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971.
通过对北秦岭丹凤地区早古生代花岗岩的Ph、Sr、Nd同位素地球化学特征的系统研究,结合元素地球化学特征,证明早古生代具成分极性的枣园、黄柏岔、石门花岗岩是由于秦岭群斜长角闪岩和黑云斜长片麻岩部分熔融,近俯冲带以熔体与熔体的混合、远离俯冲带是前者产生的熔体与后者熔融后的残留相以不同比例混合形成的。 相似文献
972.
70年代末以来,金沙江蛇绿岩带或金沙江缝合带受到人们的重视,其地质证据主要在滇西北德钦-川西南得荣一带(张之盂和金蒙,1979;陈炳蔚,1983;黄汲清等,1984;陈炳蔚等,1991)。由于该地区构造复杂,地形险峻,交通不便,研究程度不高。 相似文献
973.
974.
Temporal and compositional differences between subsolidus and anatectic migmatite leucosomes from the Quetico metasedimentary belt, Canada 总被引:3,自引:1,他引:3
Abstract Migmatites in the Quetico Metasedimentary Belt contain two types of leucosome: (1) Layer-parallel leucosomes that grew during deformation and prograde metamorphism. These are enriched in SiO2 , Sr, and Eu, but depleted in TiO2 , Fe2 O3 , MgO, Cs, Rb, REE, Sc, Th, Zr, and Hf relative to the Quetico metasediments. (2) Discordant leucosomes that formed after the regional folding events when metamorphic temperatures were at their peak. These are enriched in Rb, Ba, Sr and Eu, but display a wide range of LREE, Th, Zr, and Hf contents relative to the Quetico metasediments.
Layer-parallel leucosomes formed by a subsolidus process termed tectonic segregation. This stress-induced mass transfer process began when the Quetico sediments were deformed during burial, and continued whilst the rocks were both stressed and heterogeneous. Subsolidus leucosome compositions are consistent with the mobilization of quartz and feldspar from the host rocks by pressure solution. The discordant leucosomes formed by partial melting of the Quetico metasediments, possibly during uplift of the belt. The range of composition displayed by the anatectic leucosomes arises from crystal fractionation during leucosome emplacement. Some anatectic leucosomes preserve primary melt compositions and have smooth REE patterns, but those with negative Eu anomalies represent fractionated melts, and others with positive Eu anomalies represent accumulations of feldspar plus trapped melt. 相似文献
Layer-parallel leucosomes formed by a subsolidus process termed tectonic segregation. This stress-induced mass transfer process began when the Quetico sediments were deformed during burial, and continued whilst the rocks were both stressed and heterogeneous. Subsolidus leucosome compositions are consistent with the mobilization of quartz and feldspar from the host rocks by pressure solution. The discordant leucosomes formed by partial melting of the Quetico metasediments, possibly during uplift of the belt. The range of composition displayed by the anatectic leucosomes arises from crystal fractionation during leucosome emplacement. Some anatectic leucosomes preserve primary melt compositions and have smooth REE patterns, but those with negative Eu anomalies represent fractionated melts, and others with positive Eu anomalies represent accumulations of feldspar plus trapped melt. 相似文献
975.
胶北蓬莱群的同位素年龄及其区域大地构造意义 总被引:7,自引:0,他引:7
位于胶北带的蓬莱群是鲁东残留于太古宙—早元古代结晶基底之 上唯一的盖层。其沉积时代和变形、变质时代过去一直是未解决的问 题。本文报道并解释了从蓬莱群板岩中新获得的全岩Rb-Sr年龄、伊 利石-全岩对Rb-Sr年龄和伊利石K-Ar年龄。 在对样品的构造、变质研究和伊利石结晶度、X射线衍射及扫描电 镜分析的基础上,所得473±32Ma(奥陶纪)的全岩Rb-Sr年龄被解 释为蓬莱群遭受埋藏变质的中止时间。因此蓬莱群是老于奥陶纪的地 层。蓬莱群的第一期褶皱和同构造低绿片岩相变质(即蓬莱运动),发生于299±4Ma以前,即晚石炭世。处于华北板块南缘上胶北带的蓬莱运动,是华北和扬子板块沿胶南带碰撞的结果。这表明郯庐断裂以东华北与扬子板块的陆-陆碰撞发生在晚石炭世。这一碰撞事件在秦岭-大别山-胶南碰撞带以北的华北板块南缘带中都造成了近南北向挤压变形。 相似文献
976.
