 earthquakes(ML ≥ 3.0)from Jun. 2005 to Dec. 2008 and CAP solutions of 58 earthquakes(ML ≥ 4.0)collected and the solutions in the Global Centroid Moment Tensor(GCMT)catalog; We inverted local stress field of the reservoir-triggered earthquake clustering area, using 51 earthquakes(ML ≥ 2.5)from Jan. 2009 to Dec. 2015.
Focal mechanisms statistics show that, the Weixi-Qiaohou Fault is the seismic fault. Focal mechanisms were strike-slip type in initial stage, but normal fault type in later stage. Focal depths statistics of 51 earthquakes(ML ≥ 2.5)show that, the average value of focal depths in period Ⅰ, period Ⅱ and period Ⅲ are 8.2km, 7.3km and 7.8km respectively and the standard deviations are 4.3km, 3.5km and 6.0km respectively. The average value of focal depths is basically stable in different period, only the standard deviation is slightly different. Therefore, there is not positive connection between focal depth and deviation of focal mechanisms. What's more, there are 2 earthquakes(number 46 and number 47 in Fig.5 and Table 3)with almost the same magnitude, epicenter and focal depth, but they have different faulting types as normal and strike-slip. The focal mechanism of event No.46 is strike:302°, dip:40° and rake:-97° for plane Ⅰ, however, the focal mechanism of event No.47 is strike:292°, dip:82° and rake:140° for plane Ⅰ. Likewise, earthquake of number 3 and number 18 have similar characteristic. Therefore, the obvious focal mechanism difference of similar earthquake pair indicates the complexity of Weixi-Qiaohou Fault.
Considering the quiet-active character of reservoir-triggered earthquakes, we discussed the change of local stress field in different period. The σ1 of tectonic stress field was in the near-south direction, with a dip angle of 14° before the impoundment, however, the direction of σ1 of local stress field changed continuously, with the dip angle getting larger after the impoundment. The direction of σ1 of local stress field of reservoir-triggered earthquake clustering area is close to the strike of Weixi-Qiaohou Fault, and reservoir impoundment increased the shear stress in the fault, so the weakening of fault was beneficial to trigger earthquakes. Comprehensive analysis suggests that fluid permeation and pore pressure diffusion caused by the water impounding, and the weakening of fault caused by local stress field are the key factors to trigger earthquake in the Xiaowan reservoir. 相似文献
993.
994.
根据天山中段8套四分量钻孔应变仪观测资料,利用自洽方程计算应变观测的信度,用信度指标检验数据的可靠性,从而进一步用自洽方程计算实际各元件灵敏度的相对大小,并用相对标定的结果,对观测数据进行校正。结果表明:①石场、巴仑台、巴音沟、雀儿沟、榆树沟和库米什台经过校正后,数据观测信度有了明显提升,其中石场和雀儿沟台的数据信度最高;②库米什台校正前数据观测信度较高,因个别“坏点”影响,校正后,观测信度反而下降;③小泉沟和新源台数据信度较低,存在从自洽到失洽的情况,分析认为这可能与系统自身存在问题有关,也有可能是前兆异常,有待进一步研究。 相似文献
995.
基于Sato模型的内蒙古东北部地区尾波Q值 总被引:1,自引:1,他引:0
基于Sato模型,采用2016年3月至2018年6月内蒙古东北部及临近地区发生的526次地震事件,挑选M_L≥2.0、记录清晰且信噪比较高的102次地震事件,拟合得到内蒙古东北部地区尾波Q值,得到Q_C(f)=(64.74±29.09)f(0.8925±0.0765);Q值与依赖指数η成反比,且该区北部Q值偏高,南部Q值偏低,可能与地质构造及地震活动性有关。 相似文献
996.
997.
根据乌海地区构造环境,采用SAM方法研究乌海地区地壳各向异性特征,使用乌海地震台2014年1月至2020年6月数字地震波形进行分析。根据65个有效地震记录,得到乌海地区剪切波分裂参数,其中快剪切波平均优势偏振方向为NE63.1°±46.4°,慢剪切波平均时间延迟为(1.13±0.66)ms/km。乌海地震台快剪切波偏振显示出4个优势偏振方向,分别为NE、EW、NNE、NNW向。将得到的各向异性结果与研究区应力场和地质构造进行分析,认为研究区周边复杂的剪切波分裂变化是主压应力场、原地主压应力、断裂带分布共同作用的结果。 相似文献
998.
It is well-known that the responses of a structure are different when subjected to a static load or a sudden step load. The dynamic amplification factor (DAF), which is defined as the ratio of the amplitude of the vibratory response to the static response, is normally used to depict the dynamic effect. For a single-degree-of-freedom system (SDOF) subjected to a sudden dynamic load, the maximum value of DAF is 2. Many design guidelines therefore use 2 as an upper bound to consider the dynamic effect. For a civil engineering structure, which is normally a multiple-degrees-of-freedom (MDOF) system, the DAF may exceed 2 in certain circumstances. The adoption of 2 as the upper bond as suggested by the design guidelines therefore may lead to unsafe structural design. Very limited studies systematically investigate the DAF of a MDOF system. This study theoretically investigates the DAF of a MDOF system when it is subjected to a step load based on the fundamental theory of structural dynamics. The condition on which the DAF may exceed 2 is defined. Two numerical examples and one experimental study of a cable-stayed bridge subjected to sudden cable loss are presented to illustrate the problem. 相似文献
999.
准确定量分析湖泊河流中浮游植物群落结构对评价湖泊河流健康和保障人类饮水安全至关重要.显微镜镜检法是定量分析浮游植物群落结构的唯一方法,但不能满足浮游植物计数分析要求.在Utermhl倒置计数管视野法基础上提出倒置显微镜拍照法,使用拍照法对小球藻、四尾栅藻、斜生栅藻3种纯藻样品和鄱阳湖野外样品计数得到:1)在5、10倍物镜下拍照因浮游植物个体太小导致计数不准确,在20、40倍物镜下拍照计数准确,增加拍照次数可较好地避免计数偏差,拍照次数是影响拍照法计数分析的主要因素; 2)小球藻、四尾栅藻、斜生栅藻在20和40倍物镜下分别拍摄5和10张照片时每升浮游植物计数稳定;鄱阳湖野外样品在20和40物镜倍下分别拍摄5、10张照片时每升浮游植物计数稳定; 3)倒置显微镜拍照法比计数框行格法、目镜视野法、目镜行格法和Utermhl倒置计数管视野法计数稳定,变异系数最小为0.812. 相似文献
1000.