全文获取类型
| 收费全文 | 13501篇 |
| 免费 | 3031篇 |
| 国内免费 | 4676篇 |
专业分类
| 测绘学 | 2432篇 |
| 大气科学 | 2116篇 |
| 地球物理 | 2198篇 |
| 地质学 | 7984篇 |
| 海洋学 | 3098篇 |
| 天文学 | 244篇 |
| 综合类 | 1197篇 |
| 自然地理 | 1939篇 |
出版年
| 2024年 | 111篇 |
| 2023年 | 316篇 |
| 2022年 | 779篇 |
| 2021年 | 951篇 |
| 2020年 | 803篇 |
| 2019年 | 914篇 |
| 2018年 | 786篇 |
| 2017年 | 730篇 |
| 2016年 | 780篇 |
| 2015年 | 885篇 |
| 2014年 | 863篇 |
| 2013年 | 1103篇 |
| 2012年 | 1184篇 |
| 2011年 | 1180篇 |
| 2010年 | 1172篇 |
| 2009年 | 1105篇 |
| 2008年 | 1165篇 |
| 2007年 | 1033篇 |
| 2006年 | 1140篇 |
| 2005年 | 846篇 |
| 2004年 | 660篇 |
| 2003年 | 417篇 |
| 2002年 | 487篇 |
| 2001年 | 471篇 |
| 2000年 | 362篇 |
| 1999年 | 221篇 |
| 1998年 | 107篇 |
| 1997年 | 92篇 |
| 1996年 | 69篇 |
| 1995年 | 75篇 |
| 1994年 | 64篇 |
| 1993年 | 59篇 |
| 1992年 | 37篇 |
| 1991年 | 30篇 |
| 1990年 | 27篇 |
| 1989年 | 14篇 |
| 1988年 | 19篇 |
| 1987年 | 20篇 |
| 1986年 | 9篇 |
| 1985年 | 14篇 |
| 1984年 | 16篇 |
| 1983年 | 16篇 |
| 1982年 | 10篇 |
| 1981年 | 6篇 |
| 1979年 | 10篇 |
| 1978年 | 4篇 |
| 1964年 | 3篇 |
| 1957年 | 5篇 |
| 1954年 | 9篇 |
| 1928年 | 3篇 |
排序方式： 共有10000条查询结果，搜索用时 15 毫秒
21.
In view of rapid developments in iterative solvers, it is timely to re‐examine the merits of using mixed formulation for incompressible problems. This paper presents extensive numerical studies to compare the accuracy of undrained solutions resulting from the standard displacement formulation with a penalty term and the two‐field mixed formulation. The standard displacement and two‐field mixed formulations are solved using both direct and iterative approaches to assess if it is cost‐effective to achieve more accurate solutions. Numerical studies of a simple footing problem show that the mixed formulation is able to solve the incompressible problem ‘exactly’, does not create pressure and stress instabilities, and obviate the need for an ad hoc penalty number. In addition, for large‐scale problems where it is not possible to perform direct solutions entirely within available random access memory, it turns out that the larger system of equations from mixed formulation also can be solved much more efficiently than the smaller system of equations arising from standard formulation by using the symmetric quasi‐minimal residual (SQMR) method with the generalized Jacobi (GJ) preconditioner. Iterative solution by SQMR with GJ preconditioning also is more elegant, faster, and more accurate than the popular Uzawa method. Copyright © 2003 John Wiley & Sons, Ltd. 相似文献
22.
23.
