全文获取类型
收费全文 | 5937篇 |
免费 | 1286篇 |
国内免费 | 1964篇 |
专业分类
测绘学 | 204篇 |
大气科学 | 1148篇 |
地球物理 | 797篇 |
地质学 | 2570篇 |
海洋学 | 3378篇 |
天文学 | 29篇 |
综合类 | 535篇 |
自然地理 | 526篇 |
出版年
2024年 | 33篇 |
2023年 | 95篇 |
2022年 | 216篇 |
2021年 | 260篇 |
2020年 | 269篇 |
2019年 | 333篇 |
2018年 | 276篇 |
2017年 | 245篇 |
2016年 | 269篇 |
2015年 | 343篇 |
2014年 | 398篇 |
2013年 | 460篇 |
2012年 | 369篇 |
2011年 | 402篇 |
2010年 | 342篇 |
2009年 | 444篇 |
2008年 | 353篇 |
2007年 | 412篇 |
2006年 | 453篇 |
2005年 | 369篇 |
2004年 | 322篇 |
2003年 | 324篇 |
2002年 | 283篇 |
2001年 | 274篇 |
2000年 | 238篇 |
1999年 | 230篇 |
1998年 | 200篇 |
1997年 | 168篇 |
1996年 | 161篇 |
1995年 | 127篇 |
1994年 | 126篇 |
1993年 | 103篇 |
1992年 | 62篇 |
1991年 | 46篇 |
1990年 | 40篇 |
1989年 | 32篇 |
1988年 | 26篇 |
1987年 | 17篇 |
1986年 | 8篇 |
1985年 | 21篇 |
1984年 | 8篇 |
1983年 | 8篇 |
1982年 | 9篇 |
1981年 | 8篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1976年 | 1篇 |
1954年 | 1篇 |
排序方式: 共有9187条查询结果,搜索用时 781 毫秒
221.
222.
中下扬子区二叠系露头层序地层研究 总被引:15,自引:1,他引:15
按新近国际年代地层划分方案(ICS,2000),下扬子区二叠纪地层自下向上分为3统,9阶和相对应的华南传统6阶划分。二叠系从阿瑟尔阶至长兴阶(44Ma)共划分出14个三级层序,每个三级层序平均时限约为3.14Ma,其中“紫松阶”)相当阿瑟尔+2/3萨克马尔阶)1个(船山组中上部)、“隆林阶、(相当1/3萨克马尔阶+阿丁斯克阶)2个(分别对应船山组上部和梁山组或镇江组)、“栖霞阶”(相当库班甘德阶+1/3罗德阶)3个(栖霞组),“茅口阶”(相当于2/3罗德阶+沃德阶+卡皮丹阶)4个(孤峰组,茅口组,堰桥组,银屏组和武穴组),吴家坪阶2个(龙潭组或吴家坪组),长兴阶2个(长兴组或大隆组);共归并为4个层序组(sequence set)。 相似文献
223.
224.
Darrell S. Kaufman Gary O'Brien Jim I. Mead Jordon Bright Paul Umhoefer 《Quaternary Research》2002,58(3):329
One of the most intriguing episodes in the Quaternary evolution of the Grand Canyon of the Colorado River, Arizona, was the development of vast lakes that are thought to have backed up behind lava erupted into the gorge. Stratigraphic evidence for these deep lava-dammed lakes is expectedly sparse. Possible lacustrine deposits at six areas in the eastern canyon yielded no compelling evidence for sediment deposited in a deep lake. At two of the sites the sediment was associated with late Quaternary spring-fed pools and marshes. Water-lain silt and sand at lower Havasu Creek was deposited 3000 cal yr ago. The deposit contains an ostracode assemblage similar to that living in the modern travertine-dammed pools adjacent to the outcrop. The second deposit, at Lees Ferry, formed in a spring-fed marsh 43,000 cal yr ago, as determined by 14C and amino acid geochronology. It contains abundant ostracode and mollusk fossils, the richest assemblages reported from the Grand Canyon to date. Our interpretation of these sediments as spring-fed deposits, and their relative youth, provides an alternative to the conventional view that deposits like these were formed in deep lava-dammed lakes that filled the Grand Canyon. 相似文献
225.
Based on Coastal Zone Color Scanner data from November 1978 through December 1981, the seasonal cycle of phytoplankton pigment
in the upper part of the euphotic zone is established for the offshore Laccadive Sea. Year-round, the pigment content is low
and the seasonal range is small, following the pattern of the nutrient-poor Arabian Sea to the west. Apparently, indigenous
phytoplankton blooms are absent. July and August, however, were poorly studied because of cloud cover. Interannual differences
during the northeast monsoon and the spring intermonsoon periods are minor. The abundant phytoplankton caused by the upwelling
off India during the southwest monsoon remains essentially restricted to the shelf, but there are occasional large, zonal
outbreaks into the Laccadive Sea, as well as others advected to the south of India. Visual inspection of the raw CZCS scenes
for June through November 1982–1985, with almost no data until August or even September, shows such outbreaks of pigment-rich
water to be common. Inspection of monthly SeaWiFS images for 1997 through part of 2001 confirms the absence of indigenous
phytoplankton blooms. 相似文献
226.
