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   8894篇
  免费   2054篇
  国内免费   3967篇
测绘学   131篇
大气科学   1455篇
地球物理   1473篇
地质学   10114篇
海洋学   722篇
天文学   25篇
综合类   514篇
自然地理   481篇
  2024年   44篇
  2023年   147篇
  2022年   263篇
  2021年   356篇
  2020年   352篇
  2019年   520篇
  2018年   372篇
  2017年   371篇
  2016年   477篇
  2015年   461篇
  2014年   639篇
  2013年   598篇
  2012年   646篇
  2011年   684篇
  2010年   553篇
  2009年   712篇
  2008年   654篇
  2007年   784篇
  2006年   702篇
  2005年   609篇
  2004年   542篇
  2003年   510篇
  2002年   474篇
  2001年   406篇
  2000年   372篇
  1999年   398篇
  1998年   401篇
  1997年   338篇
  1996年   301篇
  1995年   220篇
  1994年   198篇
  1993年   167篇
  1992年   152篇
  1991年   132篇
  1990年   76篇
  1989年   72篇
  1988年   76篇
  1987年   48篇
  1986年   24篇
  1985年   20篇
  1984年   13篇
  1983年   4篇
  1982年   2篇
  1980年   4篇
  1979年   2篇
  1978年   7篇
  1973年   3篇
  1972年   1篇
  1971年   1篇
  1954年   3篇
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
51.
本文对南海中部陆坡区和海盆区的5个岩芯中的 Si,Al,Fe,Mn,Ca,Mg 和 CaCO_3成分做了分析,并对其分布特征与有关影响因素进行了讨论。受沉积区环境差异的影响,元素的分布具有区域性特征;受海区特定地理位置的影响,元素的分布呈现出过渡性特征(浅海到大洋的过渡);受沉积过程中环境变化的影响,元素的分布展示了周期性变化或旋回性。根据岩芯中元素的分布特征,并参考有关古地磁,氧碳同位素和钙质超微化石的测试分析结果,将本区岩芯划分为14层地球化学层,并将本区划分为两个沉积地球化学区,揭示了早更新世以来本区沉积环境的变化和存在的两种沉积模式。  相似文献   
52.
Rock-magnetic measurements along with grain size, acid-insoluble residue (AIR), organic carbon (OC), CaCO3 and δ18O of the planktonic foraminifers of the sediments were determined for 15 gravity cores recovered from the western continental margin of India. Magnetic susceptibility (MS) values in the surficial sediments reflect the land-derived input and, in general, are the highest in terrigenous sediment-dominated sections of the cores off Saurashtra–Ratnagiri, followed by the sediments off Indus–Gulf of Kachchh and then Mangalore–Cape Comorin.

The down-core variations in mineral magnetic parameters reveal that the glacial sediments off the Indus are characterized by low MS values/S-ratios associated with high AIR-content, low OC/CaCO3 contents and relatively high δ18O values, while those off SW India are characterized by low MS values/high S-ratio% associated with low AIR content, and relatively high OC, CaCO3 and δ18O values. Conversely, the Early Holocene sediments of all cores are characterized by high MS values/S-ratio% associated with high AIR content, low OC, CaCO3 contents and gradually decreased δ18O values. These results imply that during the Last Glacial Maximum (LGM), the cores off northwestern India received abundant continental supply leading to the predominance of eolian/fluvial sedimentation. In the SW region the influence of hinterland flux is less evident during this period, but convective mixing associated with the NE monsoon resulted in increased productivity. During the early Holocene intense SW monsoon conditions resulted in high precipitation on land, which in turn contributed increased AIR content/MS values in the continental margin sediments. A shallow water core off Kochi further suggests that the intense SW monsoon conditions prevailed until about 5 ka. The late Holocene organic-rich sediments of the SW margin of India were, however, subjected to early diagenesis at different intervals in the cores. Therefore, caution is needed when interpreting regional climatic change from down-core changes in sediment magnetic properties.  相似文献   

53.
We investigated the water structure and nutrient distribution in the Suruga Bay from April 2000 to July 2002, especially the Offshore Water, which occupies a large part of the bay. The maximum salinity in the upper 200 m varied between 34.49 and 34.71, indicating a temporal change in the influence of Kuroshio Water on the Offshore Water. Seasonal variation in nutrient concentrations was largest from surface to 50 m. On the other hand, the variance in nutrient concentrations within each season was largest in the subsurface layer of 100–300 m in spring, summer and fall. In the Offshore Water, the change of nutrients was negatively correlated with that of salinity in each season. This suggests that an increasing intrusion of saline water brings about a lower nutrient concentration in the Offshore Water. Likewise, negative correlations were observed between the change of the maximum salinity and chlorophyll a (Δ [chl.a-int])/nutrients integrated in the upper 200 m. Δ[chl.a-int] was significantly correlated with the changes of nitrate and phosphorus, but there were no significant correlations between Δ[chl.a-int] and the change of silicate. These results suggest that the concentrations of chlorophyll a and nutrients in the Offshore Water were decreased due to the increasing intrusion of Kuroshio Water. The Offshore Water is likely to be related to the regulation of primary production by nitrate.  相似文献   
54.
