全文获取类型
收费全文 | 7543篇 |
免费 | 1601篇 |
国内免费 | 2290篇 |
专业分类
测绘学 | 811篇 |
大气科学 | 1589篇 |
地球物理 | 1835篇 |
地质学 | 4237篇 |
海洋学 | 1076篇 |
天文学 | 259篇 |
综合类 | 682篇 |
自然地理 | 945篇 |
出版年
2024年 | 83篇 |
2023年 | 204篇 |
2022年 | 434篇 |
2021年 | 495篇 |
2020年 | 443篇 |
2019年 | 494篇 |
2018年 | 415篇 |
2017年 | 439篇 |
2016年 | 498篇 |
2015年 | 422篇 |
2014年 | 485篇 |
2013年 | 485篇 |
2012年 | 506篇 |
2011年 | 493篇 |
2010年 | 469篇 |
2009年 | 432篇 |
2008年 | 425篇 |
2007年 | 420篇 |
2006年 | 390篇 |
2005年 | 338篇 |
2004年 | 281篇 |
2003年 | 245篇 |
2002年 | 275篇 |
2001年 | 191篇 |
2000年 | 237篇 |
1999年 | 254篇 |
1998年 | 210篇 |
1997年 | 222篇 |
1996年 | 163篇 |
1995年 | 181篇 |
1994年 | 155篇 |
1993年 | 131篇 |
1992年 | 94篇 |
1991年 | 91篇 |
1990年 | 64篇 |
1989年 | 59篇 |
1988年 | 43篇 |
1987年 | 30篇 |
1986年 | 37篇 |
1985年 | 20篇 |
1984年 | 8篇 |
1983年 | 11篇 |
1982年 | 11篇 |
1981年 | 15篇 |
1980年 | 8篇 |
1979年 | 12篇 |
1978年 | 3篇 |
1976年 | 3篇 |
1958年 | 4篇 |
1954年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
981.
982.
利用在九江-瑞昌MS5.7地震震中附近架设的丁家山台(DJS)、狮子洞台(SZD)和武蛟台(WUJ)的地震波形资料,采用S波分裂系统分析方法,对余震进行了S波分裂分析。结果表明,震中距较小、台站附近断层分布复杂的丁家山台(DJS)的慢波时间延迟相对较大,快波偏振方向不太集中。台站附近断裂分布单一的武蛟台(WUJ)快波偏振优势方向与断裂走向角度相差约35°,与区域主压应力方向也不一致。台站附近无断层通过的狮子洞台(SZD)快波偏振优势方向接近区域主压应力方向。慢波时间延迟大小与震源深度没有明显的规律性关系。 相似文献
983.
仪器在较大波动幅度的影响下产生自动调零(电磁阀门开启),与地震信息混在一起,难以直接使用原始数据。合理消除自动调零带来的影响,还原真实情况,成为台站必须解决的问题。采用确定校正值的方法,力图还原为连续记录,结果发现:处理后的资料可以和另外一台没有调零动作的体积应变仪器的原始资料相符合。 相似文献
984.
Wang Jianglin Yang Bao Zheng Jingyun Zhang Xuezhen Wang Zhiyuan Fang Miao Shi Feng Liu Jingjing 《中国科学:地球科学(英文版)》2020,63(8):1126-1143
The temperature variability over multidecadal and longer timescales(e.g., the cold epochs in the late 15 th, 17 th, and early 19 th centuries) is significant and dominant in the millennium-long, large-scale reconstructions and model simulations;however, their temporal patterns in the reconstructed and simulated temperature series are not well understood and require a detailed assessment and comparison. Here, we compare the reconstructed and simulated temperature series for the Northern Hemisphere(NH) at multidecadal and longer-term timescales(30 years) by evaluating their covariance, climate sensitivity and amplitude of temperature changes. We found that covariances between different reconstructions or between reconstructions and simulations are generally high for the whole period of 850–1999 CE, due to their similar long-term temporal patterns. However,covariances between different reconstructions or between reconstructions and simulations steadily decline as time series extends further back in time, becoming particularly small during Medieval times. This is related to the large uncetainties in the reconstructions caused by the decreased number of proxy records and sample duplication during the pre-instrumental periods.Reconstructions based solely on tree-ring data show higher skill than multiproxy reconstructions in capturing the amplitude of volcanic cooling simulated by models. Meanwhile, climate models have a shorter recovery(i.e., lag) in response to the cooling caused by volcanic eruptions and solar activity minima, implying the lack of some important feedback mechanisms between external forcing and internal climate processes in climate models. Amplitudes of temperature variations in the latest published tree-ring reconstructions are comparable to those of the multiproxy reconstructions. We found that the temperature difference between the Medieval Climate Anomaly(950–1250 CE) and the Little Ice Age(1450–1850 CE) is generally larger in proxybased reconstructions than in model simulations, but the reason is unclear. 相似文献
985.
