全文获取类型
收费全文 | 43965篇 |
免费 | 7671篇 |
国内免费 | 9662篇 |
专业分类
测绘学 | 3517篇 |
大气科学 | 6651篇 |
地球物理 | 8873篇 |
地质学 | 22946篇 |
海洋学 | 5762篇 |
天文学 | 3638篇 |
综合类 | 2654篇 |
自然地理 | 7257篇 |
出版年
2024年 | 201篇 |
2023年 | 569篇 |
2022年 | 1431篇 |
2021年 | 1685篇 |
2020年 | 1670篇 |
2019年 | 2108篇 |
2018年 | 1525篇 |
2017年 | 1761篇 |
2016年 | 1775篇 |
2015年 | 1969篇 |
2014年 | 2535篇 |
2013年 | 2716篇 |
2012年 | 2621篇 |
2011年 | 2829篇 |
2010年 | 2423篇 |
2009年 | 3050篇 |
2008年 | 3008篇 |
2007年 | 3060篇 |
2006年 | 3009篇 |
2005年 | 2731篇 |
2004年 | 2422篇 |
2003年 | 2304篇 |
2002年 | 1977篇 |
2001年 | 1743篇 |
2000年 | 1722篇 |
1999年 | 1554篇 |
1998年 | 1321篇 |
1997年 | 985篇 |
1996年 | 852篇 |
1995年 | 714篇 |
1994年 | 656篇 |
1993年 | 575篇 |
1992年 | 421篇 |
1991年 | 365篇 |
1990年 | 251篇 |
1989年 | 198篇 |
1988年 | 165篇 |
1987年 | 90篇 |
1986年 | 56篇 |
1985年 | 50篇 |
1984年 | 35篇 |
1983年 | 26篇 |
1982年 | 22篇 |
1981年 | 18篇 |
1980年 | 15篇 |
1979年 | 6篇 |
1978年 | 28篇 |
1977年 | 10篇 |
1976年 | 4篇 |
1954年 | 11篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
981.
Christoph Breitkreuz Lucio Cortesogno Laura Gaggero 《Journal of Volcanology and Geothermal Research》2002,114(3-4)
Sedimentological, granulometric and petrographic data are presented from a detailed study on a crystal-rich mass flow deposit, which is presumably related to the eruption of a sublacustrine cryptodome. The deposit forms a prominent intercalation in the Lower Permian Collio Formation in the Italian Alps north of Brescia. Outcrops of the 10–20-m-thick volcaniclastic deposit (Dasdana I Beds, DB) can be traced over 12 km from east to west. The DB consists of a thick, crystal-rich, sandy–gravelly lower subunit representing a sequence of amalgamated Bouma-a(b) divisions overlain by a thin, well-bedded, sandy–muddy subunit that is rich in outsize porphyritic silicic fragments. Modal and computer-aided image analyses reveal that the crystal-rich lower subunit contains up to 80% of volcanogenic crystals. Some samples contain up to 60% of porphyritic fragments, which have a phenocryst content of about 20%. The wide textural range from cryptocrystalline, poikilomosaic, to rarer medium-grained granophyric groundmass, the irregular to lensoid shapes of the porphyritic fragments, and the presence of basement and sedimentary clasts suggest that the DB originated from a sublacustrine eruption of a partially extrusive cryptodome (ca. 1.6 km3). Two other porphyritic felsic cryptodomes (Dosso dei Lupi, Dosso del Bue), described briefly here, emplaced into the Collio Formation sometime after the DB event, and expose flat bases and tilted sediments at their sides. Textures observed in these domes are comparable to those found in the DB porphyritic fragments. 相似文献
982.