B. Hou L.A. Frakes M. Sandiford L. Worrall J. Keeling N.F. Alley 《Sedimentary Geology》2008,203(1-2):112-130
The Eucla Basin including the vast Nullarbor Plain lies on the margins of the Yilgarn, Musgrave and Gawler cratons in southern Australia and owes its distinctive landscape to a unique set of interactions between eustatic, climatic and tectonic processes over the last ~ 50 Ma. Understanding of the history of the basin and the palaeovalleys that drained from the surrounding cratons are important because they contain major mineral deposits, and the sediments derived from them contain remobilised gold, uranium, and heavy minerals. In particular, a remarkably preserved palaeoshoreline sequence along the north-eastern margin of the Eucla Basin is highly prospective for heavy mineral placer deposits. The record of marine, marginal marine, estuarine, fluvial and lacustrine environments, as constrained mainly by an extensive borehole dataset, reflects major depositional events during the Palaeocene–Early Eocene, Middle–Late Eocene, Oligocene–Early Miocene, Middle Miocene–Early Pliocene and Pliocene–Quaternary. These events reflect the key role of eustatic sea-level variation which, during highstands, inundated the craton margins, flooding palaeovalleys to up to 400 km inboard of the present coastline. However, a systematic eastward migration of the depocentre across the Eucla Basin during the Neogene, together with apparent flow reversals in a number of palaeovalley systems draining the Gawler Craton, suggest that the Eucla Basin has also been subject to differential vertical movements, expressed as a west-side up, east-side down tilting of ~ 100–200 m. This differential movement forms part of a broader north-down–southwest-up dynamic topographic tilting of the Australian continent associated with relatively fast (6–7 cm/yr) northward plate motion since fast spreading commenced in the Southern Ocean at ~ 43 Ma. We suggest that the evolving dynamic topography field has played a key role in facilitating development of placer deposits, largely through multistage, eastward reworking of near-shore sequences during highstand transgressive cycles on a progressively tilting platform under the influence of persistent westerly weather systems. 相似文献
24.
电感耦合等离子体质谱法同时测定地下水中硼溴碘 总被引：6，自引：4，他引：2
建立了电感耦合等离子体质谱法同时测定地下水中B、Br、I的方法。选定φ=2%(体积分数)的稀NH3.H2O介质消除碘的记忆效应。采用干扰较少的10B和79Br同位素。B、Br、I在0~10 000 ng/mL呈良好的线性关系。方法的检出限为10B 0.176 ng/mL,79Br 0.876ng/mL,127I 0.132 ng/mL;精密度(RSD,n=12)为10B 2.86%,79Br 3.36%,127I 2.69%;10B的阶梯加标回收率为94.6%~101.5%,79Br为98.3%~104.9%,127I为96.5%~102.0%。 相似文献
25.
赣南崇义县淘锡坑钨矿位于南岭东西向构造带东段,属于以黑钨矿石英脉型为主的钨多金属矿床。矿床形成与燕山期中酸性岩浆作用有密切关系,石英矿脉受一组北西向断裂控制,穿切新元古界。本文在淘锡坑钨矿区3个揭露到花岗岩体顶部的中段（206、106、56中段）采集到岩体顶部云英岩样品,利用40Ar/39Ar同位素定年测得云英岩中的白云母的坪年龄分别为152.7 ± 1.5 Ma（206中段）,153.4 ± 1.3 Ma（106中段）,155.0 ± 1.4 Ma（56中段）。与前人用其他方法测定的花岗岩成岩和成矿年龄几乎一致。花岗岩和云英岩全岩稀土元素均具有M型四分组效应和强烈的Eu亏损特征,反映出花岗质岩浆经历了高度分异演化及其岩体结晶晚期流体/熔体相互作用。综合前人在南岭地区同类矿床的研究资料,可知南岭地区160～150Ma成岩成矿作用主要分布于南岭中-东段,可能为大陆边缘弧后岩石圈伸展的构造动力学背景的产物。 相似文献
26.
27.
甲酸和乙酸稳定碳同位素组成（δ^13C）的分析对环境、食品、制药和自然产品等的研究具有重要的应用价值。但目前尚缺乏有效的测定方法。本研究利用最近出现的针式固相微萃取技术（NeedlEX）,以吹扫．捕集方式对水溶液中的有机酸进行了萃取,然后利用气相色谱．同位素比值质谱联用仪（GC—IRMS）对所萃取的有机酸分子进行了占δ^13C的测定。结果显示,质谱计的信号强度与水溶液中有机酸的浓度存在显著的线性相关关系（R^2〉0．99,P〈0．05）,表明Needl EX对水溶液中有机酸具有稳定的萃取能力。在甲酸与乙酸含量分别不低于300μg／mL与200μg／mL的水溶液中,1000mL的吹扫体积可以使两者δ^13C多次分析结果的相对误差分别保持在3％和1％左右,且整个实验流程没有造成可检测的碳同位素分馏作用。低于这两个浓度界线,则分析误差随浓度的降低迅速增加。本研究虽然是针对水溶液中有机酸δ^13C的测定,其萃取方法对其他水溶性挥发和半挥发有机物δ^13C的分析也同样具有应用价值。 相似文献
28.
29.
30.