全文获取类型
收费全文 | 1257篇 |
免费 | 241篇 |
国内免费 | 267篇 |
专业分类
测绘学 | 25篇 |
大气科学 | 297篇 |
地球物理 | 697篇 |
地质学 | 419篇 |
海洋学 | 87篇 |
天文学 | 15篇 |
综合类 | 64篇 |
自然地理 | 161篇 |
出版年
2024年 | 3篇 |
2023年 | 14篇 |
2022年 | 24篇 |
2021年 | 37篇 |
2020年 | 31篇 |
2019年 | 37篇 |
2018年 | 31篇 |
2017年 | 44篇 |
2016年 | 41篇 |
2015年 | 48篇 |
2014年 | 71篇 |
2013年 | 92篇 |
2012年 | 83篇 |
2011年 | 70篇 |
2010年 | 70篇 |
2009年 | 72篇 |
2008年 | 85篇 |
2007年 | 88篇 |
2006年 | 77篇 |
2005年 | 74篇 |
2004年 | 82篇 |
2003年 | 55篇 |
2002年 | 58篇 |
2001年 | 44篇 |
2000年 | 52篇 |
1999年 | 43篇 |
1998年 | 60篇 |
1997年 | 31篇 |
1996年 | 34篇 |
1995年 | 28篇 |
1994年 | 35篇 |
1993年 | 27篇 |
1992年 | 27篇 |
1991年 | 16篇 |
1990年 | 18篇 |
1989年 | 9篇 |
1988年 | 12篇 |
1987年 | 8篇 |
1986年 | 9篇 |
1985年 | 5篇 |
1984年 | 4篇 |
1982年 | 3篇 |
1980年 | 4篇 |
1978年 | 6篇 |
1977年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有1765条查询结果,搜索用时 31 毫秒
131.
华东地区地震前兆短期异常研究 总被引:1,自引:0,他引:1
通过对华东地区1970年以来发生的14次5级以上地震的研究表明:无论以异常开始时间判断的异常还是以异常结束时间(或转折时间)判断的异常,其空间分布与震前地震活动的空间分布存在一定关系,并且前兆异常存在不同特征的三阶段性。以前兆的开始时间作为判断标准,异常频次反映出地震孕育的中期阶段信息。以异常的转折(或结束)时间作为异常判断标准,其异常频度具有短期信息。从而提出了异常转折率TAR,研究表明,强震前TAR超过均值的高值异常具有短期信息。通过理论分析后,提出了华东地区中期向短期过渡的综合判断方法。 相似文献
132.
THE EAST ASIAN SUBTROPICAL SUMMER MONSOON INDEX AND ITS RELATION WITH THE CLIMATE ANOMALIES IN CHINA
A new East Asian subtropical summer monsoon circulation index is defined, where the barotropic and baroclinic components of circulation are included. Results show that this index can well indicate the interannual variability of summer precipitation and temperature anomalies in China. A strong monsoon is characterized by more rainfall in the Yellow River basin and northern China, less rainfall in the Yangtze River basin, and more rainfall in south and southeast China, in association with higher temperature in most areas of China. Furthermore, comparison is made between the index proposed in this paper and other monsoon indexes in representing climate anomalies in China. 相似文献
133.
The oscillation characteristics of 1948 - 2003 South China Sea (SCS) summer monsoon intensity (SCSSMI) is analyzed by wavelet transform and the relationship between SCSSMI filtered by Lanczos filter at different time scale and oceanic thermal conditions is studied. The results show that SCSSMI exhibits dominant interannual (about 4 a), decadal (about 9 a) and interdecadal (about 38 a) oscillation periods. The interannual variation is the strongest and the interdecadal variation the weakest. The region of significant correlation between SCS summer monsoon intensity and oceanic thermodynamic variables at different time scale is greatly different. Significant correlation area of interannual variation of SCSSMI is concentrated in near equatorial region. Corresponding correlation displays quasi-biannual variability. If positive anomalies of SST and the depth of thermocline happen in eastern equatorial Indian Ocean and western equatorial Pacific, and negative anomalies of SST and the depth of thermocline happen in western equatorial Indian Ocean and eastern equatorial Pacific in previous autumn and winter, the interannual variation of SCSSMI will enhance. If the condition is contrary, interannual variation of SCSSMI will weaken. The interannual variation of SCSSMI will influence SST. The region surrounding SCS and east of Australia shows significantly negative correlation in autumn, and significantly positive correlation exhibits in west equatorial Indian Ocean, eastern equatorial Pacific and equatorial Atlantic in winter. The decadal variation of SCSSMI is modulated by PDO. Interdecadal variation of SCSSMI is relevant to the global warming and PDO. 相似文献
134.
