全文获取类型
收费全文 | 12378篇 |
免费 | 2447篇 |
国内免费 | 3304篇 |
专业分类
测绘学 | 1039篇 |
大气科学 | 2392篇 |
地球物理 | 3239篇 |
地质学 | 6505篇 |
海洋学 | 1678篇 |
天文学 | 493篇 |
综合类 | 1190篇 |
自然地理 | 1593篇 |
出版年
2024年 | 88篇 |
2023年 | 284篇 |
2022年 | 641篇 |
2021年 | 761篇 |
2020年 | 590篇 |
2019年 | 711篇 |
2018年 | 748篇 |
2017年 | 741篇 |
2016年 | 785篇 |
2015年 | 676篇 |
2014年 | 824篇 |
2013年 | 796篇 |
2012年 | 853篇 |
2011年 | 860篇 |
2010年 | 902篇 |
2009年 | 807篇 |
2008年 | 738篇 |
2007年 | 675篇 |
2006年 | 539篇 |
2005年 | 471篇 |
2004年 | 392篇 |
2003年 | 336篇 |
2002年 | 335篇 |
2001年 | 360篇 |
2000年 | 337篇 |
1999年 | 461篇 |
1998年 | 333篇 |
1997年 | 339篇 |
1996年 | 279篇 |
1995年 | 275篇 |
1994年 | 223篇 |
1993年 | 231篇 |
1992年 | 154篇 |
1991年 | 106篇 |
1990年 | 66篇 |
1989年 | 92篇 |
1988年 | 82篇 |
1987年 | 45篇 |
1986年 | 32篇 |
1985年 | 24篇 |
1984年 | 24篇 |
1983年 | 14篇 |
1982年 | 23篇 |
1981年 | 15篇 |
1980年 | 23篇 |
1979年 | 7篇 |
1978年 | 4篇 |
1976年 | 3篇 |
1958年 | 12篇 |
1954年 | 4篇 |
排序方式: 共有10000条查询结果,搜索用时 0 毫秒
841.
中国海城-大石桥菱镁矿矿床举世闻名,矿床分布于辽东元古宙裂谷海槽北缘的次一级盒地中。含镁建造属元古宙上辽河群大石桥岩组的上部.按含矿建造组成岩石的各种成因标志,确定建造的沉积岩相为闭塞台地相,因此.推测它形成于裂谷边缘的泻湖环境。由于长期潮汐作用,泻湖内有充分的富镁海水周期性地供给,在当时炎热干旱的气候条件下,泻湖中的卤水不断浓缩,并通过化学与生物化学成矿作用,在泻湖盆地内形成了大型-超大型的菱镁矿矿床。元古宙末期矿床遭受了绿片岩-角闪岩相区域动力热流变质作用的改造。 相似文献
842.
准噶尔盆地第三纪磁性地层柱的建立 总被引:2,自引:2,他引:2
通过对新疆准噶尔盆地第三系3个剖面古地磁样品的分析、测试,在生物地层学研究的基础上,建立了一条较为完整的第三纪磁性地层柱,标定了各组地质年代,为在不同盆地进行对比,提供了新的依据。 相似文献
843.
1994年2月16日共和5.8级地震短临预报实况 总被引:5,自引:0,他引:5
本文真实地再了1994年2月16日青海共和5.8级地震前前兆异常的发展过程及对该地震的短临预报过程,同时系统地分析了前兆异常在时间,空间及种数上的分布特征。指出,在有一定前兆监测能力的地区,对一些较大地震作出一定的或成功的短临预报是有希望的。 相似文献
844.
海城7.3级地震前地震波动力学特征量的异常变化 总被引:1,自引:0,他引:1
本文给出对海城7.3级地震前地震波动力学特征量变化的一些最新研究结果。所研究的地震波包括体波(P,S波)、尾波和短周期地脉动三类。特征量有:体波与地脉动的波形时间线性度和空间线性度,平均半周期,频谱的峰值频率、拐角频率、相对频带宽度、相对频谱峰值、高频段的谱线斜率绝对值;尾波的时间熵、振幅比、持续时间、观测与计算持续时间差及其二阶差分、Q_c值、反映介质混浊度与震源特性的系数a_c等。所得结果表明,三类地震波的上述动力学特征量大都在震前一至半年左右出现、有的在6-10天乃至一天以内出现过不同形态的阶段性异常变化,因而可看作海城地震的中短期和临震的地震波前兆异常指标。 相似文献
845.
