全文获取类型
收费全文 | 3609篇 |
免费 | 678篇 |
国内免费 | 926篇 |
专业分类
测绘学 | 377篇 |
大气科学 | 657篇 |
地球物理 | 1048篇 |
地质学 | 1526篇 |
海洋学 | 740篇 |
天文学 | 9篇 |
综合类 | 498篇 |
自然地理 | 358篇 |
出版年
2024年 | 18篇 |
2023年 | 36篇 |
2022年 | 87篇 |
2021年 | 114篇 |
2020年 | 137篇 |
2019年 | 180篇 |
2018年 | 133篇 |
2017年 | 173篇 |
2016年 | 161篇 |
2015年 | 184篇 |
2014年 | 215篇 |
2013年 | 255篇 |
2012年 | 212篇 |
2011年 | 208篇 |
2010年 | 197篇 |
2009年 | 230篇 |
2008年 | 199篇 |
2007年 | 264篇 |
2006年 | 202篇 |
2005年 | 182篇 |
2004年 | 213篇 |
2003年 | 178篇 |
2002年 | 138篇 |
2001年 | 162篇 |
2000年 | 147篇 |
1999年 | 114篇 |
1998年 | 108篇 |
1997年 | 118篇 |
1996年 | 112篇 |
1995年 | 121篇 |
1994年 | 85篇 |
1993年 | 66篇 |
1992年 | 69篇 |
1991年 | 43篇 |
1990年 | 38篇 |
1989年 | 31篇 |
1988年 | 27篇 |
1987年 | 9篇 |
1986年 | 10篇 |
1985年 | 12篇 |
1984年 | 9篇 |
1983年 | 5篇 |
1982年 | 1篇 |
1981年 | 3篇 |
1979年 | 3篇 |
1978年 | 3篇 |
1976年 | 1篇 |
排序方式: 共有5213条查询结果,搜索用时 15 毫秒
81.
82.
83.
浙北双溪坞群的构造特征及地质意义 总被引:1,自引:0,他引:1
本文在野外地质工作基础上,通过对双溪坞群的岩层对比和构造分析,认为本区的双溪坞群与上覆地层间在构造样式上的存在着较大差异。双溪坞群的章村组和北组具有相似的地质特征,为同一火山放心回的产物。神功运动使早期形成的双溪坞群褶皱造山,开怀 竖线型平臣褶皱构造,并受后期构造的叠加改造,形成轴向北东的叠加褶皱构造格局。 相似文献
84.
华南海西—印支成矿期内,成矿序列完整,类型齐全,矿种繁多,为其它成矿期所莫及。沉积矿床需要稳定的地质背景,层控矿床形成的较有利的地质背景是稳中有动。 相似文献
85.
中国大陆第四纪地壳运动时程 总被引:5,自引:0,他引:5
本文从中国大陆有代表性的青藏高原、黄土高原、三峡地区着手,进行了新构造运动剖析。并结合全国火山活动期次,总结出中国大陆第四纪地壳运动的时程变化。从而为进一步探讨新构造运动特点和规律,为国民经济建设及人类生存环境提供了一定的地质背景资料。 相似文献
86.
P. F. Biagi T. S. Gegechkory E. N. Its P. Manjgaladze V. Sgrigna D. Zilpimiani 《Pure and Applied Geophysics》1990,133(2):317-327
A three-dimensional ultrasonic modelling was used to study the Rayleigh waves reflected from a thin low velocity vertical layer and those transmitted through the same zone. The reflection and transmission coefficients of the Rayleigh waves have been calculated by an approximate method based on the Green function technique. Nonrigid contact boundary conditions were used for the low velocity layer modelling. A rather good correspondence between the theoretical and experimental absolute values of the reflection and the transmission coefficients was obtained. Some discrepancies between experimental and theoretical results, in particular with regard to phase shifts, may be explained by a certain inadequacy of the theoretical model to the low velocity layer investigated by the ultrasonic modelling. 相似文献
87.
A simplified procedure for evaluating aseismic stability of slope subjected to earthquake shaking, in which the effect of dynamic shear strength and time-history stress on the yielding angular acceleration of sliding block is taken into account, is presented. The fundamental feature of this procedure is the dynamic shear strength. The numerical computations are performed by using the proposed method. It is shown that the computed sliding displacement for a given core dam, with either method of dynamic shear strength properly considered, is more rational compared with the conventional computational results based on static shear strength. 相似文献
88.
Thermal evolution of the orogenic lower crust during exhumation within a thickened Moldanubian root of the Variscan belt of Central Europe 总被引:4,自引:5,他引:4
At the eastern margin of the Bohemian Massif (Variscan belt of Central Europe), large bodies of felsic granulite preserve mineral assemblages and structures developed during the early stages of exhumation of the orogenic lower continental crust within the Moldanubian orogenic root. The development of an early steep fabric is associated with east–west-oriented compression and vertical extrusion of the high-grade rocks into higher crustal levels. The high-pressure mineral assemblage Grt-Ky-Kfs-Pl-Qtz-Liq corresponds to metamorphic pressures of ∼18 kbar at ∼850 °C, which are minimum estimates, whereas crystallization of biotite occurred at 13 kbar and ∼790 °C during decompression with slight cooling. The late stages of the granulite exhumation were associated with lateral spreading of associated high-grade rocks over a middle crustal unit at ∼4 kbar and ∼700 °C, as estimated from accompanying cordierite-bearing gneisses. The internal structure of a contemporaneously intruded syenite is coherent with late structures developed in felsic granulites and surrounding gneisses, and the magma only locally explored the early subvertical fabric of the felsic granulite during emplacement. Consequently, the emplacement age of the syenite provides an independent constraint on the timing of the final stages of exhumation and allows calculation of exhumation and cooling rates, which for this part of the Variscan orogenic root are 2.9–3.5 mm yr−1 and 7–9.4 °C Myr−1 , respectively. The final part of the temperature evolution shows very rapid cooling, which is interpreted as the result of juxtaposition of hot high-grade rocks with a cold upper-crustal lid. 相似文献
89.
In ground improvement projects with prefabricated vertical drains, the duration of the preloading period is set in advance
based on the predetermined time rate of consolidation of the compressible layer. If prediction is accurately done, the required
degree of consolidation is met at the pre-determined preloading time. As such, there is a requirement for in-situ tests to be carried out just prior to the removal of surcharge to assess the degree of consolidation of the improved ground.
In-situ tests were carried out after 23 months of surcharge loading at the In-Situ Test Site within the Changi East Reclamation Project in the Republic of Singapore. In-situ testing works in this research study comprises the use of field vane shear, piezocone, flat dilatometer and self-boring pressuremeter.
The in-situ tests were carried out to determine the shear strength and degree of consolidation of the Singapore marine clay at Changi
after 23 months of surcharge loading. The In-Situ Test Site consisted of a Vertical Drain Area as well as an untreated Control Area. Both areas were located adjacent to each
other and were surcharged simultaneously to the same level and surcharge left in place for a period of 23 months. Comparison
was made between the in-situ test results of the Vertical Drain Area and the untreated Control Area. 相似文献
90.