全文获取类型
收费全文 | 545篇 |
免费 | 110篇 |
国内免费 | 156篇 |
专业分类
测绘学 | 37篇 |
大气科学 | 58篇 |
地球物理 | 189篇 |
地质学 | 307篇 |
海洋学 | 34篇 |
天文学 | 5篇 |
综合类 | 95篇 |
自然地理 | 86篇 |
出版年
2024年 | 3篇 |
2023年 | 6篇 |
2022年 | 22篇 |
2021年 | 18篇 |
2020年 | 23篇 |
2019年 | 41篇 |
2018年 | 22篇 |
2017年 | 22篇 |
2016年 | 22篇 |
2015年 | 35篇 |
2014年 | 33篇 |
2013年 | 31篇 |
2012年 | 32篇 |
2011年 | 25篇 |
2010年 | 33篇 |
2009年 | 30篇 |
2008年 | 31篇 |
2007年 | 40篇 |
2006年 | 45篇 |
2005年 | 31篇 |
2004年 | 29篇 |
2003年 | 30篇 |
2002年 | 22篇 |
2001年 | 19篇 |
2000年 | 18篇 |
1999年 | 16篇 |
1998年 | 14篇 |
1997年 | 16篇 |
1996年 | 11篇 |
1995年 | 19篇 |
1994年 | 10篇 |
1993年 | 20篇 |
1992年 | 10篇 |
1991年 | 7篇 |
1990年 | 1篇 |
1989年 | 8篇 |
1988年 | 9篇 |
1987年 | 4篇 |
1986年 | 3篇 |
排序方式: 共有811条查询结果,搜索用时 15 毫秒
71.
贩卖毒品是实现毒品犯罪经济利益的重要环节,是危害最为严重的毒品犯罪类型之一。现有研究主要关注毒品犯罪与建成环境之间的关系,没有顾及打击后贩卖毒品犯罪空间转移现象以及影响因素的变化。本文基于日常活动理论、犯罪模式理论和社会解组理论,以中国ZG市主城区为例,融合多源时空数据,分别对2013年8月开始的“雷霆扫毒”前后的贩卖毒品犯罪构建负二项回归模型,分析微观尺度下半公共空间、室外公共空间和室内私人空间对贩卖毒品犯罪影响的变化。研究发现“雷霆扫毒”行动后:① 贩卖毒品犯罪案件数量显著下降;② 半公共空间对贩卖毒品犯罪的影响作用减弱;③ 室外公共空间对贩卖毒品犯罪影响作用增强,室内私人空间对贩卖毒品犯罪的影响上升。结果表明:“雷霆扫毒”专项行动开展后一年,贩卖毒品犯罪的“主阵地”发生变化,由城市半公共空间逐渐向室外公共空间和室内私人空间转移。特别的是,“雷霆扫毒”对大毒枭及贩毒团伙的打击成效突出,促使2014年贩毒案件大幅度下降,实现了专项行动开展的目的。后续一系列专项行动进一步提升了对贩卖毒品犯罪的发现和查处能力,显示出专项行动对打击隐性犯罪的明显效果。研究表明公安执法部门必须对毒品贩卖犯罪进行持续的、有针对性的打击,对发生地的变动进行定期的监控,不能一蹴而就。 相似文献
72.
73.
74.
针对2011年日本东北大地震(Tohoku-Oki地震)发生前后较短时间内的多次较大前震和余震和主震混在一起,不利于提取出主震同震信号的问题,该文利用弹性位错理论模拟计算了Tohoku-Oki地震一次较大前震和两次较大余震的同震重力变化,讨论了这3次地震单独和综合的重力效应,并与主震重力变化对比分析,认为这3次前震和余震引起的重力变化数值较大,影响范围广,会直接影响到Tohoku-Oki地震主震的同震重力信号提取,所以需要作为重要误差考虑。 相似文献
75.
