全文获取类型
收费全文 | 5881篇 |
免费 | 1207篇 |
国内免费 | 1708篇 |
专业分类
测绘学 | 436篇 |
大气科学 | 1385篇 |
地球物理 | 1464篇 |
地质学 | 3190篇 |
海洋学 | 622篇 |
天文学 | 277篇 |
综合类 | 720篇 |
自然地理 | 702篇 |
出版年
2024年 | 30篇 |
2023年 | 119篇 |
2022年 | 272篇 |
2021年 | 345篇 |
2020年 | 268篇 |
2019年 | 277篇 |
2018年 | 392篇 |
2017年 | 323篇 |
2016年 | 370篇 |
2015年 | 335篇 |
2014年 | 354篇 |
2013年 | 369篇 |
2012年 | 313篇 |
2011年 | 330篇 |
2010年 | 397篇 |
2009年 | 347篇 |
2008年 | 316篇 |
2007年 | 330篇 |
2006年 | 247篇 |
2005年 | 239篇 |
2004年 | 189篇 |
2003年 | 172篇 |
2002年 | 151篇 |
2001年 | 181篇 |
2000年 | 193篇 |
1999年 | 255篇 |
1998年 | 249篇 |
1997年 | 235篇 |
1996年 | 209篇 |
1995年 | 157篇 |
1994年 | 152篇 |
1993年 | 144篇 |
1992年 | 113篇 |
1991年 | 85篇 |
1990年 | 62篇 |
1989年 | 65篇 |
1988年 | 59篇 |
1987年 | 31篇 |
1986年 | 32篇 |
1985年 | 18篇 |
1984年 | 14篇 |
1983年 | 14篇 |
1982年 | 9篇 |
1981年 | 9篇 |
1980年 | 4篇 |
1979年 | 4篇 |
1975年 | 5篇 |
1960年 | 2篇 |
1959年 | 1篇 |
1958年 | 7篇 |
排序方式: 共有8796条查询结果,搜索用时 21 毫秒
121.
The regional stress field and seismic dynamics along the border zone between Fujian, Guangdong and Jiangxi Provinces are studied based on the seismo-geological data, GPS measurement, and seismicity. The results show that: (1) the principal compressional stress of the stress field is oriented in NW-SE direction and the principal extensional stress is in NE-SW direction; (2) the WNW-ward compression and collision of the Philippine Sea Plate to the eastern coast of Taiwan Island are the most direct and most important dynamic source for preparation and occurrence of strong earthquakes in the Taiwan area and along the border zone between Fujian, Guangdong and Jiangxi Provinces. 相似文献
122.
辽河盆地东部凹陷热历史及构造—热演化特征 总被引:9,自引:5,他引:9
根据辽河盆地东部凹陷大地热流测量和镜质体反射率数据,恢复了该区的热历史,结果表明:东部凹陷热流呈现古热流高现今热流低的变化特征,沙河街组三段沉积期到东营组沉积期(距今43~25Ma)盆地热流为66~82mWm2,现今热流值为47~70mWm2。构造沉降史分析显示,盆地经历了早期的裂谷阶段(距今43~25Ma)和后期的热沉降阶段,裂谷阶段包含了两个裂谷亚旋回。盆地现今较低的大地热流和较高的古热流及典型的裂谷型构造沉降样式为东部凹陷的构造—热演化提供了重要认识。 相似文献
123.
GIS支持下珠江三角洲城镇建筑覆盖变化遥感监测分析 总被引:15,自引:0,他引:15
从珠江三角洲区域总体出发,探讨大范围城镇建筑覆盖变化的遥感监测方法。分析了城镇建筑覆盖变化专题信息提取方法概况,比较了最大似然法、上下文分类法、人工神经网络三种分类方法的优缺点。借助GIS技术的术持,在计算机自动分类的基础上利用专家知识改进了分类结果。根据遥感监测结果,对1988—1998年间珠江三角洲城镇建筑覆盖变化特征进行了分析。 相似文献
124.
基于GPS基准站网的GPS测量 总被引:5,自引:0,他引:5
采用基于GPS基准网的GPS测量可以提高GPS测量的可靠性和准确性 ,可以消除和减小GPS测量观测值中与时间和空间相关的大气误差和轨道误差的影响 ,使中、长距离快速静态定位和RTK动态定位成为现实 ,还具有可直接得到WGS84Z坐标等优点。本文介绍基于GPS基准站网的GPS测量 ,简要地论述GPS虚拟参考站法VRS和区域改正数法FKP的原理、方法和特点 ,以及目前实施中存在的一些问题 相似文献
125.