A photostrictive type of opto-electromechanical actuator activated by high-energy lights can introduce actuation and control effects without hard-wired connections.This paper addresses the controllability aspect in wireless vibration control of plate structures via photostrictive actuators.A modal force index,which has taken into account the mode number,the spatial distribution,and the dimension of the actuator,is chosen as an objective function to determine the optimal locations of photostrictive actuators.A linear methodology is proposed in this paper and the vibration equation is written in the standard state-space form.A binary-coded GA based combined optimal placement and LQR(linear quadratic regulator) control scheme has been incorporated,which maximizes the modal force index,the closed loop damping and minimizes input light intensity to the actuators.In the present method only three weighting factors have been used to search optimal Q and R matrices using GA,which reduces chromosome length and hence minimizes computational time.Numerical results demonstrate that the use of strategically positioned actuator patches can effectively control the fundamental modes that dominate the structural vibration. 相似文献
986.
Numerical evaluation of the effect of fracture network connectivity in naturally fractured shale based on FSD model 总被引:1,自引:0,他引:1
In this paper, the effect of pre-existing discrete fracture network (DFN) connectivity on hydraulic fracturing is numerically investigated in a rock mass subjected to in-situ stress. The simulation results show that DFN connectivity has a significant influence on the hydraulic fracture (HF) & DFN interaction and hydraulic fracturing effectiveness, which can be characterized by the total interaction area, stimulated DFN length, stimulated HF length, leak-off ratio, and stimulated total length. In addition, even at the same fluid injection rate, simulation models exhibit different responses that are strongly affected by the DFN connectivity. At a low injection rate, total interaction area decreases with increasing DFN connectivity; at a high injection rate, total interaction area increases with the increase of DFN connectivity. However, for any injection rate, the stimulated DFN length increases and stimulated HF length decreases with the increase of connectivity. Generally, this work shows that the DFN connectivity plays a crucial role in the interaction between hydraulic fractures, the pre-existing natural fractures and hydraulic fracturing effectiveness; in return, these three factors affect treating pressure, created microseismicity and corresponding stimulated volume. This work strongly relates to the production technology and the evaluation of hydraulic fracturing effectiveness. It is helpful for the optimization of hydraulic fracturing simulations in naturally fractured formations. 相似文献
987.
Metamorphic core complex(MCC) is characterized by the exhumation of lower crust over a large-scale detachment fault, providing natural records for tectonic extension. MCCs are widely identified in the North China Craton(NCC), which have been intensively studied on their structural and geological characteristics. Yet, the condition for the formation of MCCs and their link with NCC destruction are still in debate. In this study, we perform numerical simulations to investigate MCC formation under extension, with a focus on the effect of crustal rheologies. Results indicate that three end-member modes of deformation may occur: the metamorphic core complex mode, the detachment fault-uplifting mode and the pure shear mode. Weaker lower crust and stronger upper crust may promote the formation of MCC. In contrast, stronger lower crust(1.3×1021 Pa s) may prohibit the exhumation of lower crust(detachment fault-uplifting mode), while weaker upper crust(7.8×1021 Pa s) may fail to develop detachment faults(pure shear mode). Given that cratons typically have a strong crust, we suggest that the lower crust of NCC was weakened prior to extension, which promoted the formation of MCC in a later stage under the back-arc extension. 相似文献
988.
