全文获取类型
收费全文 | 9124篇 |
免费 | 2211篇 |
国内免费 | 3405篇 |
专业分类
测绘学 | 1562篇 |
大气科学 | 1408篇 |
地球物理 | 1756篇 |
地质学 | 6313篇 |
海洋学 | 1586篇 |
天文学 | 154篇 |
综合类 | 821篇 |
自然地理 | 1140篇 |
出版年
2024年 | 87篇 |
2023年 | 203篇 |
2022年 | 511篇 |
2021年 | 688篇 |
2020年 | 550篇 |
2019年 | 679篇 |
2018年 | 605篇 |
2017年 | 579篇 |
2016年 | 572篇 |
2015年 | 669篇 |
2014年 | 696篇 |
2013年 | 781篇 |
2012年 | 833篇 |
2011年 | 840篇 |
2010年 | 825篇 |
2009年 | 756篇 |
2008年 | 793篇 |
2007年 | 732篇 |
2006年 | 675篇 |
2005年 | 572篇 |
2004年 | 456篇 |
2003年 | 329篇 |
2002年 | 261篇 |
2001年 | 247篇 |
2000年 | 204篇 |
1999年 | 141篇 |
1998年 | 82篇 |
1997年 | 80篇 |
1996年 | 61篇 |
1995年 | 56篇 |
1994年 | 27篇 |
1993年 | 29篇 |
1992年 | 23篇 |
1991年 | 19篇 |
1990年 | 18篇 |
1989年 | 9篇 |
1988年 | 7篇 |
1987年 | 9篇 |
1986年 | 4篇 |
1985年 | 5篇 |
1984年 | 3篇 |
1983年 | 4篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 5篇 |
1976年 | 1篇 |
1958年 | 1篇 |
1957年 | 3篇 |
1954年 | 8篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
71.
山东三山岛金矿床流体包裹体特征及其地质意义 总被引:5,自引:0,他引:5
三山岛金矿床位于莱州市三山岛—仓上断裂带内,矿石主要为蚀变岩和含金石英脉2种类型。随着胶东金矿床研究的深入和三山岛金矿资源的不断减少,对三山岛金矿床的成矿作用及深部开发前景问题研究具有更重要的意义。针对上述问题,对三山岛金矿床2种类型矿石的成矿流体特征进行对比研究,认为代表成矿早—中期的蚀变岩型矿石形成于中温(均一温度为325~240℃)、低盐度(2.07%~6.88%)、低密度(0.720~0.868g/cm3)、酸碱性不均匀(pH=3.27~10.43)、以氟化物和氯化物为成矿物质载体的还原性流体;代表成矿中—晚期的含金石英脉型矿石形成于中—低温(均一温度为306~160℃)、低盐度(1.05%~9.73%)、低密度(0.739~0.962g/cm3)、碱性(pH=9.25~9.85)、以氯化物和硫化物为成矿物质载体的还原性流体。成矿流体性质的转变反映了成矿流体处于由比较封闭到比较开放的构造环境的转变期,且成矿流体早期以原生岩浆水为主,后期有变质水、大气降水以及海水的参与作用。三山岛金矿成矿深度为2.5~5km,根据目前的开采深度推算其深部还有一定的资源量可供开发。 相似文献
72.
73.
74.
Studies on rain-runoff process in the peripheral mountainous area of the Sichuan Basin, which is regarded as a key ecological shelter, will contribute to flood control and environmental protection for the Upper Yangtze River Basin. In two typical catchments--the Fujiang River Catchment and the Wujiang River Catchment, rainfall simulations have been conducted to study the rain-runoff processes of yellow soil and limestone soil in three types of land use--forestland, farmland and grassland. Results showed that (1) within the same rainfall process, overland flow occurs first on farmland, then on grassland, and finally on forestland; (2) soil surface coverage has a great impact on the occurrence and amount of overland flow. The runoff amount can increase 2-4 times after the coverage is removed; (3) the infiltration before the occurrence of overland flow will decrease because of higher gravel contents of soil, but it takes no effect on infiltration once overland flow becomes stable; (4) the runoff coefficient of the limestone soil forestland is greater than that of the yellow soil forest land, but less than that of the farmland; (5) three empirical infiltration models, including Horton' model, Kostiakov' model, and modified Kostiakov' model, were compared by using the observed results under rainfall simulation. The results showed that the Kostiakov' model performed better than both the Horton' model and modified Kostiakov model. According to the results of this research, the Kostiakov's model can be used to simulate rainfall infiltration when water erosion is modeled in the peripheral mountainous area of the Sichuan Basin. 相似文献
75.
