全文获取类型
收费全文 | 423篇 |
免费 | 84篇 |
国内免费 | 108篇 |
专业分类
测绘学 | 19篇 |
大气科学 | 118篇 |
地球物理 | 102篇 |
地质学 | 255篇 |
海洋学 | 29篇 |
天文学 | 14篇 |
综合类 | 29篇 |
自然地理 | 49篇 |
出版年
2023年 | 8篇 |
2022年 | 20篇 |
2021年 | 23篇 |
2020年 | 22篇 |
2019年 | 21篇 |
2018年 | 20篇 |
2017年 | 21篇 |
2016年 | 18篇 |
2015年 | 15篇 |
2014年 | 16篇 |
2013年 | 26篇 |
2012年 | 18篇 |
2011年 | 22篇 |
2010年 | 16篇 |
2009年 | 15篇 |
2008年 | 20篇 |
2007年 | 10篇 |
2006年 | 10篇 |
2005年 | 12篇 |
2004年 | 13篇 |
2003年 | 8篇 |
2002年 | 14篇 |
2001年 | 12篇 |
2000年 | 22篇 |
1999年 | 26篇 |
1998年 | 26篇 |
1997年 | 29篇 |
1996年 | 17篇 |
1995年 | 15篇 |
1994年 | 19篇 |
1993年 | 9篇 |
1992年 | 6篇 |
1991年 | 10篇 |
1990年 | 6篇 |
1989年 | 7篇 |
1988年 | 4篇 |
1987年 | 4篇 |
1986年 | 2篇 |
1985年 | 6篇 |
1984年 | 2篇 |
1982年 | 3篇 |
1974年 | 2篇 |
1964年 | 2篇 |
1962年 | 1篇 |
1961年 | 1篇 |
1960年 | 1篇 |
1959年 | 1篇 |
1958年 | 1篇 |
1938年 | 1篇 |
1936年 | 4篇 |
排序方式: 共有615条查询结果,搜索用时 296 毫秒
61.
Microdiamond and graphite occur in quartzofeldspathic rocks (saidenbachites) of the central Erzgebirge in Saxony. Zircon from such rocks contains not only relatively high but also variable amounts of early formed graphite and later crystallized diamond, however no carbonate. Six purified zircon concentrates were analysed by mass spectrometry for δ13C(PDB) values which were between −24 and −33‰. The carbon inclusions resulted in C contents of the concentrates as high as 0.5 wt%. It is hypothesized that the observed δ13C signature results from organic material in the sedimentary protoliths of the saidenbachites probably deposited not earlier than Mid‐Devonian. This material was transformed to graphite during early metamorphism and subsequently to diamond after an anatectic event at great depths (>150 km). During these processes, the δ13C signature of the carbon did not (significantly) change. 相似文献
62.
63.
商丹断裂带作为扬子板块与华北板块的缝合带,在秦岭造山带中占据重要的地位。对其进行精细的构造研究,是了解扬子板块与华北板块相互作用过程的关键。研究工作在商丹断裂带东段展开,对该带进行了详细的野外观察、显微构造观察、糜棱岩化过程中温度的估算、有限应变测量、差异应力的计算以及糜棱岩化过程中运动学涡度的计算。变形温压条件指示糜棱岩形成于中-高绿片岩相到低角闪岩相变质条件。差异应力计算结果指示商丹带具备大型构造动力特征。涡度分析表明该断裂带的变形以纯剪切作用占据主导作用,但包含有简单剪切的分量,从而证明了扬子板块与华北板块之间具有以碰撞挤压为主的斜向汇聚方式。 相似文献
64.
66.
Natural Hazards - Tsunamis occur not only in marine settings but also in lacustrine environments. Most of the lacustrine tsunamis are caused by seismically- or aseismically-triggered mass... 相似文献
67.
The Hala’alat Mountains are located at the transition between the West Junggar and the Junggar Basin.In this area,rocks are Carboniferous,with younger strata above them that have been identified through well data and high-resolution 3D seismic profiles.Among these strata,seven unconformities are observed and distributed at the bases of:the Permian Jiamuhe Formation,the Permian Fengcheng Formation,the Triassic Baikouquan Formation,the Jurassic Badaowan Formation,the Jurassic Xishanyao Formation,the Cretaceous Tugulu Group and the Paleogene.On the basis of balanced sections,these unconformities are determined to have been formed by erosion of uplifts or rotated fault blocks primarily during the Mesozoic and Cenozoic.In conjunction with the currently understood tectonic background of the surrounding areas,the following conclusions are proposed:the unconformities at the bases of the Permian Jiamuhe and Fengcheng formations are most likely related to the subduction and closure of the Junggar Ocean during the late Carboniferous-early Permian;the unconformities at the bases of the Triassic Baikouquan and Jurassic Badaowan formations are closely related to the late Permian-Triassic Durbut sinistral slip fault;the unconformities at the bases of the middle Jurassic Xishanyao Formation and Cretaceous Tugulu Group may be related to reactivation of the Durbut dextral slip fault in the late Jurassic-early Cretaceous,and the unconformity that gives rise to the widely observed absence of the upper Cretaceous in the northern Junggar Basin may be closely related to large scale uplift.All of these geological phenomena indicate that the West Junggar was not calm in the Mesozoic and Cenozoic and that it experienced at least four periods of tectonic movement. 相似文献
68.
SUN Jilin ) )* XU Delong ) and GU Dejun ) ) Physical Oceanography Laboratory Ocean-Atmosphere Interaction Climate Laboratory Ocean University of China Qingdao P.R.China) Institute of Tropical Meteorology Guangzhou P.R.China 《中国海洋大学学报(英文版)》2006,5(3):200-206
1Introduction Theglobalclimatechangehasbeenoneoftheprob lemschallengingtheworldinrecentyears.TheweatherandclimateonEarthhasbeeninvariationontimescalesfromseasonaltomillennialorevenlonger.ResearchesonvariationsofweatherandclimateintheNorthernHemispherehave… 相似文献
69.
A comparison has been made between the predictions of the theory for radial variations of both Alfvénic fluctuations and solar wind proton temperatures proposed by Tu (1987, 1988) and the statistical results of hourly averaged plasma and magnetic field data observed by Helios 1 and 2 from launch through 1980 for different solar wind speed regimes. The comparison shows that for speed ranges between 500–800 km s-1, the radial variation of the proton temperature between 0.3 and 1 AU can be explained by heating from the cascade energy determined by the radial variation of the total variance of magnetic field vector. The explanation of the radial variations of both temperature and the total variance of magnetic fields for speed ranges less than 400 km s -1 is less clear.This project was supported by National Natural Science Foundation of China for Tu's part of the work. 相似文献
70.
通过对龙永煤田童子岩组煤系顶部鲕状带"鲕粒"赋存规律及其矿物学特征、宏观特征、围岩特征的野外研究及镜下观察,分析了"鲕粒"的成因及其岩相意义,为龙永煤田童子岩组顶部地层提供了对比依据. 相似文献