全文获取类型
收费全文 | 8302篇 |
免费 | 2139篇 |
国内免费 | 1947篇 |
专业分类
测绘学 | 58篇 |
大气科学 | 248篇 |
地球物理 | 1029篇 |
地质学 | 8484篇 |
海洋学 | 979篇 |
天文学 | 11篇 |
综合类 | 296篇 |
自然地理 | 1283篇 |
出版年
2024年 | 105篇 |
2023年 | 288篇 |
2022年 | 467篇 |
2021年 | 570篇 |
2020年 | 466篇 |
2019年 | 581篇 |
2018年 | 491篇 |
2017年 | 599篇 |
2016年 | 652篇 |
2015年 | 523篇 |
2014年 | 625篇 |
2013年 | 648篇 |
2012年 | 592篇 |
2011年 | 558篇 |
2010年 | 509篇 |
2009年 | 600篇 |
2008年 | 515篇 |
2007年 | 550篇 |
2006年 | 444篇 |
2005年 | 414篇 |
2004年 | 325篇 |
2003年 | 287篇 |
2002年 | 249篇 |
2001年 | 188篇 |
2000年 | 164篇 |
1999年 | 188篇 |
1998年 | 124篇 |
1997年 | 130篇 |
1996年 | 102篇 |
1995年 | 80篇 |
1994年 | 86篇 |
1993年 | 56篇 |
1992年 | 76篇 |
1991年 | 44篇 |
1990年 | 21篇 |
1989年 | 19篇 |
1988年 | 18篇 |
1987年 | 3篇 |
1986年 | 7篇 |
1985年 | 3篇 |
1984年 | 3篇 |
1983年 | 1篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 6篇 |
1979年 | 5篇 |
1977年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
991.
992.
南天山西段南缘断裂构造特征及对乌什凹陷发育的控制 总被引:10,自引:7,他引:3
乌什凹陷位于南天山西段以南,新生代受南天山崛起的陆内造山作用制约,与库车坳陷有相同的成盆动力学背景。因乌什凹陷南有温宿凸起阻挡了挤压应力的传播,东与库车坳陷间有北西向的构造变换带(西秋里塔格构造带)所隔,新生代变形与库车地区有不同的特征。以吉迪克组的泥岩层为滑脱面,乌什凹陷的中-新生界可分为上、下两个构造层,总体看上构造层以背冲构造为特征,下构造层则发育基底卷入的对冲构造。乌什凹陷的这一变形特征还与新生代挤压应力场自东向西迁移和走滑作用吸收了部分冲断变形有关,反映了南天山新生代构造对海西-印支期碰撞构造的继承性。文章简述了南天山造山带的构造演化,介绍了乌什凹陷周缘的主要断裂的特征,恢复了乌什凹陷中-新生代的演化并与库车坳陷进行了对比。在此基础上探讨了乌什凹陷的成盆动力学机制,分析了乌什凹陷与南天山造山带的耦合演化,指出该区的油气勘探应以三叠系为主要目的层。 相似文献
993.
基于长江流域148个气象站1980—2017年的蒸发皿观测数据,将旋转经验正交函数(REOF)和模糊C均值聚类(FCM)相结合,对流域蒸发皿蒸发量(PE)进行分区,然后运用Modified Mann-Kendall检验和多元逐步回归等方法,分析各子区域PE的变化特征并识别其主要影响因子。结果表明:1) REOF的前4个空间模态显示流域PE存在5个主要的异常敏感区,基于这4个空间模态,流域PE在空间上可划分为9个子区域。2)在年尺度上,各区PE呈不同程度的增加趋势,其中中部盆地区上升速率最大(111.28 mm/10 a),西部高原区上升速率最小(12.5 mm/10 a);而在季节尺度上,秋、冬季流域PE呈显著上升趋势,春、夏季PE的变化具有明显的区域差异性,部分地区PE为下降趋势。3)影响PE变化的主要因子因地而异,但大多子区域的PE变化与平均气温和饱和水汽压差的变化显著相关。 相似文献
994.
995.
996.
997.