Churyumov Klim I. Luk'yanyk Igor V. Berezhnoi Alexei A. Chavushyan Vahram H. Sandoval Lourdes S. Palma Alejandro A. 《Earth, Moon, and Planets》2002,90(1-4):361-368
We present a preliminary analysis of medium resolution optical spectra of comet C/2000 WM1 (LINEAR) obtained on 22 November
2001. Theemission lines of the molecules C2, C3, CN, NH2,H2O+ and presumably CO (Asundi and triplet bands) and C2
-were identified in these spectra. By analysing the brightnessdistributions of the C2, C3, CN emission lines along theslit of the spectrograph we determined some physical parameters of theseneutrals, such as their
lifetimes and expansion velocities inthe coma. The Franck–Condon factors for the CO Asundi bands and C2
- bands were calculated using a Morse potential model. 相似文献
76.
位错模式反演的算法研究 总被引:1,自引:0,他引:1
综述了大地测量反演算法的发展状况,详细介绍了模拟退火,随机耗费和区间算法等3种优化方法,并基于位错模式,采用模拟的重力测量观测数据,比较了3种算法的反演效果,结果表明:模拟退火法优于随机耗费法,而区间算法的可靠性又优于模拟退火法,区间算法是最可靠的反演方法。 相似文献
77.
论多种数据联合反演的模式及算法 总被引:9,自引:3,他引:6
针对日益丰富的数据资料,综述了大地测量反演的发展进程,论述了多种数据联合反演的意义和必要性,给出了兼顾权比确定的大地测量、地震和地质三类数据的联合反演模式及采用水准测量、GPS和重力三种数据联合反演断层参数的具体公式,特别介绍了求解优化问题所有全局最优解的区间算法,并给出了基本算例,结果体现了区间算法无可比拟的优越性及其在大地测量反演领域中的应用前景。 相似文献
78.
79.
80.
Peitao Wang Zhiyuan Ren Lining Sun Jingming Hou Zongchen Wang Ye Yuan Fujiang Yu 《海洋学报(英文版)》2021,40(11):11-30
The systematic discrepancies in both tsunami arrival time and leading negative phase (LNP) were identified for the recent transoceanic tsunami on 16 September 2015 in Illapel, Chile by examining the wave characteristics from the tsunami records at 21 Deep-ocean Assessment and Reporting of Tsunami (DART) sites and 29 coastal tide gauge stations. The results revealed systematic travel time delay of as much as 22 min (approximately 1.7% of the total travel time) relative to the simulated long waves from the 2015 Chilean tsunami. The delay discrepancy was found to increase with travel time. It was difficult to identify the LNP from the near-shore observation system due to the strong background noise, but the initial negative phase feature became more obvious as the tsunami propagated away from the source area in the deep ocean. We determined that the LNP for the Chilean tsunami had an average duration of 33 min, which was close to the dominant period of the tsunami source. Most of the amplitude ratios to the first elevation phase were approximately 40%, with the largest equivalent to the first positive phase amplitude. We performed numerical analyses by applying the corrected long wave model, which accounted for the effects of seawater density stratification due to compressibility, self-attraction and loading (SAL) of the earth, and wave dispersion compared with observed tsunami waveforms. We attempted to accurately calculate the arrival time and LNP, and to understand how much of a role the physical mechanism played in the discrepancies for the moderate transoceanic tsunami event. The mainly focus of the study is to quantitatively evaluate the contribution of each secondary physical effect to the systematic discrepancies using the corrected shallow water model. Taking all of these effects into consideration, our results demonstrated good agreement between the observed and simulated waveforms. We can conclude that the corrected shallow water model can reduce the tsunami propagation speed and reproduce the LNP, which is observed for tsunamis that have propagated over long distances frequently. The travel time delay between the observed and corrected simulated waveforms is reduced to <8 min and the amplitude discrepancy between them was also markedly diminished. The incorporated effects amounted to approximately 78% of the travel time delay correction, with seawater density stratification, SAL, and Boussinesq dispersion contributing approximately 39%, 21%, and 18%, respectively. The simulated results showed that the elastic loading and Boussinesq dispersion not only affected travel time but also changed the simulated waveforms for this event. In contrast, the seawater stratification only reduced the tsunami speed, whereas the earth's elasticity loading was responsible for LNP due to the depression of the seafloor surrounding additional tsunami loading at far-field stations. This study revealed that the traditional shallow water model has inherent defects in estimating tsunami arrival, and the leading negative phase of a tsunami is a typical recognizable feature of a moderately strong transoceanic tsunami. These results also support previous theory and can help to explain the observed discrepancies. 相似文献