Effect of Bacillus mucilaginosus on weathering of phosphorite and a preliminary analysis of bacterial proteins 总被引:3,自引:0,他引:3
The authors investigated the effect of Bacillus mucilaginosus on weathering of phosphorite. Analysis of different proteins was of significance in exploring the molecular biological mechanism in the bacterial weathering process. The concrete methods are described as follows: Mineral powder was put into liquid culture medium and B. mucilaginosus was incubated in the medium. The control (group) had no mineral powder in the medium. The treatments and controls were cultured simultaneously under the same condition. In a few days, the supernatant was filtrated, the main cations (Ca^2+, Mg^2+, Na^+, Mn^2+, Al^3+, Fe^3+, K^+) were measured by ICP-OES, and the contents of water soluble phosphorus (Pws) and silicon (Siws) were determined by colorimetry. The residual solid was weighed on the filter paper, followed by digestion with concentrated HNO3. The concentrations of the main cations and Pws, Siws in the digest liquid were measured by using the method mentioned above. After the supernatant was centrifuged, the precipitation was used to analyze the protein differences between the treatment groups and the control groups by 2-dimentional gel electrophoresis (2-DE). The experimental results showed that apatite and quartz were partially weathered, but kaolinite was dissolved completely. The population of bacteria increased when mineral powder was added in the liquid medium. Software analysis and comparison of the 2-DE pictures of bacterial proteins revealed 1134 visible protein spots in the treatment group, and 729 visible protein spots in the control group. To compare the bacterial protein expression contents of the treatment group with those of the control group, there were 496 different protein spots, including 214 protein spots which indicated that the protein contents increased, 75 protein spots were indicative of a decrease, and 207 proteins were newly synthesized. It is proposed that the increased bacterial contents may be related to some protein expression and activation after the 相似文献
76.
The Xitieshan lead-zinc deposit is located at the northern margin of the Qaidam Basin, Qinghai Province, China, and had developed a complete marine sedimentary-exhalative system. Our preliminary study of ore-forming fluids shows that fluid inclusions in quartz from altered stockwork rocks that represent the pipe facies have a wide range of temperature and salinity. The intense fluid activities are characteristics of the pipe facies of the exhalative system. Fluid inclusions in carbonates near the unstratified ore bodies hosted in the thick-bedded marble which represents vent-proximal facies are large in size and have moderate to high temperatures. They represent unerupted sub-seafloor fluid activity. Fluids in altered stockwork rocks and carbonates have similar H2O-NaCl-CO2 system, both belonging to the sedimentary-exhalative system. The fluids migrate from the pipe facies to the unstratified ore bodies. Boiling of the fluids causes the separation of CO2 vapor and liquid H2O. When the fluids migrate into the unconsolidated thick-bedded marble, the escape of CO2, decreasing temperature and pressure as well as some involvement of seawater into the fluids result in the unmixing of fluids with high and low salinity and deposition of ore-forming materials. The two unmixed fluids were trapped in unconsolidated carbonates and the ore-forming materials were deposited in the unconsolidated carbonates to form the sedimentary-exhalative type unstratified ore bodies. The ore-forming temperature of unstratified ore bodies is up to high temperature indicating that there is a huge ore-forming potential in its deep. 相似文献
77.
藏南冈底斯带西段麦拉花岗岩锆石SHRIMP定年及地质意义 总被引:1,自引:0,他引:1
用SHRIMP测定了冈底斯岩带西段麦拉山口岩体同碰撞黑云母二长花岗岩锆石的U-Pb年龄,黑云母二长花岗岩锆石SHRIMP U-Pb年龄为47.1±1.1Ma。这就为前人提出的雅鲁藏布江地区洋盆闭合、板块开始碰撞的时间为50Ma左右提供了同位素年代学的证据。 相似文献
78.
79.
80.
天山公路地质灾害决策支持地理信息系统的设计研究 总被引:1,自引:0,他引:1
天山公路由于其特殊复杂地形、地质条件及受降雨、地下水等因素,严重影响其正常通行,同时天山公路还经常受到泥石流、滑坡、崩塌、溜砂坡等地质灾害的危害,这对该公路稳定性和沿线居民的安全性都具有一定的威胁。因此,运用先进的技术手段,建立一套适应于天山公路的地质灾害决策支持信息系统就显得尤其重要。该系统的建立,对天山公路的建设改造和管理提供了强有力的支持。天山公路地质灾害决策支持地理信息系统利用强大的ArcEngine开发组件,针对新疆天山公路实际,引入RS、GIS的相关理论、方法和技术分析手段,采用相应的数学分析评价模型,对提高天山公路地质灾害防治管理水平和地质灾害的有效防治,以及评价决策等方面,都具有重要的意义。 相似文献