全文获取类型
收费全文 | 701篇 |
免费 | 112篇 |
国内免费 | 54篇 |
专业分类
测绘学 | 54篇 |
大气科学 | 61篇 |
地球物理 | 239篇 |
地质学 | 144篇 |
海洋学 | 37篇 |
天文学 | 10篇 |
综合类 | 32篇 |
自然地理 | 290篇 |
出版年
2023年 | 6篇 |
2022年 | 13篇 |
2021年 | 41篇 |
2020年 | 29篇 |
2019年 | 22篇 |
2018年 | 23篇 |
2017年 | 26篇 |
2016年 | 22篇 |
2015年 | 29篇 |
2014年 | 45篇 |
2013年 | 74篇 |
2012年 | 31篇 |
2011年 | 30篇 |
2010年 | 27篇 |
2009年 | 33篇 |
2008年 | 29篇 |
2007年 | 35篇 |
2006年 | 39篇 |
2005年 | 30篇 |
2004年 | 48篇 |
2003年 | 29篇 |
2002年 | 26篇 |
2001年 | 21篇 |
2000年 | 17篇 |
1999年 | 15篇 |
1998年 | 22篇 |
1997年 | 13篇 |
1996年 | 18篇 |
1995年 | 11篇 |
1994年 | 9篇 |
1993年 | 14篇 |
1992年 | 3篇 |
1991年 | 10篇 |
1990年 | 2篇 |
1989年 | 1篇 |
1988年 | 5篇 |
1987年 | 4篇 |
1986年 | 1篇 |
1985年 | 4篇 |
1984年 | 6篇 |
1983年 | 3篇 |
1979年 | 1篇 |
排序方式: 共有867条查询结果,搜索用时 468 毫秒
161.
Local reactivations of landslides in forests are rarely reported in landslide catalogues. The occurrence of hillslope sections with fresh morphological landslide features in forested old, deep‐seated landslides, however, suggests that landslide reactivations are not restricted to residential areas. In this study, a dendrogeomorphological analysis of beech stands was used to investigate the periods of reactivation of a deep‐seated rotational slide in the Koppenberg forest (Flemish Ardennes, Belgium). The relation to rainfall and the correspondence to landslide reactivations reported in a nearby built‐up area were also analysed. A dendrometrical study preceding the dendrochronological analysis proved that, compared with the nearby reference site, trees on the Koppenberg forest landslide site were significantly more inclined and showed more knees, indicating that the landslide site has not stabilized yet. As the sampled trees are younger than the landslide, dendrochronology did not allow determination of the year in which the landslide was initiated, but analysis of two different tree ring width parameters (i.e. ring eccentricity and growth change) calculated for trees sampled on the Koppenberg landslide and the reference site proved to be of great help in determining the temporal sequence of landslide reactivation. During the past 80 years, several periods indicative of local reactivations (i.e. 1943–1945, 1949–1952, 1967–1970, 1972–1977, 1979–1981, 1988–1997) were found within the investigated landslide, but delineation of the spatial extent of the reactivations during these indicative periods was not straightforward. These periods generally correspond to years with above‐average rainfall. Finally, the fact that at least 34% of the years indicative of reactivation of the Koppenberg forest landslide correspond to a year in which a landslide reactivation was reported in the Flemish Ardennes suggests that in built‐up areas, apart from anthropogenic interventions, natural triggering factors remain very important. Copyright © 2009 John Wiley & Sons, Ltd. 相似文献
162.
More than 240 items of historical records containing climatic information were retrieved from official historical books, local
chronicles, annals and regional meteorological disaster yearbooks. By using moisture index and flood/drought (F/D) index obtained
from the above information, the historical climate change, namely wet-dry conditions in borderland of Shaanxi Province, Gansu
Province and Ningxia Hui Autonomous Region (BSGN, mainly included Ningxialu, Hezhoulu, Gongchanglu, Fengyuanlu and Yan’anlu
in the Yuan Dynasty) was studied. The results showed that the climate of the region was generally dry and the ratio between
drought and flood disasters was 85/38 during the period of 1208–1369. According to the frequencies of drought-flood disasters,
the whole period could be divided into three phases. (1) 1208–1240: drought dominated the phase with occasional flood disasters.
(2) 1240–1320: long-time drought disasters and extreme drought events happened frequently. (3) 1320–1369: drought disasters
were less severe when flood and drought disasters happened alternately. Besides, the reconstructed wet-dry change curve revealed
obvious transition and periodicity in the Mongol-Yuan Period. The transitions occurred in 1230 and 1325. The wet-dry change
revealed 10- and 23-year quasi-periods which were consistent with solar cycles, indicating that solar activity had affected
the wet-dry conditions of the study region in the Mongol-Yuan Period. The reconstructed results were consistent with two other
study results reconstructed from natural evidences, and were similar to another study results from historical documents. All
the above results showed that the climate in BSGN was characterized by long-time dry condition with frequent severe drought
disasters during 1258 to 1308. Thus, these aspects of climatic changes might have profound impacts on local vegetation and
socio-economic system. 相似文献
163.
