首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   985篇
  免费   215篇
  国内免费   298篇
测绘学   19篇
大气科学   270篇
地球物理   268篇
地质学   582篇
海洋学   103篇
天文学   24篇
综合类   39篇
自然地理   193篇
  2024年   2篇
  2023年   17篇
  2022年   55篇
  2021年   49篇
  2020年   61篇
  2019年   72篇
  2018年   51篇
  2017年   52篇
  2016年   55篇
  2015年   46篇
  2014年   63篇
  2013年   85篇
  2012年   70篇
  2011年   59篇
  2010年   42篇
  2009年   71篇
  2008年   79篇
  2007年   68篇
  2006年   68篇
  2005年   45篇
  2004年   60篇
  2003年   52篇
  2002年   32篇
  2001年   29篇
  2000年   29篇
  1999年   32篇
  1998年   27篇
  1997年   19篇
  1996年   24篇
  1995年   15篇
  1994年   12篇
  1993年   18篇
  1992年   6篇
  1991年   10篇
  1990年   5篇
  1989年   4篇
  1988年   3篇
  1987年   1篇
  1986年   2篇
  1985年   2篇
  1984年   1篇
  1983年   3篇
  1980年   1篇
  1978年   1篇
排序方式: 共有1498条查询结果,搜索用时 15 毫秒
171.
南黄海陆架区15ka以来的古气候事件与环境演变   总被引:10,自引:0,他引:10  
于1986-1994年间,陆续对南黄海7个柱状样品进行了孢粉分析研究,结合^14C测年数据,参考古地磁、热释光测年等分析资料,以其中3个主要岩芯剖面资料为代表,论述了南黄海陆架区15ka以来的古气候环境演变。结果表明,在第四纪末次冰期冰消期中,气候曾剧烈波动,并逐渐由晚冰期向冰后期过渡。这一演变特点与全球气候背景下的中国东部地理环境相关。同时识别出3个短期降温和两个升温事件:其中A1亚带冷期出现在  相似文献   
172.
近50 年华南地区极端强降水频次的时空变化特征   总被引:7,自引:2,他引:7  
利用华南地区110 个台站1961—2008 年逐日降水资料,采用百分位法定义各站极端强降水事件的阈值,运用线性回归、M-K 突变检验、正交函数分解(EOF)、旋转经验正交函数分解(REOF)等方法,对华南地区年极端强降水频次的时空变化特征进行分析。结果表明:在空间分布上,年极端强降水频次在华南中部较大、广东沿海和广西西部内陆较小;华南极端强降水频次有3 个主要的空间异常模态,一致性异常特征是华南极端强降水频次分布的最主要空间模态,而东、西反向和南、北反向变化模态也是比较重要的异常模态。在时间分布上,华南的极端强降水事件主要发生在夏半年,夏半年极端强降水频次占全年总频次的83.7%;1960 年代和1980 年代极端强降水频次较少,从1980 年代中后期起,极端强降水频次有由少变多的趋势。华南区域各站极端强降水频次气候倾向率不一致,除中部呈减少趋势外,其余大部呈上升趋势,华南区域各站极端强降水频次的平均序列也呈上升趋势,但上升趋势不显著。华南极端强降水频次从区域变化特征上可分为6 个主要区域,分别具有不同的年际变化趋势,其中有3 个区域的代表站先后发生了显著增多的突变现象。   相似文献   
173.
Multi-stage differential transgression controls sequence architecture and its sedimentary type and distribution during the tectonic evolution of lacustrine rift basin. Combined with the seismic data of the Baxian sag as well as drilling,logging,core and paleontological materials from 800 exploration wells,the study targeted the Members 1 and 3 of the Shahejie Formation to analyze sequence architecture and sedimentological difference within the sequence framework during the differential lake transgression,based on the investigation of the Paleogene lake basin evolution. The results showed that the fault slope-break slope architecture was well developed with back-stepping deltas and fan deltas during the slow lake transgression of the Member 3 of Shahejie Formation,in which forms thick high quality source rocks. The flexural-gentle slope architecture was well developed with mixed beach bar and small scale nearshore subaqueous fans(fan deltas)during the rapid transgression of the Member 1 of Shahejie Formation. The differential subsidence controlled the sequence architecture,paleogeomorphology and provenance supply,regulating the spatial lithological distribution. And there are significant differences in sequence architecture and sedimentary system during the different evolution stages of the lake basin. On this basis,the response model of sedimentary system characteristics under differential lacustrine transgression is established,which can be used for reference for oil and gas exploration,especially for lithologic oil and gas reservoir in the same type of basin.  相似文献   
174.
MDD模式与快速冷却事件   总被引:6,自引:0,他引:6  
陈文寄  李齐 《地学前缘》1999,6(4):371-377
MDD 模式(Multiple Diffusion Domain model) 是Dodson 模式的扩展,它可以从一个钾长石样品分析中,得到温度在≤350 ~150 ℃之间的一条连续的冷却曲线,因此,MDD 模式的一个突出贡献是对快速冷却事件的定量制约。冈底斯岩带与哀牢山- 红河剪切带中新世的快速冷却事件与构造含义是利用这一模式进行研究的成功实例,它不仅定量厘定了快速冷却事件的时间,证实了其存在的普遍性,而且明确指出了中新世印度和欧亚板块碰撞后岩石圈质量转移过程的时间序列,定量地指出了冈底斯岩带逆冲抬升导致的地壳增厚与沿哀牢山- 红河剪切带地壳块体的侧向挤出在时间上的同步性和差异性  相似文献   
175.