南海北部及广东沿海新生代火山活动   总被引:17,自引:0,他引:17  
调查区新生代火山活动十分活跃。岩性以基性为主,少数属超基性Sr~(87/86)初始值最高0.706189,最低0.703178,陆区和海盆新生代火山岩均来自地幔。 K-Ar年龄最老62.86百万年,最新0.43百万年。从老至新可划分为8个活动期,分别为古新世早期、始新世早期、渐新世末期、中新世中期、中新世晚期、早更新世早期、早更新世晚期和中更新世中期。 海盆与陆区火山活动在岩性、同位素特征、活动时期、喷发方式以及岩浆来源等方面都十分相似,二者属统一的新生代火山岩区。  相似文献   
55.
使用块体混合层模式对一个固定海洋观测站所测的上层海洋之物理特性进行了模拟,结果发现了难以重复观测到的许多物理特征。文章提出了水块混合层模式,着重模拟了扩展湾流体系(EGSS)中的一个水块,在它被海流从佛罗里达海峡(24°N,80°W)带到挪威海(68°N,10°E)的过程中,其物理特性(其中包括温度、盐度、混合层深度和夹卷速度)随时间的变化。模拟结果较好地再现了所观测的物理特性的演化。  相似文献   
56.
用Niiler—Kraus类型的混合层积分模式,对TOGA—COARE强化观测期间由《实验3号》科学考察船观测资料得到的混合层深度和SST在季节内时间尺度的变化进行了模式研究。指出:1.混合层耗散参数与较长时间尺度过程风应力的变化存在着比较好的对应关系;2.模式可以较好的对风场和热通量场在季节内时间尺度的变化作出响应,模拟出季节内时间尺度SST的变化;3.Niiler,-Kraus模式在考虑耗散作用后,可用于海洋季节内时间尺度变化的模式研究。  相似文献   
57.
58.
Scientific sea-floor dredging is currently used in marine geology primarily by the hard-rock community interested in the recovery of basement rock samples from the unsedimented deep ocean floor. The technique has generally been eclipsed by ocean drilling for recovery of sedimentary rocks, because of perceived uncertainties in the location of sampling and in the representativeness of recovered material. This contribution reviews dredging equipment currently in use by marine geological institutions and refers to pinger attachments that allow precise information on the behaviour of the dredge to be telemetered back to the ship. We argue that improvements in ship navigation and transponder navigation at the seafloor, when used in conjunction with surface and/or deeply towed sidescan and swathemapping surveys, now allow for considerably less uncertainty on the location of dredge sampling. Refined sorting criteria for dredge hauls are now also available. Recent comparisons of regional sample recovery by ocean drilling and by dredge sampling indicate that the dredge hauls can usefully supplement the drilling data in the construction of sedimentary and tectonic histories of seafloor areas.  相似文献   
59.
徐清明  穆旭 《海岸工程》1997,16(3):47-54
本文介绍的基岩水下爆破属临近重要建筑物的水下控制爆破。当岩石裂隙发育,且岩面有较厚的石碴覆盖层,其技术难度大,采取的诸如搭钢平台钻孔。塑料套管护孔,以及孔间、排间塑料导爆管雷管接力式微差起爆网路等措施,都是成功之经验,值得今后类似工程推广应用。  相似文献   
60.
Wave induced excess flow of momentum(WIEFM)is the averaged flow of momentum over a wave period due to wave presence,which may also be called 3-D radiation stress.In this paper,the 3-D current equations with WIEFM are derived from the averaged Navier-Stokes equations over a wave period,in which the velocity is separated into the large-scale background velocity,the wave particle velocity and the turbulent fluctuation velocity.A concept of wave fluctuating layer(WFL)is put forward,which is the vertical column from the wave trough to wave ridge.The mathematical expressions of WIEFM in WFL and below WFL are given separately.The parameterized expressions of WIEFM are set up according to the linear wave theory.The integration of WIEFM in the vertical direction equals the traditional radiation stress(namely 2-D radiation stress)given by Longuet-Higgins and Stewart.  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