WeiGuo Liu Hong Yang HuanYe Wang Yuan Yao Zheng Wang YunNing Cao 《中国科学:地球科学(英文版)》2016,59(7):1368-1377
The hydrogen isotopic composition(δD) of leaf wax long-chain n-alkanes(C27, C29, and C31) from lacustrine sediments has been widely applied to reconstruct terrestrial paleoclimatic and paleohydrological changes. However, few studies have addressed whether the aquatic-derived n-alkanes can affect the δD values of lake sedimentary long-chain n-alkanes, which are usually regarded as a recorder of the terrestrial hydrological signals. Here we systematically investigated δD values of long-chain n-alkanes from modern aquatic plants, both near-shore and off-shore surface sediments, surrounding terrestrial plant litters, as well as river water and lake water in Lake Qinghai and its satellite lakes on the northeastern Qinghai-Tibet Plateau. Our data showed that(i) δD values of long-chain n-alkanes from aquatic plants varied from-184‰ to-132‰ for n-C27, from-183‰ to-138‰ for n-C29, and from-189‰ to-130‰ for n-C31, respectively, with no significant differences among the three n-alkanes homologues;(ii) δD values of long-chain n-alkanes from aquatic plants were generally more positive than those from surrounding terrestrial plants, possibly because that they recorded the D-enrichment of lake water in this semi-arid region;(iii) δD values of long-chain n-alkanes from surface sediments showed significant differences among the three n-alkanes homologues, due to the larger aquatic input of n-C27 to the sedimentary lipid pool than that of n-C31, and(iv) n-C27 δD values of near-shore aquatic plants and near-shore sediments are more negative than those from off-shore as a result of lower δD values of near-shore lake water. Our findings indicate that in this region(i) the offset between sedimentary n-C27 and n-C31 δD values(ΔδDC27-C31) could potentially be used to evaluate if sedimentary long-chain n-alkanes are derived from a single source;(ii) while δD values of n-C27 may be influenced by lake water hydrological changes, sedimentary n-C31 is derived predominantly from terrestrial plants and thus its δD can serve as a relatively reliable indicator for terrestrial paleoclimatic and paleohydrological reconstructions. 相似文献
989.
The estimation of the quality factor Q plays a fundamental role in enhancing seismic resolution via absorption compensation in the near-surface layer. We present a new geometry that can be used to acquire field data by combining surface and cross-hole surveys to decrease the effect of geophone coupling on Q estimation. In this study, we drilled number of receiver holes around the source hole, each hole has different depth and each geophone is placed geophones into the bottom of each receiver hole to avoid the effect of geophone coupling with the borehole wall on Q estimation in conventional cross-hole seismic surveys. We also propose a novel tomographic inversion of the Q factor without the effect of the source signature, and examine its stability and reliability using synthetic data. We estimate the Q factors of the near-surface layer in two different frequency bands using field data acquired in the Dagang Oilfield. The results show that seismic absorption in the near-surface layer is much greater than that in the subsurface strata. Thus, it is of critical practical importance to enhance the seismic solution by compensating for near-surface absorption. In addition, we derive different Q factors from two frequency bands, which can be treated, to some extent, as evidence of a frequency-dependent Q. 相似文献
990.
我国是一个地质灾害多发的国家,特别是滑坡发生的次数比较多、危害性比较大。因此对滑坡的位移进行监控预测有着十分重要的意义。对于滑坡位移变化的非线性问题,可以利用支持向量机在回归分析中的方法——ε-支持向量回归机(ε-SVR)进行预测,该方法基于统计学理论,在处理小样本、非线性、高维数等问题上有一定的优势。以福建八尺门滑坡的监测数据为例,将前面的17个位移数据作为学习样本,后面的6个位移数据作为预测样本,采用不同的核函数分别进行位移预测来与原始监测值进行对比,比较其预测精度。结果显示,该方法产生的预测值与原始监测值之间的误差比较小,其位移变化趋势与原始数据的变化趋势也基本一致,这说明该方法预测精度高,实用性强。 相似文献