135.
北祁连西段作为甘肃一个重要的多金属成矿带,随着地质找矿工作不断地加强,日渐重要。根据熬油沟及卡洼沟一带水系沉积物、岩屑和岩石剖面测量结果,对Au、Pt、Pd和Pb、Zn等成矿元素的分布特征和组合关系进行了分析,总结了该处成矿地质背景和地球化学异常特征,指出了找矿方向。 相似文献
136.
纳米级微粒测量是寻找隐伏矿的新方法,选取实地模拟实验和在已知隐伏矿区,利用液态捕集剂和等离子体质谱分析测试样品,进行重复测量试验,研究结果表明,不同成矿元素,在地表形成异常的运移富集速率不同,其运移速率主要取决于纳米级微粒本身的地球化学性质,地下上升气流、断裂等裂隙有利于微粒的上升运移富集;纳米级微粒地球化学重复测量时,异常可具有良好的重现性,但异常重现较常规气体缓慢,通常需要2~3个月。 相似文献
137.
138.
在实验室使用红外热像仪和接触式测温仪同步观测记录了压性和张性雁列断层失稳错动前后的热场变化过程.从实验记录中发现,在断层失稳引起温度场和热红外辐射亮温温度场上升之前,在两断层段之间的岩桥区发生降温变化.断层带开始升温发生在失稳前2~3 s内,岩桥区的降温却发生在失稳前约20s,这两个超前时间长度相差近一个量级.此类热场先降后升变化过程在雁列构造变形中有一定的普遍性,可能作为雁列断层失稳错动的热场前兆模式.根据实验观测结果,详细描述了上述热场变化的时间过程及其空间分布特征,分析了产生此种失稳前兆模式的机制,显著异常出现的条件及有利观测部位,讨论了它在地震前兆探索等研究中的意义. 相似文献
139.
在分析阿尔金区域地质和物化探异常资料的基础上,对阿尔金东段的构造特点和不同地层、岩石建造的成矿元素分布分配进行了分析和讨论,重点研究了阿尔金东段区域地球化学异常的分布规律和特点,分析和推断了引起Cu、Pb、Zn、Au、Ag等异常密集区带的地质因素,讨论了地球化学异常和区域成矿问题。认为阿尔金东段成矿潜力较大,并初步探讨了找矿方向。 相似文献
140.
Andrs Folguera Antonio Introcaso Mario Gimnez Francisco Ruiz Patricia Martinez Cynthia Tunstall Ezequiel García Morabito Víctor A. Ramos 《Tectonophysics》2007,439(1-4):129-147
The western retroarc of the Southern Andes between 38° and 40° S is formed by a NNW-elongated ridge not associated with stacked thrust sheets. On the contrary, during the last 4–3 Ma this ridge was affected by extensional deformation, regional uplift and related folding on a very broad scale. Receiver function analysis shows that the drainage divide area and adjacent retroarc lie over an attenuated crust. Expected crustal thickness at these latitudes is around 38 km, whereas in this part of the retroarc the thickness is less than 32 km. The causes for such attenuation have been linked to a moderate steepening of the subducted Nazca plate beneath the South American plate, which is suggested by a westward shift and narrowing of the magmatic arc during the last 4 to 5 Ma. Gravimetric studies show that the upper plate did not react homogeneously to slab steepening, but ancient sutures and lithospheric discontinuities deeply buried under Mesozoic to Cenozoic sequences in the retroarc were locally reactivated. These processes resulted in an asthenospheric anomaly that correlates at the surface with the area of Pliocene to Quaternary doming, widespread extension and three radial troughs. Two of the troughs have accommodated substantial amounts of extension, but the third was probably aborted at an early stage. Moreover, the presence of an anomalous concentration of calderas and large volcanic centers over the proposed asthenospheric anomaly, and their age distribution, may indicate minor migration of the asthenospheric anomaly between 4 and 2 Ma through the western South American plate. 相似文献