全文获取类型
收费全文 | 2552篇 |
免费 | 595篇 |
国内免费 | 1203篇 |
专业分类
测绘学 | 2篇 |
大气科学 | 25篇 |
地球物理 | 302篇 |
地质学 | 3554篇 |
海洋学 | 165篇 |
天文学 | 35篇 |
综合类 | 79篇 |
自然地理 | 188篇 |
出版年
2024年 | 11篇 |
2023年 | 51篇 |
2022年 | 81篇 |
2021年 | 96篇 |
2020年 | 109篇 |
2019年 | 137篇 |
2018年 | 134篇 |
2017年 | 141篇 |
2016年 | 180篇 |
2015年 | 138篇 |
2014年 | 174篇 |
2013年 | 207篇 |
2012年 | 185篇 |
2011年 | 165篇 |
2010年 | 161篇 |
2009年 | 225篇 |
2008年 | 200篇 |
2007年 | 210篇 |
2006年 | 200篇 |
2005年 | 175篇 |
2004年 | 154篇 |
2003年 | 149篇 |
2002年 | 128篇 |
2001年 | 120篇 |
2000年 | 119篇 |
1999年 | 117篇 |
1998年 | 100篇 |
1997年 | 84篇 |
1996年 | 69篇 |
1995年 | 66篇 |
1994年 | 75篇 |
1993年 | 35篇 |
1992年 | 42篇 |
1991年 | 24篇 |
1990年 | 25篇 |
1989年 | 21篇 |
1988年 | 14篇 |
1987年 | 14篇 |
1986年 | 2篇 |
1985年 | 3篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1981年 | 2篇 |
1980年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有4350条查询结果,搜索用时 218 毫秒
991.
对河北阳原晚白垩世地层的沉积环境进行了系统地分析,初步认为它为一套湖北和扇三角洲沉积,并对沉积环境的基本特征和盆地充填过程进行了详细论述,通过对恐龙化石产出层位的沉积环境分析,将对恐龙的埋藏与生态环境的研究具有重要的参考意义。 相似文献
992.
TAN Fuwen PAN Guitang XU Qiang Chengdu Institute of Geology Mineral Resources Chengdu 《Continental Dynamics》2001,(1)
1. Introduction The uplift and evolution of the Qinghai Tibet Plateau has been the most important projects for studying the dynamic process of the plateau, and the uplift mechanism and history are the essential problems. Researches have been done extensively in terms of tectonics, sedimentology, geophysics, paleontology, paleoclimate and paleomagnetism for several tens of years. Many evolution models have been suggested but so far none of them have been explained perfectly. In recent years,… 相似文献
993.
青藏高原主夷平面形成的上限年龄为3.6MaB.P.,临夏盆地新生代湖相沉积同时结束,青藏运动开始,分为A(3.6MaB.P.),B(2.6MaB.P.)和C(1.7MaB.P.)3幕,A幕现代亚洲季风形成,B幕黄土开始堆积,C幕黄河出现;昆黄运动(1.2~0.6MaB.P.)使黄河干流切入青藏高原,大面积山地进入冰冻圈,可能导致中更新世之气候转型;共和运动造成黄河切穿龙羊峡,青海湖孤立,高原达到现代高度.中国三大自然区是高原隆升驱动大气环流改变而导致的中国最高层次的景观分异.本文讨论了8MaB.P.的有限高度隆升及亚洲干旱化的问题,亚洲夏季风22MaB.P.已经开始,是高原隆升及其它因素共同作用的结果,为亚洲古季风阶段.3.6MaB.P.才是现代亚洲季风真正开始的时期,可能北半球进入冰期也与此有密切关系. 相似文献
994.
鲜水河—安宁河断裂带磨西—冕宁段的滑动速率与强震位错 总被引:10,自引:1,他引:10
航片解译及野外地震地质考察结果表明,鲜水河-安宁河断裂带磨西-冕宁段存在明显的晚第四纪活动性,其以左旋走滑运动为主,并伴有显著的垂直滑动分量。晚第四纪以来的平均水平滑动速率在鲜水河断裂磨西以南段为6.0-9.9mm/a,安宁河断裂冕宁以北段为4.7-5.3mm/a。同震位错及地震地表破裂研究表明,A.D.1786年康定-泸定磨西73/4级地震的地表破裂可能南延至田湾以南;安宁河断裂冕宁以北段则具有蕴育71/2级左右地震的构造背景,最晚一次强震的地质记录极有可能是史料记载不全的A.D.1327年一次6级或6级以上地震的证据。 相似文献
995.
996.
997.
998.