概述了北黄海盆地的区域地质背景和速度分析的原理,通过对北黄海盆地速度谱的解释和计算,得到了层速度、平均速度、砂岩百分含量等信息,利用这些速度资料识别多次波、辨别坳陷区和隆起区,进行时深转换、构造分析以及岩性分析,为北黄海盆地地震资料解释、沉积相分析以及资源量计算提供可靠的依据。 相似文献
998.
河流相沉积的河型转换特征与控制因素及其油气地质意义
——以南苏丹Melut盆地Ruman地区坳陷期Jimidi组为例 总被引:1,自引:1,他引:0
河流相砂体是陆相含油气盆地的重要储层类型,其河型的时空转换不仅是研究盆地演化的直接证据,更是精准评价与预测油气储层的核心内容,已成为近年来国内外沉积研究的热点之一.以Melut盆地Ruman地区坳陷期Jimidi组为例,通过开展层序划分、岩相类型与岩相组合分析、高分辨率储层反演、以及砂体平面展布分析,结果表明:1)坳陷... 相似文献
999.
A.W. Ratsimandresy M.G. Sotillo J.C. Carretero Albiach E. Álvarez Fanjul H. Hajji 《Coastal Engineering》2008
A set of 44-year (1958–2001) homogeneous and high-resolution hindcasts of atmospheric, sea level residuals, and wave states was performed for the Mediterranean Basin within the framework of the HIPOCAS European Project. To this aim, different numerical models were used. As a first step, a Mediterranean high-resolution atmospheric database, suitable to provide realistic and homogeneous forcing for ocean hindcast runs was generated. The HIPOCAS atmospheric database was created by means of dynamical downscaling from the global reanalysis NCEP, using for that the limited area model SN-REMO along with a spectral nudging technique. In a second stage, different Mediterranean oceanic hindcasts were performed. On one hand a long-term database of sea state over the western Mediterranean was generated by means of the wave model WAM and on the other hand a sea level residual database containing storm surge events was obtained from a long-term integration of the HAMSOM model over the entire basin. The three different hindcast runs have been exhaustively validated. On that score, various simulated parameters have been compared to both satellite and in situ measurements. Such comparisons provide a measure of the skills of the different simulated fields to realistically reproduce the observed features. Once these skills are evaluated, a study of the ocean and atmospheric climate trends as well as the interannual variability for the whole 44-year period was carried out with the hindcasted data. The reliability of the data as shown by its comparison to measurements and a proven temporal homogeneity over the 44 years of simulation make the Mediterranean HIPOCAS ocean–atmosphere hindcasted database a useful tool for studies focused on regional climatic variability, as well as for further applications in coastal and environmental decision processes in the Mediterranean area. 相似文献
1000.
Sensitivity of penman-monteith reference crop evapotranspiration in Tao’er River Basin of northeastern China 总被引:1,自引:0,他引:1
A non-dimensional relative sensitivity coefficient was employed to predict the responses of reference crop evapotranspiration (ET0) to perturbation of four climate variables in Tao'er River Basin of the northeastern China. Mean monthly ET0 and yearly ET0 from 1961 to 2005 were estimated with the FAO-56 Penman-Monteith Equation. A 45-year historical dataset of average monthly maximum/minimum air temperature, mean air temperature, wind speed, sunshine hours and relative humidity from 15 meteorological stations was used in the analysis. Results show that: 1) Sensitivity coefficients of wind speed, air temperature and sunshine hours were positive except for those of air temperature of Arxan Meteorological Station, while those of relative humidity were all negative. Relative humidity was the most sensitive variable in general for the Tao'er River Basin, followed by sunshine hours, wind speed and air temperature. 2) Similar to climate variable, monthly sensitivity coefficients exhibit large annual fluctuations. 3) Sensitivity coefficients for four climate variables all showed significant trends in seasonal/yearly series. Also, sensitivity coefficients of air temperature, sunshine hours and wind speed all showed significant trends in spring. 4) Among all sensitivity coefficients, the average yearly sensitivity coefficient of relative humidity was highest throughout the basin and showed largest spatial variability. Longitudinal distribution of sensitivity coefficients for air temperature, relative humidity and sunshine hours was also found, which was similar to the distribution of the three climate variables. 相似文献