全文获取类型
收费全文 | 4041篇 |
免费 | 1084篇 |
国内免费 | 114篇 |
专业分类
测绘学 | 5篇 |
大气科学 | 1篇 |
地球物理 | 4099篇 |
地质学 | 857篇 |
海洋学 | 155篇 |
天文学 | 9篇 |
综合类 | 32篇 |
自然地理 | 81篇 |
出版年
2024年 | 20篇 |
2023年 | 62篇 |
2022年 | 95篇 |
2021年 | 76篇 |
2020年 | 145篇 |
2019年 | 152篇 |
2018年 | 125篇 |
2017年 | 150篇 |
2016年 | 155篇 |
2015年 | 151篇 |
2014年 | 267篇 |
2013年 | 182篇 |
2012年 | 129篇 |
2011年 | 183篇 |
2010年 | 183篇 |
2009年 | 243篇 |
2008年 | 269篇 |
2007年 | 217篇 |
2006年 | 225篇 |
2005年 | 202篇 |
2004年 | 167篇 |
2003年 | 161篇 |
2002年 | 194篇 |
2001年 | 137篇 |
2000年 | 147篇 |
1999年 | 125篇 |
1998年 | 135篇 |
1997年 | 128篇 |
1996年 | 170篇 |
1995年 | 151篇 |
1994年 | 105篇 |
1993年 | 107篇 |
1992年 | 57篇 |
1991年 | 48篇 |
1990年 | 46篇 |
1989年 | 31篇 |
1988年 | 25篇 |
1987年 | 20篇 |
1986年 | 5篇 |
1985年 | 5篇 |
1984年 | 14篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1980年 | 4篇 |
1979年 | 4篇 |
1978年 | 4篇 |
1977年 | 8篇 |
1954年 | 6篇 |
排序方式: 共有5239条查询结果,搜索用时 15 毫秒
331.
Dacite tephras produced by the 1991 pre-climactic eruptive sequence at Mt. Pinatubo display extreme heterogeneity in vesicularity,
ranging in clast density from 700 to 2580 kg m–3. Observations of the 13 surge-producing blasts that preceded the climactic plinian event include radar-defined estimates
of column heights and seismically defined eruptive and intra-eruptive durations. A comparison of the characteristics of erupted
material, including microlite textures, chemical compositions, and H2O contents, with eruptive parameters suggests that devolatilization-induced crystallization of the magma occurred to a varying
extent prior to at least nine of the explosive events. Although volatile loss progressed to the same approximate level in
all of the clasts analyzed (weight percent H2O=1.26-1.73), microlite crystallization was extremely variable (0–22%). We infer that syn-eruptive volatile exsolution from
magma in the conduit and intra-eruptive separation of the gas phase was facilitated by the development of permeability within
magma residing in the conduit. Correlation of maximum microlite crystallinity with repose interval duration (28–262 min) suggests
that crystallization occurred primarily intra-eruptively, in response to the reduction in dissolved H2O content that occurred during the preceding event. Detailed textural characterization, including determination of three-dimensional
shapes and crystal size distributions (CSD), was conducted on a subset of clasts in order to determine rates of crystal nucleation
and growth using repose interval as the time available for crystallization. Shape and size analysis suggests that crystallization
proceeded in response to lessening degrees of feldspar supersaturation as repose interval durations increased. We thus propose
that during repose intervals, a plug of highly viscous magma formed due to the collapse of vesicular magma that had exsolved
volatiles during the previous explosive event. If plug thickness grew proportionally to the square root of time, and if magma
pressurization increased during the eruptive sequence, the frequency of eruptive pulses may have been modulated by degassing
of magma within the conduit. Dense clasts in surge deposits probably represent plug material entrained by each subsequent
explosive event.
Received: 4 December 1997 / Accepted: 13 September 1998 相似文献
332.
We analyzed more than 1700 earthquakes related to the 1982 eruption of El Chichon volcano in southern Mexico. The data were
recorded at specific periods throughout the whole eruptive interval of March to April 1982, by three different networks. The
seismic activity began several months before the first eruption on 28 March. During this period the seismicity consisted of
hybrid and long-period shallow earthquakes most likely related to processes of faulting, fracturing, and fluid movement underneath
the volcano. The foci of events occurring before the eruption circumscribe an aseismic zone from approximately 7 to 13 km
below the volcano. After the eruption, the seismic activity consisted of tectonic-type earthquakes that peaked at 1200 events/h.
This later activity occurred over a wide range of depths, mostly between 5 and 20 km, that includes the former aseismic zone
and is roughly limited by the major tectonic faults in the area.
Received: 19 May 1998 / Accepted: 13 June 1999 相似文献
333.
