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871.
滇东岩溶区表层岩溶水源地特征及其开发利用 总被引:1,自引:0,他引:1
表层岩溶水源地是解决分散农村生活用水困难的重要水源,而且分布广泛,水质较好。但水源地含水介质的富水性不均匀,岩溶水动态变幅大,脆弱性突出,易受污染和生态环境变化的影响。由此,表层岩溶水源地生态环境建设及保护尤为重要。表层泉以池、管调蓄系统开发最为有效。表层富水块段适宜打浅井开发,建设庭院式供水工程。采用地质雷达验证地质认识,确定井位,是经济有效的技术手段。 相似文献
872.
达金海相碎屑岩出露于西藏冈仁波齐峰山脚下,长期以来,该套岩石与冈底斯砾岩一起被视为印度-亚洲板块碰撞形成的陆相磨拉石.该套岩石组合是由凝灰质粉砂岩、杂砂岩、含砾杂砂岩和砾岩组成的一套深海-浅海相沉积组合.杂砂岩、砾岩碎屑组成与地球化学组成研究表明,该套岩石组合的形成与岛弧的发展密切相关,源区大地构造背景以岛弧为主,但也存在被动大陆边缘和碰撞构造带(蛇绿混杂带)两个不同构造背景的源区.区域上,在该套岩石组合的北侧存在着冈底斯岛弧带,南侧为雅鲁藏布蛇绿混杂带.这些特征共同表明,达金海相碎屑岩是西藏雅鲁藏布缝合带与冈底斯岛弧带之间的日喀则弧前盆地的一部分. 相似文献
873.
874.
European geodetic very long baseline interferometry (VLBI) sessions (also known as EUROPE sessions) have been carried out
on a regular basis for the past 15 years to study relative crustal motions within Europe. These sessions are based on observations
of extragalactic radio sources, which serve as distant fiducial marks to establish an accurate and stable celestial reference
frame for long-term geodetic measurements. The radio sources, however, are not always point-like on milliarcsecond scales,
as VLBI imaging has revealed. In this work, we quantify the magnitude of the expected effect of intrinsic source structure
on geodetic bandwidth synthesis delay VLBI measurements for a subset of 14 sources regularly observed during the EUROPE sessions.
These sources have been imaged at both X-band (8.4 GHz) and S-band (2.3 GHz) based on dedicated observations acquired with
the European VLBI Network (EVN) in November 1996. The results of this calculation indicate that the reference source 0457+024
causes significant structural effects in measurements obtained on European VLBI baselines (about 10 picoseconds on average),
whereas most of the other sources produce effects that are only occasionally larger than a few picoseconds. Applying the derived
source structure models to the data of the EUROPE5-96 session carried out at the same epoch as the EVN experiment shows no
noticeable changes in the estimated VLBI station locations. 相似文献
875.
876.
应用改进的主地震相对定位法对17年伽师强震群3级以上地震进行了精确定位,根据较强地震的空间分布和震源机制解推断出伽师震群的发震构造为北北西向的雁行断裂.根据伽师震群地震的2177个P波初动方向记录,计算了伽师震群的平均震源机制解.基于Silver的震源模型,由震源谱推断了伽师震群主要地震的破裂方向,破裂尺度及应力降.文中最后用右阶雁行断裂的数值模型计算了伽师震群的发震构造所产生的扰动应力场的空间分布图像,用其解释了序列地震震源机制的多样性和低应力降现象,并认为特定的雁行发震构造与强震的多发性有关. 相似文献
877.
878.
Weidong Guo Chao Wang Yan Li Liyin Qu Muchen Lang Yongbin Deng Qinglong Liang 《地球科学进展》1986,35(9):933-947
Since 1990s, spectral analysis has become an important technique to characterize the properties of chromophoric and fluorescent dissolved organic matter (CDOM and FDOM) from various aquatic systems and a series of spectral indices have been suggested to trace the sources of DOM and their biogeochemical regulation processes. DOM samples were collected from an aquatic continuum from watershed to deep ocean, i.e. Zhangjiang River and Estuary, Dongshan Bay, Taiwan Strait, Northeast basin of the South China Sea, Luzon Strait and the vertical profile of the Kuroshio region of the West Pacific Ocean. This continuum covered many critical interfaces (land-ocean, shelf-basin, marginal sea basin-open ocean and euphotic and aphotic layer). The spatial distribution and variation of various qualitative and quantitative parameters along the continuum were clearly revealed. Combined with literature review, the sources and sinks of CDOM/FDOM and their inherent regulation processes under significant hydrological and biogeochemical gradient variation were systematically summarized. The geochemical differentiation of the quantitative DOM spectral index in various aquatic systems was discussed. The tracing ability of the qualitative DOM spectral index was commented. The coupling study of soil-river organic matter systems, mechanism of mineralization-related microbial production of CDOM/FDOM, quantified geochemical framework concept and perturbation of global change on CDOM/FDOM dynamics were suggested as future key topics. 相似文献
879.
