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991.
骑马沟铅锌矿赋存于熊耳群条纹状硅质大理岩与火山凝灰岩之间.通过对矿床地质、岩石、矿物组合特征等方面的初步研究,认为该矿床为热水沉积-热液改造成因铅锌矿床,其成矿主要与熊耳期火山岩及火山气液作用有关.这是在河南熊耳群火山岩中首次发现的该类矿床类型. 相似文献
992.
结合一工程实例,通过浸水CBR试验,分析高塑性土在毛细饱水情况下的强度特征,揭示高塑性土的路用特性,并将室内研究成果结合现场工艺试验,研究在不添加外掺剂的前提下,直接利用高塑性土填筑路基的途径和方法。 相似文献
993.
994.
结合煤田地质勘探工程监理工作实际,对煤田地质勘探工程监理与建设工程监理进行了比较,认为煤田地质勘探监理与建筑监理程序基本相同,目的都是提高工程水平,规范工程。但煤田地质勘探专业性较强,与建设工程相比也有许多不同之处,故而有必要建立煤炭地质勘探工程监理规范以指导煤炭地质勘探工程监理工作。 相似文献
995.
哈巴特盖测区1/5万土壤地球化学测量发现了4个异常区,多元素组合异常多分布在黑云母二长花岗岩的内、外接触带上,土壤地球化学异常特征显示本区成矿是多期次的,多元素组合异常在露头矿和盲矿上方均有出现,且异常连续、浓集中心明显,异常的强度和规模大,呈带状、宽带状或面状产出。 相似文献
996.
997.
青云山铜金矿为次火山低温热液矿床,矿区共有6个工业铜金矿体,矿体受断裂及构造蚀变带控制,Ⅰ号矿体为石英脉型,其余皆属构造破碎带蚀变岩型.矿区东矿段天花寨一带的不整合面、西矿段的深部、F37和F3断裂及旁侧次级断裂在走向(倾向)上的变化部位是下一步找矿的有利地段. 相似文献
998.
In this paper, we summarized the characteristics of tropical cyclones (TC) activity over the western North Pacific in 2004 and analyzed their causation. Compared with the normal, the annual frequency of TC in 2004 was slightly higher, tropical cyclones in 2004 had a longer life span and occurred in a concentrated period, the source of TC were situated eastward; in all tracks of TC, the recurvature tracks took up larger proportion, the landfall regions of TC were located northward, which concentrated from East China to Japan. The primary causes were revealed as follows. Firstly, the intensity and area of the western North Pacific subtropical high was stronger and larger than usual respectively, and its ridge was frequently in the form of cells and stretched northwestward. Secondly, the convergence of intertropical convergence zone (ITCZ) was reinforced and the convergence zone moved more eastward than average. Thirdly, the meridionality of the westerlies was larger than average and the cell-shaped ridge formed a saddle region, which is in favor of TC northward motion and recurature. 相似文献
999.
Synergy of multiple geophysical approaches to unravel explosive eruption conduit and source dynamics - A case study from Stromboli 总被引:1,自引:0,他引:1
An effective approach to understanding the dynamics of explosive volcanic eruptions and the conduit systems that drive them is through synergy of multiple data sets. Three data sets that lend themselves to ease of integration are seismic, infrasonic and thermal. Although approaches involving these data have been used to record volcanological phenomena since 1862, 1955 and 1965, respectively, their integrated use has only developed since 1999. When combined, these three data sets allow constraint of shallow system geometry and the dynamics of the explosive events that occur within that system. Using Stromboli volcano (Italy) as a case study, we review the complete range of geochemical and geophysical studies that can be applied. In doing so, we aim to show how integration of these diverse studies allows insights into a plumbing system and the dynamics of the eruptive activity that the system feeds. When combined at Stromboli, these data provide constraint of multiple system parameters including chamber depths, gas and magma fluxes, shallow system magma residence times, explosion source depths, and the rise/ejection velocities of ascending gas slugs and ejecta. In turn, these results allow various conduit and eruption dynamic models to be applied and tested.The persistent and repeated mildly explosive events that characterize Stromboli have been modeled in terms of the coalescence of gas within the magma to form large gas slugs that ascend the remaining portion of the conduit to burst at the free surface. Our integrated seismic, infrasonic and thermal data sets indicate that gas coalescence occurs at a depth of ∼260 m, with a typical event frequency of ∼9/h. Infrasonic and thermal data show the explosion source to be located 20-220 m below the vent. Thermal data give emission velocities for the ejected fragments of 8-20 m/s, which converts to gas jet velocities of 23-39 m/s. Tracking these parameters in space and time shows that, although eruptions at Stromboli can be grouped into two characteristic types (simple and complex-each of which characterizes a particular crater, NE and SW, respectively), events within each type show significant short-term variability. The system does, however, appear robust, maintaining its characteristic strombolian eruption style after significant effusive phases and more energetic explosive events. 相似文献
1000.