W.A. Mulder 《Geophysical Prospecting》2014,62(1):17-33
Migration velocity analysis with the constant‐density acoustic wave equation can be accomplished by the focusing of extended migration images, obtained by introducing a subsurface shift in the imaging condition. A reflector in a wrong velocity model will show up as a curve in the extended image. In the correct model, it should collapse to a point. The usual approach to obtain a focused image involves a cost functional that penalizes energy in the extended image at non‐zero shift. Its minimization by a gradient‐based method should then produce the correct velocity model. Here, asymptotic analysis and numerical examples show that this method may be too sensitive to amplitude peaks at large shifts at the wrong depth and to artefacts. A more robust alternative is proposed that can be interpreted as a generalization of stack power and maximizes the energy at zero‐subsurface shift. A real‐data example is included. 相似文献
334.
Faisal Alonaizi Roman Pevzner Andrej Bóna Mohammad Alshamry Eva Caspari Boris Gurevich 《Geophysical Prospecting》2014,62(2):197-209
Time‐lapse seismic analysis is utilized in CO2 geosequestration to verify the CO2 containment within a reservoir. A major risk associated with geosequestration is a possible leakage of CO2 from the storage formation into overlaying formations. To mitigate this risk, the deployment of carbon capture and storage projects requires fast and reliable detection of relatively small volumes of CO2 outside the storage formation. To do this, it is necessary to predict typical seepage scenarios and improve subsurface seepage detection methods. In this work we present a technique for CO2 monitoring based on the detection of diffracted waves in time‐lapse seismic data. In the case of CO2 seepage, the migrating plume might form small secondary accumulations that would produce diffracted, rather than reflected waves. From time‐lapse data analysis, we are able to separate the diffracted waves from the predominant reflections in order to image the small CO2 plumes. To explore possibilities to detect relatively small amounts of CO2, we performed synthetic time‐lapse seismic modelling based on the Cooperative Research Centre for Greenhouse Gas Technologies (CO2CRC) Otway project data. The detection method is based on defining the CO2 location by measuring the coherency of the signal along diffraction offset‐traveltime curves. The technique is applied to a time‐lapse stacked section using a stacking velocity to construct offset‐traveltime curves. Given the amount of noise found in the surface seismic data, the predicted minimum detectable amount of CO2 is 1000–2000 tonnes. This method was also applied to real data obtained from a time‐lapse seismic physical model. The use of diffractions rather than reflections for monitoring small amounts of CO2 can enhance the capability of subsurface monitoring in CO2 geosequestration projects. 相似文献
335.
中国西部地区是地震活动十分强烈的地区,天山、阿尔泰、帕米尔和西昆仑都是著名的地震构造带,在这些地震构造带和周边地区发生了多次震级大于5级的强震.本文通过分析西部地区的重力场特征,根据重力数据结合地震剖面、应用Parker-Oldenburg方法反演得到了研究区莫霍面深度,通过对比地震层析成像的反演结果,分析了研究区的地壳结构特征.计算结果表明,研究区地壳结构不均匀特征明显,在造山带地区一般是莫霍面坳陷区,盆地则是莫霍面隆起区,主要造山带地壳速度结构表现为高速区,盆地和主要凹陷区为低速区.根据计算结果和以往强震震中位置分析了地壳构造与强震活动的相关性,西部地区的地震活动与地壳结构的横向不均匀密切相关,强震主要发生在地壳速度变化带附近和地壳速度结构差异较大的地区,在构造应力作用下,这些地壳介质非均匀地区易发生强震,这是中国西部造山带和盆-山边界附近频发强震的构造原因之一. 相似文献
336.
潮汐应力-应变对某些地震序列的调制触发 总被引:1,自引:1,他引:1
对1960年以来中国大陆浅源地震序列与潮汐应变的相关分析表明, 某些地区某些地震序列, 包括前震序列、 前震-主震序列、 前震-主震-余震序列和主震-余震序列明显受到潮汐应力-应变的调制触发。 如龙陵地震的前震-主震序列, 邢台地震的前震-主震-余震序列、 唐山地震的主震-余震序列等。 这些地震序列受到潮汐力调制触发的特征明显, 对地震预测有意义, 并作了具体的叙述。 同时对地震序列受调制触发的机理作了初步的探讨, 指出不同类型地震序列的调制触发特征与孕育系统地质构造, 地震震源岩石性质和区域构造应力场方向以及地震破裂机制有关, 对地震机理和预测的研究有一定意义。 相似文献
337.
ESEP3.0专家系统在新疆年度地震形势预测中的应用检验 总被引:1,自引:0,他引:1
使用2000—2003年度新疆地震局震情研究报告中的资料建立异常证据文件,应用ESEP3.0专家系统进行了推理预测,将其中的1年以内的预测意见与这4年新疆“震情研究报告”的预测意见及实际发生的地震情况进行了对比,并按中国地震局制定的“地震预报评分办法”进行了评分,最后认为:ESEP3.0专家系统目前可以用于新疆的年度地震趋势和地震危险区预测。 相似文献
338.
339.
340.
应用Windows操作系统的网络技术和自行开发的报警软件,解决了牡丹江地震台连续波形数据断记问题。本文详细介绍了解决方案和报警软件的安装及使用方法。 相似文献