The Upper Cretaceous Mukalla coals and other organic-rich sediments which are widely exposed in the Jiza-Qamar Basin and believed to be a major source rocks, were analysed using organic geochemistry and petrology. The total organic carbon (TOC) contents of the Mukalla source rocks range from 0.72 to 79.90% with an average TOC value of 21.50%. The coals and coaly shale sediments are relatively higher in organic richness, consistent with source rocks generative potential. The samples analysed have vitrinite reflectance in the range of 0.84–1.10 %Ro and pyrolysis Tmax in the range of 432–454 °C indicate that the Mukalla source rocks contain mature to late mature organic matter. Good oil-generating potential is anticipated from the coals and coaly shale sediments with high hydrogen indices (250–449 mg HC/g TOC). This is supported by their significant amounts of oil-liptinite macerals are present in these coals and coaly shale sediments and Py-GC (S2) pyrograms with n-alkane/alkene doublets extending beyond nC30. The shales are dominated by Type III kerogen (HI < 200 mg HC/g TOC), and are thus considered to be gas-prone.One-dimensional basin modelling was performed to analysis the hydrocarbon generation and expulsion history of the Mukalla source rocks in the Jiza-Qamar Basin based on the reconstruction of the burial/thermal maturity histories in order to improve our understanding of the of hydrocarbon generation potential of the Mukalla source rocks. Calibration of the model with measured vitrinite reflectance (Ro) and borehole temperature data indicates that the present-day heat flow in the Jiza-Qamar Basin varies from 45.0 mW/m2 to 70.0 mW/m2 and the paleo-heat flow increased from 80 Ma to 25 Ma, reached a peak heat-flow values of approximately 70.0 mW/m2 at 25 Ma and then decreased exponentially from 25 Ma to present-day. The peak paleo-heat flow is explained by the Gulf of Aden and Red Sea Tertiary rifting during Oligocene-Middle Miocene, which has a considerable influence on the thermal maturity of the Mukalla source rocks. The source rocks of the Mukalla Formation are presently in a stage of oil and condensate generation with maturity from 0.50% to 1.10% Ro. Oil generation (0.5% Ro) in the Mukalla source rocks began from about 61 Ma to 54 Ma and the peak hydrocarbon generation (1.0% Ro) occurred approximately from 25 Ma to 20 Ma. The modelled hydrocarbon expulsion evolution suggested that the timing of hydrocarbon expulsion from the Mukalla source rocks began from 15 Ma to present-day. 相似文献
880.
热带印度洋与全球大气相互作用的信息传输特征分析 总被引:2,自引:0,他引:2
基于气象场信息源汇概念和定义方法, 使用海表温度(SST)和位势高度场(GH)资料计算热带印度洋和全球大气相互作用过程中的信息传递, 给出了热带印度洋(20°S~20°N, 50°E~100°E)与热带地区、北半球和南半球大气之间的信息传递的区域分布特征, 并分析热带印度洋与大气相互作用中信息传递特征的季节差异和年代际变化。研究结果表明, 热带印度洋信息源主要分布在(10°S~10°N, 60°E~90°E)的区域内, 北半球和南半球大气信息汇均呈现显著的带状分布, 且主要分布在中纬度地区, 而热带地区的大气信息汇则主要分布于热带中东太平洋上空。热带印度洋对处在冬半年的半球的影响更强, 不同季节下热带印度洋与大气相互作用中的信息源汇证实了这一可能性。同时, 热带印度洋与大气之间的信息传递特征在20世纪70年代末期的年代际气候转型前后南北半球的变化不太一致:北半球大气对热带印度洋的响应存在不同程度的减弱, 南半球则存在不同程度的增强。 相似文献