Abstract The orientations of both healed extension microcracks and microcracks in quartz grains sealed mostly by carbonate minerals were measured from Cretaceous granodiorite core samples drilled along the Nojima Fault, southwest Japan. The preferred orientations of both healed and sealed microcracks consist of approximately three orthogonal sets, (components) A, B and C, in which A strikes NS–NW-SE and dips vertically, B strikes EW–NE-SW and dips vertically, and C is subhorizontal. Both the healed and sealed microcracks were possibly formed by hydraulic fracturing, and the successive release of tensile stress due to pore fluid overpressure in the principal stress directions could have caused this microcracking in mutually orthogonal directions. The quartz grains are also very moderately plastically deformed, which is indicated by the occurrence of kink bands and undulose extinction. The association of healed microcracks and kink bands in the quartz suggests that these microstructures formed under subgreenschist facies conditions (≈300°C) during hydrothermal activity that could have occurred immediately after the emplacement of granodiorite during the Late Cretaceous period. Based on both the preferred orientation of microcracks, and c-axis fabrics of kinked and unkinked grains (so called kink method), it is inferred that the σ1 -and σ3 -axis were oriented horizontally in NS–NW-SE and EW–NE-SW directions, respectively. The inferred paleostress field does not conform to the east–west-trending compression during the Quaternary period, but to the activation of EW–NE-SW-trending, left–lateral strike–slip faults during the Late Cretaceous period in southwest Japan. 相似文献
999.
Philippe Alvarez 《International Journal of Earth Sciences》1995,84(3):636-648
During Late Proterozoic times, the Archaean Central African craton was affected by trough faulting which led to the formation of grabens, the Sangha aulacogen being the main structure of this type in the studied area. This transverse basin connects with other basins on the northern and south-western borders of the craton. During the Cryogenian, this network of basins was filled with fluvio-deltaic and lacustrine periglacial deposits. The glacio-eustatic transgression in Neoproterozoic III (end-Proterozoic) times flooded extensive areas of shelf on the northern edge of the craton, leading to the development of carbonate sedimentation in a broad outer shelf environment associated with nearshore barriers and evaporitic lagoons. These facies are similar to those developed in the West Congolian Schisto-calcaire (shale-limestone) ramp succession. The North-Central African ramp succession (sediment slope) contains an example of tidal rhythmites in vertical accretion, which occurs beneath the barrier deposits on the subtidal outer shelf. Mathematical analysis of the bedding pattern yields a period of 29–30 days for the lunar month, a result which is in agreement with astrophysical evidence for this epoch (i.e. 650 Ma ago). Major subsidence and seismic activity on this gently sloping platform, associated with the proximity of the Sangha aulacogen, caused the triggering of carbonate turbidites and mass flow deposits. The proliferation of microbial mats under euphotic conditions on an extensive shelf led to the build-up of a carbonate platform. During early Neoproterozoic III times, the West Congolian and North-Central African ramps prograded northwards and southwards, respectively, into the Sangha aulacogen. The sea at that time was restricted to a long graben-like basin, while a remaining area of marine sedimentation persisted into the Palaeozoic. Thus the pattern of end-Proterozoic carbonate sedimentation on the borders of the Central African craton can be interpreted in terms of an overall gently sloping ramp model with progradation converging towards the Sangha aulacogen. 相似文献
1000.
Tectonic Environments of Cenozoic Volcanic Rocks in China and Characteristics of the Source Regions in the Mantle 总被引:1,自引:0,他引:1
Extensive volcanism is one of the important features of Cenozoic geology in China.Based on temporal-spatial distribution,the volcanism was associated with three major different geological settings:1)the continental rift basalts in Northeast and North China;2)the tension-fault basalts on the continental margins of Southeast China; and 3) the collision-zone high-K volcanics in the Qinghai-Xizang Plateau and its vicinities.The characteristics of “depletion in the south and enrichment in the north“of the China continental mantle are strongly supported by isotopic evidence.The Cenozoic continental cal characters,into the following geochemical provinces:1)the depleted mantle in South China;2)the primary mantle in Northeast and NorthChina; 3)the hybrid and transi-tional mantle in the region of Shandong ,Anhui,Jiangsu and northern Zhejiang;4)the depleted mantle around the Bohai Bay and the Lower Liaohe River;5)the K-metasomatic enriched mantle in the northern part of Northeast China;and 6)the re-cycled enriched mantle in the ancient subduction zone in the Qinghai-Xizang Plateau and its surround-ings.These geochemical characteristics on a regional scale must be a reflection of the nature of lithosphere evolution. 相似文献