126.
127.
128.
Despite growing evidence for environmental oscillations during the last glacial–interglacial transition from high latitude, terrestrial sites of the North Pacific rim, oxygen-isotopic records of these oscillations remain sparse. The lack of data is due partially to the paucity of lakes that contain carbonate sediment suitable for oxygen-isotopic analysis. We report here the first record of oxygen-isotopic composition in diatom silica (δ18OSi) from a lake in that region. δ18OSi increases gradually from 19.0 to 23.5‰ between 12,340 and 11,000 14C yr B.P., reflecting marked climatic warming at the end of the last glaciation. Around 11,000 14C yr B.P., δ18OSi decreases by 1.7‰, suggesting a temperature decrease of 3.5–8.9 °C at the onset of the Younger Dryas (YD) in southwestern Alaska. Climatic recovery began ca. 10,740 14C yr B.P., as inferred from the increase of δ18OSi to a maximum of 23.9‰ near the end of the YD. Our data reveal that a YD climatic reversal in southwestern coastal areas of Alaska occurred, but the YD climate did not return to full-glacial conditions. 相似文献
129.
Lipid distribution in a subtropical southern China stalagmite as a record of soil ecosystem response to paleoclimate change 总被引:3,自引:0,他引:3
Shucheng Xie Yi Yi Junhua Huang Chaoyong Hu Yanjun Cai Matthew Collins Andy Baker 《Quaternary Research》2003,60(3):340-347
Lipid extracts from a 61.7-cm-long subtropical stalagmite in southern China, spanning the period of ca. 10,000–21,000 yr ago as constrained by U–Th dating, were analyzed using gas chromatography–mass spectrometry. The higher plants and microorganisms in the overlying soils contribute a proportion of n-alkanes identified in the stalagmite. The occurrence of LMW (lower molecular weight) n-alkanols and n-alkan-2-ones in the stalagmite was mainly related to the soil microorganisms. We suggest that HMW (higher molecular weight) n-alkanols and n-alkan-2-ones identified in the stalagmite originate from soil organics and reflect input from contemporary vegetation. Shifts in the ratio of LMW to HMW n-alkanols or n-alkan-2-ones indicative of the variation of soil ecosystems (e.g., microbial degradation of organic matter and/or the relative abundance of soil microorganisms to higher plants) are comparable with the subtropical alkenone-SST (sea surface temperature) record of the same period. The similar trends seen in the δ13C data and the lipid parameters in this stalagmite imply that the overlying soil ecosystem response to climate might be responsible for the variation of δ13C values. 相似文献
130.
The influence of NaCl, CaCl2, and dissolved minerals on the oxygen isotope fractionation in mineral-water systems at high pressure and high temperature was studied experimentally. The salt effects of NaCl (up to 37 molal) and 5-molal CaCl2 on the oxygen isotope fractionation between quartz and water and between calcite and water were measured at 5 and 15 kbar at temperatures from 300 to 750°C. CaCl2 has a larger influence than NaCl on the isotopic fractionation between quartz and water. Although NaCl systematically changes the isotopic fractionation between quartz and water, it has no influence on the isotopic fractionation between calcite and water. This difference in the apparent oxygen isotope salt effects of NaCl must relate to the use of different minerals as reference phases. The term oxygen isotope salt effect is expanded here to encompass the effects of dissolved minerals on the fractionations between minerals and aqueous fluids. The oxygen isotope salt effects of dissolved quartz, calcite, and phlogopite at 15 kbar and 750°C were measured in the three-phase systems quartz-calcite-water and phlogopite-calcite-water. Under these conditions, the oxygen isotope salt effects of the three dissolved minerals range from ∼0.7 to 2.1‰. In both three-phase hydrothermal systems, the equilibrium fractionation factors between the pairs of minerals are the same as those obtained by anhydrous direct exchange between each pair of minerals, proving that the use of carbonate as exchange medium provides correct isotopic fractionations for a mineral pair.When the oxygen isotope salt effects of two minerals are different, the use of water as an indirect exchange medium will give erroneous fractionations between the two minerals. The isotope salt effect of a dissolved mineral is also the main reason for the observation that the experimentally calibrated oxygen isotope fractionations between a mineral and water are systematically 1.5 to 2‰ more positive than the results of theoretical calculations. Dissolved minerals greatly affect the isotopic fractionation in mineral-water systems at high pressure and high temperature. If the presence of a solute changes the solubility of a mineral, the real oxygen isotope salt effect of the solute at high pressure and high temperature cannot be correctly derived by using the mineral as reference phase. 相似文献