根据大量的野外地质调查和测量资料分析,讨论了地震滑坡沿昌马断裂带走向和倾向的展布特征。研究认为昌马断裂带地震滑坡主要发生在山坡坡度30°-50°的部位和山坡地形高差100-300m的部位;地震滑坡规模、数量的分布特征与断裂活动强度的分布变化有密切的关系,这是地震滑坡与降水滑坡、人为滑坡和融冻滑坡的最大区别;最后讨论了地震滑坡最大水平滑距的规律,对地震滑坡灾害预测有很现实的意义。 相似文献
977.
青藏高原隆升的主因—大陆板块内的盆-山碰撞作用 总被引:7,自引:0,他引:7
在地壳运动中,盆地和山脉的形成机制是不可分割而有联系的。上地幔的波动起伏引起地壳上部物质的分配,在重力均衡作用的支配下,地壳物质由上地幔的隆升区域向拗陷区域蠕动,因而形成大陆板块内的盆地和山脉的分异和盆-山运动。高耸的喜马拉雅山和青藏高原就是塔里木盆地、卡拉库姆盆地和印-恒盆地等巨大盆地的扩张作用挤压而造成的。盆-山运动是真正的造山运动。 相似文献
978.
Suresh C. Baral Carlos Daganzo Michael Hood 《Geotechnical and Geological Engineering》1987,5(4):391-404
Summary The transportation of coal out of a mine is usually done by a serially linked system of conveyors. It is apparent that in a serially dependent system of this type the failure of any one component (conveyor) causes the complete system to be shut down. The provision of bunkers at strategically located points in the conveyor system can result in the production of coal even in the event of failure of some outbye conveyors. Although the use of bunkers can increase mine system availability, the maximum possible system availability may not be attained if the bunker capacity is inadequate and/or the location of these bunkers in the system is inappropriate. This paper presents a stochastic model by which the optimum capacities and locations of bunkers can be determined for a system consisting of a single production section and a system of serially linked conveyors. 相似文献
979.
The construction of the Yangtze River Economic Belt is one of the major strategic initiatives to promote the sustained and steady growth of China's economy at current and the new normal stages. Comprehensive enhancing the governance levels of various natural disaster risks in the Yangtze River Economic Belt is the basic guarantee for promoting the implementation of the development strategy. Based on the multi-hazard integrated risk theory, the main disaster risks of the core cities (Shanghai, Wuhan, and Chongqing) of the Yangtze River Economic Belt and the major risk-earthquake disaster chain were systematically analyzed. The status and existing problems of multi-hazard integrated risk governance in the Yangtze River Economic Belt were expounded in this paper. The main problems include: Insufficient understanding of multi-hazard integrated risk formation mechanism; low level of safety fortification; Imperfect regional coordination and linkage mechanism; and insufficient role of insurance and reinsurance in risk transfer. Finally, the overall promotion strategies were proposed, including establishing multi-hazard integrated risk identification mechanism and governance capability evaluation system; comprehensive improving the fortification level of multi-hazard integrated risk prevention; establishing multi-hazard and multi-party linkage disaster monitoring and early warning systems; strengthening major disaster risk management and evacuation facilities construction; accelerating the construction of catastrophe insurance systems based on multi-hazard risks. This will provide a theoretical reference for major disaster risks studies in the Yangtze River Economic Belt. 相似文献
980.
Z.N. Pojarkova 《Cretaceous Research》1984,5(1):1-14
Northeastern Central Asia during the Albian and Early Cenomanianwas one of the peripheral basins of the Central Asian region. The similarity of their freshwater molluscs makes it possible to correlate isolated series in these two regions. Subsequently, a pulsating transgression of the Tadzhik Sea invaded northeastern Central Asia which became a part of the Central Asian Province of the Tethys. The complicated palaeogeography means that there are many different local biostratigraphic successions. The relations between these have been worked out from an integrated study of the biostratigraphy, palaeogeography, ecology and biogeography. Marked endemism amongst the molluscs, sometimes total, limits correlation with other regions of the Tethys; in particular, correlation of some of the local biozones (or “lones”) with western European zones is still uncertain. 相似文献