全文获取类型
收费全文 | 8265篇 |
免费 | 2117篇 |
国内免费 | 2652篇 |
专业分类
测绘学 | 264篇 |
大气科学 | 1576篇 |
地球物理 | 3121篇 |
地质学 | 5024篇 |
海洋学 | 1675篇 |
天文学 | 73篇 |
综合类 | 409篇 |
自然地理 | 892篇 |
出版年
2024年 | 60篇 |
2023年 | 201篇 |
2022年 | 262篇 |
2021年 | 278篇 |
2020年 | 297篇 |
2019年 | 396篇 |
2018年 | 403篇 |
2017年 | 430篇 |
2016年 | 429篇 |
2015年 | 429篇 |
2014年 | 583篇 |
2013年 | 563篇 |
2012年 | 504篇 |
2011年 | 527篇 |
2010年 | 409篇 |
2009年 | 574篇 |
2008年 | 558篇 |
2007年 | 606篇 |
2006年 | 597篇 |
2005年 | 486篇 |
2004年 | 491篇 |
2003年 | 492篇 |
2002年 | 461篇 |
2001年 | 378篇 |
2000年 | 333篇 |
1999年 | 318篇 |
1998年 | 277篇 |
1997年 | 256篇 |
1996年 | 245篇 |
1995年 | 226篇 |
1994年 | 204篇 |
1993年 | 168篇 |
1992年 | 146篇 |
1991年 | 117篇 |
1990年 | 77篇 |
1989年 | 81篇 |
1988年 | 64篇 |
1987年 | 37篇 |
1986年 | 17篇 |
1985年 | 3篇 |
1984年 | 12篇 |
1983年 | 5篇 |
1982年 | 2篇 |
1979年 | 12篇 |
1978年 | 6篇 |
1977年 | 2篇 |
1954年 | 7篇 |
1908年 | 1篇 |
1900年 | 1篇 |
1872年 | 1篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
91.
rmIoxThe averag annual dischaIge of the Zhujiang Xiver is 3. 32 x l0ll m3, which ranks theZhujiang River just end to the Changjiang River in China. The dischnye occutring duringthe fltal m between APril and ffepteTnber accounts for 80% of the yearly total. The Zhu-jiang hiver has a yeaIy sediment load of about 1 x l08 tons, which also concentrates in theM arn (Zhao, l990; Chen et al., 1998). The Zhujiang Xiver delta,which has l2 cities ofdifferent sizes and more than 40 towns with a po… 相似文献
92.
聚类分析法在浅海水团分析中的应用及黄、东海变性水团的分析 总被引:1,自引:0,他引:1
本文引入变性水团概念,用聚类分析确定黄、东海浅海海域变性水团的边界及其变化。根据给定的标准进行聚类,确定了水团的个数、边界及混合区。 由聚类方法所得结果看出,在该海区中有八个变性水团。根据温、盐相对指标,将这些水团分为九种不同的特征。也可以把这些水团划分为三种盐度类型。在温—盐点聚图上,不同变性水团的温盐点,分布于一条曲线附近,它体现出逐级变性的特点。各变性水团的变化范围都很大,这说明该海区中水团变性强烈。在暖季中的增温降盐和冷季中的降温增盐,可认为是整个黄海和东海水体变性的特征。所有季节性水团都经历一个形成与消亡的过程。 文中讨论了变性水团和海洋环境的相互关系。水团变性是热力因素和动力因素共同作用而产生的。通过变性水团的分析,作者认为,在该海区水团的变性中,热力因素起着主要作用。变性水团界线的舌状分布与流向之间的关系是很明显的,可作为分析环流的旁证。最后描述了变性水团和底层中心渔场之间的关系。 相似文献
93.
94.
95.
东海陆架外缘隆起带地质构造特征 总被引:1,自引:0,他引:1
根据地质、地球物理及钻探资料,结合周边区域地质资料,论证东海外缘隆起带前中中新世基底岩系组成及地质构造特征。 相似文献
96.