It is critical to understand and quantify the temporal and spatial variability in hillslope hydrological data in order to advance hillslope hydrological studies, evaluate distributed parameter hydrological models, analyse variability in hydrological response of slopes and design efficient field data sampling networks. The spatial and temporal variability of field‐measured pore‐water pressures in three residual soil slopes in Singapore was investigated using geostatistical methods. Parameters of the semivariograms, namely the range, sill and nugget effect, revealed interesting insights into the spatial structure of the temporal situation of pore‐water pressures in the slopes. While informative, mean estimates have been shown to be inadequate for modelling purposes, indicator semivariograms together with mean prediction by kriging provide a better form of model input. Results also indicate that significant temporal and spatial variability in pore‐water pressures exists in the slope profile and thereby induces variability in hydrological response of the slope. Spatial and temporal variability in pore‐water pressure decreases with increasing soil depth. The variability decreases during wet conditions as the slope approaches near saturation and the variability increases with high matric suction development following rainfall periods. Variability in pore‐water pressures is greatest at shallow depths and near the slope crest and is strongly influenced by the combined action of microclimate, vegetation and soil properties. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
983.
Channel curvature produces secondary currents and a transverse sloping channel bed, along which the depth increases towards the outer bank. As a result deep pools tend to form adjacent to the outer bank, promoting bank collapse. The interaction of sediment grains with the primary and secondary flow and the transverse sloping bed also causes meanders to move different grain sizes in different proportions and directions, resulting in a consistent sorting pattern. Several models have been developed to describe this process, but they all have the potential to over‐predict pool depth because they cannot account for the influence of erodible banks. In reality, bank collapse might lead to the development of a wider, shallower cross‐section and any resulting flow depth discrepancy can bias associated predictions of flow, sediment transport, and grain‐size sorting. While bed topography, sediment transport and grain sorting in bends will partly be controlled by the sedimentary characteristics of the bank materials, the magnitude of this effect has not previously been explored. This paper reports the development of a model of flow, sediment transport, grain‐size sorting, and bed topography for river bends with erodible banks. The model is tested via intercomparison of predicted and observed bed topography in one low‐energy (5·3 W m?2 specific stream power) and one high‐energy (43·4 W m?2) study reach, namely the River South Esk in Scotland and Goodwin Creek in Mississippi, respectively. Model predictions of bed topography are found to be satisfactory, at least close to the apices of bends. Finally, the model is used in sensitivity analyses that provide insight into the influence of bank erodibility on equilibrium meander morphology and associated patterns of grain‐size sorting. The sensitivity of meander response to bank cohesion is found to increase as a function of the available stream power within the two study bends. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
984.
中国西南及邻区上地幔P波三维速度结构/ 总被引:8,自引:0,他引:8
利用ISC报告以及中国和NEIC基本测震台网报告中的80974条P波初至到时资料(地震数为7053,台站数为165,且地震和台站都分布在研究区内),对中国西南及邻区(北纬10~36、东经70~110)的深至400km的上地幔三维速度结构进行了研究,分辨率达22.初步结果表明:①研究区速度的横向不均匀性,虽随深度增加而减弱,但至400km深度时仍很明显;②在北纬16和24的纵剖面上,可以看到与印度板块向东和欧亚板块相碰撞挤压相对应的速度结构,以及印度板块与欧亚板块速度结构的差异.在东经90的纵剖面上,与印度板块向北俯冲到欧亚板块(青藏高原)之下相对应的速度结构也比较明显;③在90km深度的横剖面上,由缅甸的密支那至越南的洞海的低速条带,可能与红河断裂带有关;④ 提出并使用了能够更为准确直观地描述分辨率好坏的图示方法. 相似文献
985.
提出了一种估计一个地区平均构造剪应力值的方法.用这种方法,选取哈佛大学公布的1977~1999年共15 993次地震的矩张量数据,估计了美国西部19个地区、中国和邻区43个地区(每个地区为1010范围)的平均环境剪应力值.结果表明,美国西部南加州西部海域和南加州应力最高,达13.7和12.0 MPa,然后向北、向南和向东逐渐递减,但最小也达8.7 MPa,是最高值的63%.中国新疆西北部地区和西藏察隅地区应力水平最高,达17.2和12.9 MPa,比美国高.中国的华北、云南、四川、台湾和美国南加州的应力水平差不多.中国南北地震带的应力水平为13 MPa左右,比南加州略高.两个重要地区的平均剪应力值分布图,提供了地学的基本数据.这些结果可为研究地震活动的大背景提供依据,对研究强地面运动参数(如峰值加速度及反应谱等)的衰减关系也是有用的. 相似文献
986.
987.