历史将永远铭记他们——记在叠溪大地震的考察、研究和救灾工作中作出贡献的几位前辈 总被引:4,自引:0,他引:4
考证并记叙了在1933年叠溪地震的考察、研究和救灾工作中作出过重要贡献的若干前辈的事迹,包括常隆庆、李善邦、周郁如、徐近之、庄学本、张雪岩等先生和四川大学的师生们。他们是中国地震科学和防震减灾事业的先行者,永远值得我们怀念。 相似文献
164.
165.
166.
In this paper we present magnitude (Ms) – magnitude(mb) and magnitude-intensity relationships which areconsidered the most adequate in the Ibero-Maghrebianregion. This work is based on selected samples ofrecently revised events with magnitude mb assigned bythe Instituto Geográfico Nacional (I.G.N.) and Msassigned by I.S.C and N.E.I.C., and isoseismal mapsfrom 142 events. Using these data, we have obtainedone magnitude (Ms) – magnitude (mb) relationship, twomagnitude (mb and Ms) assignment relationships viaepicentral intensity (I0), and ten magnitude (mb andMs) assignments relationships via macroseismicinformation: four using Ambraseys' methodology (1985)and six using the isoseismal area of degree III, IV and VI.According to the obtained results it could be concluded that historical magnitude assignment with lesser uncertainties are those obtained via macroseismic information using magnitude-intensity relationships with Ambraseys' methodology (1985). The magnitude-isoseismal area assignment relationships have, in most cases, great differences depending on the degree of the isoseismal area used. Magnitude assignments via epicentral intensity have the highest uncertainties. Geographic regionalization of the relationshipshas been studied but the highest correlations and statistical significance are obtained when we fit all the Ibero-Maghrebian region data.Finally we have used the results obtained in this workto assign magnitude to some important historicalearthquakes in the Ibero-Maghrebian region: the 1755Lisbon earthquake, the 1680 Málaga earthquake, the1829 Torrevieja earthquake and the 1884 Arenas del Reyearthquake. According to our relationships andmethodology we have assigned an Ms value of 9.3 ±0.6 to the 1755 Lisbon earthquake (its mb magnitudecannot be estimated due to the saturation of the mbscale), an mb value of 6.3 ±0.4 and an Ms valueof 6.9 ± 0.6 to the 1829 Torrevieja earthquake, anmb value of 6.2 ± 0.4 and an Ms value of 6.4 ±0.6 to the 1680 Málaga earthquake and an mb valueof 6.1 ± 0.4 and an Ms value of 6.5 ± 0.6 tothe 1884 Arenas del Rey earthquake. 相似文献
167.
168.
IntroductionThe downfaulted system around Ordos block is a typical area in China, in which active normal dip-slip or strike-slip faults with normal dip-slip faults developed, and is also an area in which historical strong earthquakes actively occurred. According to historical records, there were ten strong earthquakes with M(7 occurred during past 1 500 years, including 4 M=8 earthquakes. Study on these historical large earthquakes in the area will be helpful to recognize segmentation charac… 相似文献
169.
Ivo Allegretti Davorka Herak Marijan Herak Seweryn J. Duda 《Studia Geophysica et Geodaetica》2000,44(1):13-25
The magnitudes (M
S
, m
bP
, m
bS
) of the largest historical earthquakes which occurred in the first half of the 20
th
century, calculated on the basis of records of Wiechert horizontal seismographs in Göttingen (Germany) and Zagreb (Croatia), are compared with one another, as well as with the magnitudes reported in worldwide catalogues. Systematic trends are observed in the data regarding the temporal stability of magnitude estimations in Göttingen, as well as the apparent non-linearity of the instrument responsle in the case of the Wiechert seismograph in Zagreb. We were unable to clearly identify their causes – possible explanations include effects caused by the interaction of the seismometer's frame and mass, as well as local soil conditions, but nonhomogeneity of the reference catalogues cannot be ruled out. The results indicate that a careful re-examination and cross-checking of the reported magnitude figures for the earthquakes from the first half of the 20th century is required. 相似文献
170.
GIS在历史、文化地理学研究中的应用及展望 总被引:3,自引:0,他引:3
李凡 《地理与地理信息科学》2008,24(1):21-26,48
通过对文献的综合分析,总结了GIS应用于历史地理学、文化地理学、考古和文化资源管理以及空间社会科学的研究进展,并介绍了我国历史文化地理信息系统的建设实践。尽管在历史地理和文化地理研究中GIS应用仍面临一些问题,但它拥有巨大的潜力。因此,国内历史地理和文化地理学者应该重新认识GIS的作用,开发适合的GIS应用软件,搭建跨学科的合作研究平台,争取将GIS在历史文化研究中的应用纳入数字城市计划之中。 相似文献