辽西四合屯脊椎动物集群死亡事件:火山爆发的灾变记录   总被引:6,自引:1,他引:5  
辽西北票以ConfuciusornisSinosauropteryxZhangheotherium为代表的四合屯脊椎动物组合发现于义县组下部湖相沉积中,时代为早白垩世Barremian中期(J—K界线144 Ma)或Valanginian晚期(J—K界线136 Ma)。化石包括鱼类、两栖类、爬行类、鸟类和哺乳类及无脊椎动物和被子植物,孔子鸟类群和具“羽毛”的小型兽脚类恐龙共生。野外发掘表明,化石完整地保存骨骼硬体及羽毛、食物、胃石、卵等软体及生理组织,确认多次非正常生物集群死亡事件。在四合屯发掘剖面上,含化石正常沉积的湖相页岩与火山喷发事件形成的沉凝灰岩互层,中酸性火山爆发形成的环境突变效应是导致脊椎动物集群死亡的主要原因。  相似文献   
176.
1INTRODUCTIONTheUpperMississippiRiver(U-MR)extendsfromCairo,Illinois,totheheadwaiersoftheMississippiRiver(MR)nearLakeltascainMinnesota.Theentirerivercanbedividedintotwomajorreachesf1)theUpperMississippiRiverfromheadwaierstoCairo,Illinois,totheconfluenceoftheOhioRiverwiththeMississippiRiver,and2)theLowerMississippiRiver(LMR)fromCairo,Illinois,totheGulfofMexico.FigureIshowsthisdivision,includingabreakdownoftheentireriverintofive(5)segmentswhichwillbedescribedinasubsequentsectio…  相似文献   
177.
Recent technological advances in geosensor networks demand new models of distributed computation with dynamic spatial information. This paper presents a computational model of spatial change in dynamic regions (such as may be derived from discretizations of continuous fields) founded on embeddings of graphs in orientable surfaces. Continuous change, connectedness and regularity of dynamic regions are defined and local transition rules are used to constrain region evolution and enable more efficient inference of a region's state. The model provides a framework for the detection of global high‐level events based on local low‐level ‘snapshot’ spatiotemporal data. The approach has particular relevance to environmental monitoring with geosensor networks, where technological constraints make the detection of global behaviour from local conditions highly advantageous.  相似文献   
178.
地震数据中发育的层间多次波是影响速度分析和偏移成像的精度和可靠性的关键.通常情况下,层间多次波的动校正量、叠加速度和频率与一次波并无明显差异,从而对识别、预测和压制多次波带来了极大挑战.传统虚同相轴方法基于物理图像和定性公式,其预测的层间多次波振幅和相位精度难以满足实际需求,造成了其对匹配算法的过度依赖.本文针对传统虚同相轴方法的理论缺陷和计算精度问题,通过理论推导得到了新的自适应虚同相轴方法.相比于传统方法,自适应虚同相轴方法能够显著提高压制多次波能力,同时减少对匹配算法的依赖.本文给出了自适应虚同相轴方法的推导过程,并运用一维和二维模型算例验证了方法相较于传统虚同相轴方法的多次波预测精度优势.通过在PLUTO模型和实际陆地地震数据上的应用实例,证明了本文新研究的自适应虚同相轴方法对去除层间多次波,恢复并突出目标储层同相轴,提高地震成像分辨率的显著作用.  相似文献   
179.
While isolation can provide significantly enhanced performance compared to fixed‐base counter parts in design level or even maximum considered level earthquakes, there is still uncertainty over the performance of isolation systems in extreme events. Researchers have looked at component level stability of rubber bearings and on the effect of moat impact on behavior of structures isolated on general bilinear isolators. However, testing of triple friction pendulum (TFP) sliding bearings has not been done dynamically or incorporated into a building system. Here, one‐third scale laboratory tests were conducted to on a 2‐story 2‐bay TFP‐isolated structure. Input motions were increasingly scaled until failure occurred at the isolation level. As the superstructure was designed with a yield force equivalent to the force of the bearing just at their ultimate displacement capacity, there was minimal yielding. A numerical model is presented to simulate the isolated building up to and including bearing failure. Forces transferred to the superstructure in extreme motions are examined using both experimental and numerical data. Additionally, the effect of the hardening stage of the TFP bearing is evaluated using the numerical model, finding slight benefits.  相似文献   
180.
Geomorphic effectiveness has been an influential concept in geomorphology since its introduction by Reds Wolman and John Miller in 1960. It provided a much needed framework to assess the significance of an event by comparing event magnitude to the resultant geomorphic effects. Initially, this concept was applied primarily in river channels, under the linear assumption that geomorphic responses to similarly sized flood events will be consistent. Numerous authors have since attempted to quantify a direct, proportional relationship between event magnitude and different forms of geomorphic response in a variety of geomorphic settings. In doing so, these investigations applied an array of metrics that were difficult to compare across different spatiotemporal scales, and physiographic and geomorphic environments. Critically, the emergence of other geomorphic concepts such as sensitivity, connectivity, thresholds, and recovery has shown that relationships between causes (events) and geomorphic effects (responses) are often complex and non‐linear. This paper disentangles the complex historical development of the geomorphic effectiveness concept and reviews the utility of various metrics for quantifying effectiveness. We propose that total energy (joules) is the most appropriate metric to use for quantifying the magnitude of disturbance events (cause) and volumetric sediment flux associated with landform modification is the most appropriate metric for quantifying geomorphic effects. While both metrics are difficult to quantify, they are the only ones which facilitate comparison across a range of spatiotemporal scales (comparability) in a variety of geomorphic environments (flexibility). The geomorphic effectiveness concept can continue to be useful provided that geomorphologists use flexible and comparable metrics. Today, geomorphologists are better prepared to consider the influence of non‐linear processes on determinations of geomorphic effectiveness, allowing investigators to not only determine if a disturbance event was effective but also to explain why or why not. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号