利用172-182年IMP-8飞船的太阳风观测资料和相应地磁活动性指数Dst和AE,研究了43个南向行星际磁场事件期间太阳风和磁层的耦合问题. 与这43个事件对应的地磁暴是中等的和强的磁暴(Dst<-50nT). 结果表明:(1) 在43个事件中有11个(约占25.6髎)紧随激波之后,18个处于激波下游流场中(占42髎),其余14个(占33髎)和激波没有关连. 绝大多数事件都伴有太阳风动压和总磁场强度的增加;(2) 当行星际晨昏向电场强度EI>-4mV/m时,只引起磁亚暴,对Dst指数没有明显影响. 仅当EI<-5mV/m时,磁亚暴和磁暴才会同时出现;(3) 太阳风动压的增加会增强能量向环电流的输入,但不是密度和速度单独起作用,而是以PK=ρV2的组合形式影响能量的输入;(4) 虽然行星际磁场(IMF)南向分量BZ对太阳风和磁层的耦合起着关键作用,但IMF的BX和BY分量相对于BZ的大小对太阳风向磁层的能量传输也有一定影响. 当BX、BY相对BZ较大时能量耦合加强. 相似文献
988.
流动成像测井研究进展 总被引:2,自引:3,他引:2
流动成像测井属于对非均匀介质动态的非线性测量,通过对油气井内多相流体信息的投影扫描和反演处理,实时成像显示流体分布及流动状况,国外研制的电导法,电容法仪器采用电导探针或电容元件构成阵列测量探头,分别利用油气与水的导电特性和介电特性差异辨识井内流体,对流动截面的测量局限于个别点上,已在水平井中见到应用效果,但对物场信息投影测量的数据量和分辨率未能满足成像要求。我国提出的电磁法采用环状阵列电极构成测量探头,综合利用油气与水的导电和介电特性差异辨识井内流体,可以测量获得多相流体流动截面的清晰图像,为研究开发全新的流动成像测井系统奠定了良好基础。 相似文献
989.
Xiaoxian Zhang A. Glyn Bengough John W. Crawford Iain M. Young 《Journal of Hydrology》2002,260(1-4):75-87
The non-linear solvers in numerical solutions of water flow in variably saturated soils are prone to convergence difficulties. Many aspects can give rise to such difficulties and in this paper we address the gravity term and the prescribed-flux boundary in the Picard iteration. The problem of the gravity term in the Picard iteration is iteration-to-iteration oscillation as the gravity term is treated, by analogy with the time-step advance technique, ‘explicitly’ in the iteration. The proposed method for the gravity term is an improvement of the ‘implicit’ approach of Zhang and Ewen [Water Resour. Res. 36 (2000) 2777] by extending it to heterogeneous soil and approximating the inter-nodal hydraulic conductivity in the diffusive term and the gravity term with the same scheme. The prescribed-flux boundary in traditional methods also gives rise to iteration-to-iteration oscillation because there is no feedback to the flux in the solution at the new iteration. To reduce such oscillation, a new method is proposed to provide such a feedback to the flux. Comparison with traditional Picard and Newton iteration methods for a wide range of problems show that a combination of these two proposed methods greatly improves the stability and consequently the computational efficiency, making the use of small time step and/or under-relaxation solely for convergence unnecessary. 相似文献
990.
Predicting average annual groundwater levels from climatic variables: an empirical model 总被引:8,自引:0,他引:8
On the basis of one-dimensional theoretical water flow model, we demonstrate that the groundwater level variation follows a pattern similar to recharge fluctuation, with a time delay that depends on the characteristics of aquifer, recharge pattern as well as the distance between the recharge and observation locations. On the basis of a water budget model and the groundwater flow model, we propose an empirical model that links climatic variables to groundwater level. The empirical model is tested using a partial data set from historical records of water levels from more than 80 wells in a monitoring network for the carbonate rock aquifer, southern Manitoba, Canada. The testing results show that the predicted groundwater levels are very close to the observed ones in most cases. The overall average correlation coefficient between the predicted and observed water levels is 0.92. This proposed empirical statistical model could be used to predict variations in groundwater level in response to different climate scenarios in a climate change impact assessment. 相似文献