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991.
地图信息度量方法的研究 总被引:2,自引:0,他引:2
概率统计方法是最早用于确定地图信息量的方法。但是,由于它的种种不适宜性而受到越来越多的怀疑。本文通过对概率统计方法的分析评价,试图跳出概率统计方法的框框,寻找一种更为有效的测度地图信息量的方法——综合指数法。试验结果表明,这种尝试是十分有效的。 相似文献
992.
准噶尔盆地头屯河地区侏罗系陆相层序包含4种沉积:(1)冲积扇平原湿地中的砾石质河流沉积(八遭湾组),其特征提示在湿地中发育了规模不同的大河道(深3—5m,宽1OOm左右)及较小的分流或决口河道(深2m以下,宽6—30m)。(2)沙质低弯度河沉积,晚三工河、早西山窑、头屯河及齐古组沉积期的河流沉积属之。其特点是河道相与河间相间的界线清楚,提示河道在某一段时期固定于平原的特定地带;河道规模受古气候和构造的制约;气候干旱化和构造抬升(如头屯河组沉积时期),侵蚀基面降低,河流动力增加,因而河流规模变大,反之变小;晚头屯河组沉积期的干旱气候存在暂时性河道。(3)三角洲前缘沉积(河口中坝),见于八道湾、三工河及喀拉扎组中。(4)开阔湖相沉积,以三工河组厚的页岩层序为代表。 砂岩成分逆向反映源区剥蚀顺序。下侏罗统富含泥质岩屑,表示天山上古生界浅变质及沉积层系被剥蚀。自下而上,碎屑中稳定矿物增加,粒度变细,反映源区由于剥蚀而后退。中—上侏罗统砂岩成分演化方向不同于下侏罗统,可能与三工河组沉积末期盆地边缘构造回春有关。在Q-F-L三角图中,侏罗系样品大都落在构造区之间,反映陆相盆地充填物的混合来源。下—中侏罗统的煤既有原地生成,亦有重要的他生类型。 相似文献
993.
本文通过对和田河和克里雅河流域不同类型沙物质的矿物和化学成分研究,揭示了河流沙、沙丘沙和地层沙的矿物成分和化学成分存在的差异,指出这种差异是有关元素及化合物(或矿物)在不同环境下具有不同地球化学行为的结果。 相似文献
994.
Chemical composition of saline and subsaline lakes of the northern Great Plains,western Canada 总被引:2,自引:0,他引:2
William M. Last 《International Journal of Salt Lake Research》1992,1(2):47-76
The northern Great Plains of Canada stretch from the Precambrian Shield near Winnipeg, Manitoba, westward for ∼1,700 km to
the Rocky Mountains foothills. This vast region of flat to gently rolling terrain contains a very large number of salt lakes.
Major ion chemical data on ∼500 of them are available. Although the average brine (salinity, 37 ppt) is a Na+−SO4
2− type of water, the lakes exhibit a wide range of salinities and ionic compositions. This diversity is confirmed by Q-mode
cluster analysis; it identified thirteen major water chemistry types. Most ions display distinct trends, both spatially and
with increasing salinity. All dissolved components increase with increasing salinity, but at different rates. The relative
proportions of Ca2+ and HCO3
−+CO3
2− ions show a strong decrease with increasing brine salinity, whereas SO4
2− ions increase with increasing salinity. The ionic proportions of Na+, Mg2+, K+ and Cl− exhibit no significant relationship with salinity. R-mode factor analysis of the lake water chemistry, combined with selected
environmental parameters, identifies groundwater composition, climate, and the elevation of the lake within the drainage system
as most important in controlling brine chemistry and salinity on a regional basis. Variability in source of ions, reaction
processes and products are undoubtedly key factors in helping to explain brine chemistry of an individual basin or variation
from a local perspective, but these factors are generally poorly understood and not quantified on a regional basis.
Palliser Triangle Global Change Project Contribution Number 3. 相似文献
995.
A. Carrara M. Cardinali R. Detti F. Guzzetti V. Pasqui P. Reichenbach 《地球表面变化过程与地形》1991,16(5):427-445
Geographical Information Systems (GIS) and numerical cartography may greatly facilitate the development and use of statistical models for the assessment of regional landslide hazard. From a small drainage basin located in Central Italy, relevant geological and geomorphological factors were collected and processed by applying GIS technology. In particular, modules were used which both generate high-fidelity digital terrain models and automatically partition the terrain into main slope-units. The resulting information was then analysed by discriminant analysis which enabled landslide hazard and risk to be evaluated in each slope-unit. Although not lacking drawbacks, the method proved to be a feasible and cost-effective approach to landslide susceptibility assessment and mapping. 相似文献
996.
997.
二叠纪海相碳酸盐的锶同位素演化及其意义 总被引:4,自引:0,他引:4
本文从沫阳和熊家场剖面二叠纪海相碳酸盐和玄武岩的锶同位素变化出发,讨论了碳酸盐的锶同位素组成与峨嵋山玄武岩喷发之间的关系,以及玄武岩中海相碳酸盐的锶同位素贫化原因,指出海相碳酸盐的锶同位素组成可作为了解地球构造演化的工具。 相似文献
998.
999.
Consideration of sources and growth dynamics of aerosols has led to the conclusion that there may be a distribution or variation of chemical composition and physical structure among atmospheric aerosol particles as a function of size, and within a narrow size range as well. A mathematical representation of these particle properties in terms of an additional dimension to the number size distribution is described. Examples of the relevance of this aspect of aerosol characterization for physical and chemical processes in the atmosphere are discussed. A review of the available techniques shows that several methods are available which can and have provided quantitative results on the distribution of particle properties. Examples of data from the literature have been selected and are presented as three-dimensional distributions illustrating the wide range of particle properties which may exist in narrow size intervals. An evaluation of these results reiterates the value of taking the distribution of particle properties in the atmosphere into account for sampling and modeling purposes. 相似文献
1000.