Yugo Nakamura Yoshinori Katayama Kazuomi Hirakawa 《Journal of Volcanology and Geothermal Research》2002,114(3-4)
Refractive indices of incompletely hydrated tephra glasses vary widely. Thus, glass refractive index is not a practical indicator for identifying Holocene tephras. Hydration near the surface of tephra glass shards can be removed by either hydrofluoric acid treatment or annealing for 12 h at 400°C. The annealing procedure is a particularly reliable and simple way to dehydrate tephra glasses. Standard deviations (s) of refractive indices for glasses after 12 h annealing are small (s=0.0014–0.0018), in contrast with untreated glasses (s=0.0034–0.0405). The refractive indices of dehydrated tephra glasses are 0.006–0.014 lower than those of the untreated (hydrated) glasses. Using the 400°C 12-h annealing procedure, values for the refractive indices of eight Holocene tephras in Hokkaido were obtained. These refractive indices are useful indicators for identification and correlation of Holocene tephras. 相似文献
227.
Antonio Longinelli Paola IacuminMichele Ramigni 《Earth and Planetary Science Letters》2002,203(1):445-459
Belemnite guards of Cretaceous and Jurassic age were found to contain varying amounts of quartz deposited both on the external surface and inside the rostrum. The oxygen isotopic composition of coexisting carbonate, quartz and phosphate from the same rostrum was measured according to well-established techniques. None of these compounds showed isotopic values in equilibrium with one another. Assuming δ18O values of the diagenetic water within the range of meteoric waters, the δ18O(SiO2) yield temperatures in agreement with the apparent secondary origin of this phase. The δ18O(CO32−) range, with a certain continuity, between −10.8 and +0.97 PDB-1 with most of the intermediate values being within the range of the carbonate isotopic values of Mesozoic fossils. The most positive isotopic results obtained from phosphate are close to +23/+24‰ (V-SMOW). They can hardly be related to a secondary origin of the phosphate, or to the presence of diagenetic effects, since these results are among the most positive ever measured on phosphate. As far as we know there is no widespread diagenetic process determining an 18O enrichment of phosphate. The very low concentration of phosphate did not allow the determination of its mineralogical composition. All the available δ18O(PO43−) values from belemnite and non-belemnite fossils of marine origin of Tertiary and Mesozoic age are reported along with the newly measured belemnites. The following conclusions may be drawn from the data reported: (1) the pristine oxygen isotope composition of fossil marine organisms (either carbonate or phosphate) may easily undergo fairly large changes because of oxygen isotope exchange processes with diagenetic water; this process is apparent even in the case of geologically recent fossils; (2) the δ18O(PO43−) of belemnite rostra seems to be, at least in the case of the most positive results, in isotopic equilibrium with environmental water because of the similarity between the results from Cretaceous belemnites and the results from Cretaceous and Lower Tertiary pelecypods and fish teeth; 3) if so, the only feasible interpretation that can be suggested for the 18O enriched data is the possibility of a relatively large variation of the oxygen isotopic composition of ocean paleowater from Jurassic to recent time. 相似文献
228.
雄关漫道真如铁——论中国油气二次创业 总被引:17,自引:19,他引:17
半个多世纪以来,中国经历了油气资源的第一次创业,在祖国大陆和近海大陆架地区的新生代陆相碎屑岩沉积盆地中,发现了一批油气田,使原油年产量达1.67亿吨,位居世界第五,天然气疸这241亿立方米,居世界第十五位,成绩是巨大的,但是,1993年开始进口原油3000万吨,2000年进口原油7200万吨,严重影响国家经济建设,而且这种趋势还在不断发展,预测2010年将进口原油1亿吨,天然气200亿立方米,那么,中国油气资源的出路何在?作者指出,从中国大地构造演化来看,前新生代海相残留盆地还有巨大的油气潜力,尽管其勘探的难度是世界级的,但是,只要我们切实地依靠科学技术,进行油气资源的二次创业,困难上,在实践中克服困难,就可以发现更多的石油天然气,支持国家经济建设的持续发展。 相似文献
229.
Water resources for agricultural development and landscape enhancement in Kuwait are very scarce; the quality is saline (brackish), and the soil texture is sandy, incapable of holding nutrients and moisture. Most of the rainfall in Kuwait either evaporates due to the high temperatures or percolates through the soil. The rainfall is not sufficient to recharge the underground water supply. A variety of alternative water sources have been studied, including seawater desalination and wastewater treatment. Wastewater treatment proved to be convenient due to the relatively low salinity detected in the treated water. Furthermore, the amount of wastewater is expected to increase as more residential areas are connected to the sewage system as the population increases.
The development of a greenery plan for Kuwait requires intensive water management. This goal can be achieved through manpower training in landscape development, selection of plants tolerant to arid environments, usage of appropriate irrigation and drainage systems, promotion of greenery programs within public and the governmental agencies for their direct participation in urban area beautification, and extension of wastewater treatment techniques. 相似文献
230.
江苏淤泥质潮滩对海平面变化的形态响应 总被引:9,自引:0,他引:9
通过对江苏滨海平原淤泥质潮滩1980年以来19个固定潮滩断面112个测次滩面高程测量的统计分析,探讨典型淤泥质潮滩剖面形态对海平面变化的形态响应过程。结果表明,典型淤涨岸段海平面上升,多年平均潮位线以上滩面仍将淤积加高,但淤高幅度除多年平均高潮线附近滩面相对较大外,其余均较小,表明随海平面上升该滩带总体淤积速率将趋于减小;与此相反,多年平均潮位线以下滩面则趋于蚀低,且侵蚀强度较大,表明该滩带的侵蚀有加剧趋向,最终滩面总体形态将因上带不断淤高和下带不断蚀低而逐渐变陡,剖面上凸形态的曲率不断加大。曲型侵蚀岸段,海平面上升的效应则相反,海平面上升,多年平均潮位线以上滩面强烈蚀低;而多年平均潮位线以下滩面则强烈淤积加高,剖面的上凹形态最终将因上带不断蚀低和下带不断淤高而趋于平直。 相似文献