MONITORING OF 1991 EASTERN CHINA FLOODING WITH POLAR ORBITING METEOROLOGICAL SATELLITES FY-1 AND NOAA 下载免费PDF全文
Xu Jianmin Wang Dachang Sa Yang Xiao Qianguang Feng Yurong 《Acta Meteorologica Sinica》1995,9(1):87-94
With polar orbiting meteorological satellites FY-1 and NOAA,flooding was monitored in the areas of the HuaiheRiver basin and the Taihu Lake region during June and July 1991.All satellite images from FY-1 and NOAA for concerned areas before and during flooding were examined.Thoseof cloud-free,with small amount of cumulus or thin cirrus were selected to exam the situation.Navigation and projec-tion were carefully performed,to ensure the projected images at different time overlap accurately with each other in 1—2pixels.Channel 1 (CH1) and Channel 2 (CH2) data of FY-1 and NOAA satellites with wavelength of 0.58—0.68μm and0.725—1.1μm were used to monitor the flooding.Albedo of Channel 2 and normalized vegetation index (NDVI) wereadopted as indicators to identify water body from land.With histogram and man-machine interactive methods,analysiswas done.In cloud-free condition,the two indicators identified the same area and scope of the water body.Totally cloud-free image in a large area is quite rare.To understand flood process,it is necessary to use more fre-quent images.It was investigated to distinguish water from land in partly cloudy condition.The result showed that whenthere is small amount of cumulus or thin cirrus,satellite images are still valuable in monitoring water body.In case ofmonitoring area covered with cirrus,vegetation index is useful,and while there is small amount of cumulus on land,albedo of Channel 2 can be used.Ten images from May 16 to August 18 of 1991 were examined.The results show that in the Lixiahe area,JiangsuProvince,the area submerged in total was the largest;along main stream of the Huaihe River,the Chuhe River,andaround the Chaohu Lake,a large percentage of area submerged;while in the Taihu Lake area,less field submerged.Flood monitoring was performed for 87 counties in the region concerned.These counties were put in order accord-ing to the percentage of submerged area in total.This order showed the extent of disaster at one view point. 相似文献
846.
847.
冻土蠕变过程中结构的CT分析 总被引:5,自引:1,他引:5
CT为非破坏的持续检测和定量描述不同实验条件下试样的内部结构提供了可能,本文利用这一手段观测分析了冻土蠕变过程结构的变化情况,认为冻土蠕变过程中所进行的发育微裂隙、颗粒集合体的破坏以及其它结构缺陷的增生与扩展,制约着土结构的强化与弱化作用,控制着蠕变过程的形态特征,同时还给出了CT值与物密度和含水量之间的定量关系。 相似文献
848.
本文是1:400万“中国及邻近海域岩石圈动力学图”说明书的节要。它对我国现今活动着或在新生代活动过的地质和地球物理作用过程作了综合概括,重点是板内现象,并从板块构造作用基本过程上对它们加以解释。 中国的岩石圈很不均匀。其动力学涉及8个活动亚板块和有关的17个构造块体的性质、它们的相对运动和构造应力场、以及新构造变形的特征。阐明了我国岩石圈现今运动和变形 相似文献
849.
850.
We have compared the Haicheng foreshock sequence with several earthquake swarms which occurred in its neighborhood. The spatial distribution of the earthquakes is relatively concentrated. For the most part, the events occurred within a few kilometers of each other. The focal mechanisms are comparatively stable. However, there are several swarms in which the variations of focal mechanisms are quite obvious after the occurrence of the largest event of the sequence, which would allow it to be recognized as a swarm. However, there are also swarms whose focal mechanisms are no less stable throughout the sequence compared to the Haicheng foreshock sequence. This feature could thus not be used to identify a foreshock sequence. The temporal distributions of foreshocks and swarms are quite similar in some cases. This is again not a definite criterion for identifying foreshocks, but is worthy of further study. Thus, no definite criterion for identifying foreshock sequences has been found. However, some earthquake swarms may be recognized in their later stage.Finally, we introduced a magnitude sequence with gaps which can be used to see whether a large event is still forthcoming. This method (in conjunction with other methods) could be used in areas prone to large earthquakes, immediately before a large event, to improve the probability of predicting the occurrence of a large event. We also report that the temporal distribution of all the sequences showed a 12-hour recurrence pattern that corresponded with the earth tides, indicating that tidal forces might be influencing foreshocks and earthquake swarm occurrence. 相似文献