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101.
102.
洪泽地区由于沉积的特点,储层横向变化快,油藏受构造、岩性、油源多因素控制。在对该区三维AVO属性体解释中,利用多元回归方法求取了横波曲线,分岩性和含油气性统计了纵、横波、泊松比参数分布规律,建立了本区的含油砂岩的正演模型,从而降低了AVO解释的多解性。通过井-震结合对四种AVO属性数据体进行了标定,并确定了各属性体应用范围,进而进行了储层和含油气检测。实践表明,该方法能有效地利用AVO属性数据体进行储层预测及油气检测,具有一定的推广价值。 相似文献
103.
We analysed local earthquake waveforms recorded on a broad-band seismic network in northwestern Himalayas to compute the intrinsic and scattered attenuation parameters from coda waves. Similar to other tectonically active and heterogeneous regions, attenuation-frequency relation for western Himalaya is Q −1 c = (113 ± 7) f (1.01±0.05) where Qc is the coda Q parameter. Intrinsic ( Q −1 i ) and scattering ( Q −1 s ) attenuations was separated using Qc and direct S -wave Q data ( Qd ) . It is observed that estimated Q −1 c is close to Q −1 i and both of them are much larger than Q −1 s suggesting that coda decay is predominantly caused by intrinsic attenuation. At higher frequencies, both the attenuation parameters Qc and, Qd are similar indicating that coda is predominantly composed of back-scattered S waves at these frequencies. 相似文献
104.
A. D. Kuzmin V. I. Kondrat’ev S. V. Kostyuk B. Ya. Losovsky M. V. Popov V. A. Soglasnov N. D’Amico S. Montebugnoli 《Astronomy Letters》2002,28(4):251-256
We measured the frequency dependence of the pulsar pulse broadening by scattering over a wide frequency range, from 40 to 2228 MHz, based on direct measurements of this parameter using giant pulses from the pulsar PSR B0531+21 in the Crab Nebula. Our measurements were carried out at the following seven frequencies: 40, 60, and 111 MHz at the Pushchino Radio Astronomy Observatory (Astrospace Center, Lebedev Physical Institute, Russian Academy of Sciences), 406 MHz at the Medicina Observatory (Instituto di Radioastronomia, Italy), and 594, 1430, and 2228 MHz at the Kalyazin Radio Astronomy Observatory (Astrospace Center, Lebedev Physical Institute, Russian Academy of Sciences). The measured frequency dependence of the pulse broadening by scattering τSC (υ) ? υγ, where γ=?3.8±0.2, agrees with a model Gaussian distribution of interstellar inhomogeneities (γ=?4) but falls outside the error limits of correspondence to a Kolmogorov model spectrum of inhomogeneities (γ=?4.4). 相似文献
105.
用紫金山天文台青海观测站13.7米毫米波望远镜新安装的3毫米系统,对一组包括大质量恒星形成区、稠密云核、Bok球、主序前发射线星和演化晚期恒星的源进行了12COJ=1-0的辐射搜寻.结果在不同质量恒星形成区域全部测到了12CO辐射,并发现了大的线宽、红和蓝的线翼、线心速度变化及多重辐射的特征,表明相应源可能具有双极喷流,存在膨胀、旋转或多核斑结构.有两个演化晚期星中已观测到了12COJ=1-0谱线,说明其具有较浓厚的拱星气体包层. 相似文献
106.
The May 20, 1986, Hualien earthquake sequence occurred on the northeastern coast of Taiwan. TheM=6.1 (GS mb) mainshock was followed by a large number of closely-clustered aftershocks with the largest being anM=5.5 event. One seismic station, TWD of the Taiwan Telemetered Seismographic Network, is located in the surface projection of the source region and provides excellent recordings of the entire earthquake sequence. These recordings, plus events occurring in the same source area preceding the mainshock, offer a unique opportunity to study the spatial and temporal variations of codaQ in a region of active subduction. A simple technique is devised that uses the envelope of the coda waveform to enable a quick determination of the codaQ from drum records. For recordings with a peak power at about 8 Hz, the following findings have been obtained: 1. The ambient codaQ near an active subduction region was as low as 145; 2. There was no significant decrease in codaQ within the period beginning one year and four months prior to the mainshock; 3. There was a significant drop of codaQ immediately after the mainshock; this drop lasted approximately two days before returning to the ambient level; 4. CodaQ values varied with focal depth. 相似文献
107.
用WKBJ方法结合特征线法求得了重力波波包在水平非均匀层结和时变层结大气中演变的渐近解,结果表明层结水平非均匀性除引起重力波波幅的变化外,还引起波长和包络宽度的变化,当波包由层结大值区移向层结小值区时,水平波长变短,包络宽度变窄,同时振幅增加。层结随时间的变化不会引起波包波长和包络的宽度的变化,但层结随时间减小时,波包振幅增加。 相似文献
108.
Inversion of local S-wave velocity structures from average H/V ratios, and their use for the estimation of site-effects 总被引:2,自引:1,他引:2
H/V spectral ratios from microtremors areused to retrieve the S-velocity structurefrom a single ambient vibration record, byusing its relation to the ellipticity ofthe fundamental mode Rayleigh wave and theamplitude of observed H/V ratio.Constraints are needed in order to restrictthe possible range of solutions, and theinversion is applied to sites where thethickness of the unconsolidated sedimentsis approximately known from boreholeinformation. Within the uncertainty, theinverted structures agree well with theresults from other S-wave measuringtechniques such as downhole and cross-holemeasurements, and the analysis of ambientvibrations measured on an array.The influence of the inversion uncertaintyon site-amplification estimates forearthquakes is then investigated. For allinverted models, site response is computedfor a large number of events, which allowsto define the uncertainty by the aprioriunknown source position and mechanism of afuture earthquake. In most cases thevariability between the results obtainedfor the different models is much smallerthan the variability introduced by theunknown source position. The accuracy withwhich S-wave velocity structures can beretrieved from observed H/V ratios istherefore sufficient for an application ofthe method in seismic hazard analysis for aspecific site. 相似文献
109.
将复模量引入Biot方程后,在一维条件下通过S波的波动方程研究了S波的传播特性,S波的数值分析显示在频率域或温度域上都能获得热弛豫衰减峰和Biot衰减峰. 在频率域上由于温度的变化引起两峰相向位移,在温度域上,因频率的变化也发生相对移动. 随着温度和频率的不断提高,两峰发生叠加,叠加后两峰互换位置. 低频或低温段的热弛豫峰移到了高频或高温段,高频或高温段的Biot峰移到了低频或低温段.由于两峰的衰减机制不同,导致S波波速随频率或温度变化规律的复杂性. 这些规律已部分被共振实验所证实,证实该理论模型具有实验基础. 相似文献
110.
人工横波地震是工程物探的一种新技术,但由于理论上存在一些误区,在工程实践中给地质解释带来一定困难。正确理解和计算横波波速是解决这个问题的首要任务,利用多次叠加时动校正的速度能量团计算横波速度比较可靠,该技术的应用已成功地解决了一些疑难复杂地质问题。准确的横波波速计算可使横波勘探得到更好地推广和应用,为工程设计和建设提供可靠的地质资料。 相似文献