长江口及济州岛附近海域变性水团的初步分析 总被引:1,自引:0,他引:1
基于变性水团的概念,本文把聚类分析用于确定长江口及济州岛附近海域变性水团的边界。由聚类分析得到的结果表明,在该海区有十个水团。对它们的特征、分布与变化进行了初步分析。作者得出的结论是:1、在十个水团中,有四个大洋性水团,六个变性水团。2、该海域水团变性的特点为暧季增温、降盐、降氧,而冷季则相反。3、水团变性是由海区内、外因素综合作用而发生的,而后者在浅水区域起主要作用。4、水团边界的舌状分布与流向之间有明显关系。因之,海流的方向及强度,大致可依水团舌状分布而判断。5、底层中心渔场基本上位于各变性水团之间的混合区或其附近。 相似文献
97.
Moo Hee Kang Hyun-Chul Han Hyesu Yun Gee Soo Kong Kyong O. Kim Youn Soo Lee 《Marine Geophysical Researches》2007,28(3):257-269
A seamount chain with an approximately WNW trend is observed in the northeastern Ulleung Basin. It has been argued that these
seamounts, including two islands called Ulleung and Dok islands, were formed by a hotspot process or by ridge related volcanism.
Many geological and geophysical studies have been done for all the seamounts and islands in the chain except Anyongbok Seamount,
which is close to the proposed spreading ridge. We first report morphological characteristics, sediment distribution patterns,
and the crustal thickness of Anyongbok Seamount using multibeam bathymetry data, seismic reflection profiles, and 3D gravity
modeling. The morphology of Anyongbok Seamount shows a cone shaped feature and is characterized by the development of many
flank cones and flank rift zones. The estimated surface volume is about 60 km3, and implies that the seamount is smaller than the other seamounts in the chain. No sediments have been observed on the seamount
except the lower slope, which is covered by more than 1,000 m of strata. The crustal structure obtained from a 3D gravity
modeling (GFR = 3.11, SD 3.82 = mGal) suggests that the seamount was formed around the boundary of the Ulleung Plateau and
the Ulleung Basin, and the estimated crustal thickness is about 20 km, which is a little thicker than other nearby seamounts
distributed along the northeastern boundary of the Ulleung Basin. This significant crustal thickness also implies that Anyongbok
Seamount might not be related to ridge volcanism. 相似文献
98.
In-Seong Han Koichiro Kamio Takeshi Matsuno Atsuyoshi Manda Atsuhiko Isobe 《Journal of Oceanography》2001,57(2):235-249
Relation between internal waves with short time scale and density distribution near the shelf break in the East China Sea is studied utilizing moored current meters, thermometers and conductivity-temperature-depth (CTD) casts. A well developed pycnocline was frequently observed around 150–200 m depth near the shelf break accompanied with the development of internal waves with short time scale. During the cruise in May 1998, the intensified internal wave motion with short time scale and the distinct offshore flow were observed just below the lower pycnocline, which shoaled and extended above the shelf area. It is suggested that vertical mixing generated by amplified internal waves would produce cross-shelf ageostophic density current around the pycnocline. During the cruise in May 1999, on the other hand, the lower pycnocline was located offshore below the shelf break, and the internal wave motion was amplified just above the lower pycnocline. In this case, the offshore flow should be generated above the lower pycnocline, but vertical profiles of current velocity were not obtained because acoustic Doppler current profiler (ADCP) data were not available around the lower pycnocline. 相似文献
99.
Concentrations of total recoverable inorganic tin (TRISn), monomethyltin (MeSn3+), dimethyltin (Me2Sn2+), trimethyltin (Me3Sn+) and (3-dimethylsulphonio)propionate (DMSP) were determined in leaves of Spartina alterniflora from three sites in the Great Bay estuary (NH) from 8 May to 15 September 1989. Total methyltin concentration increased from 8·9 ng g−1 (fresh weight) on 8 May to 472 ng g−1 on 23 May, decreased to 52 ng g−1 on 7 June and 16ng g−1 on 20 June, and remained low until the last sample on 18 September. Statistical calculations showed that methyltin concentrations varied significantly with sampling week, but not with site. DMSP concentrations showed very different behaviour. During the same sampling period DMSP concentrations varied only from 7·5 to 26 μmol g−1 (fresh weight). DMSP concentrations varied significantly for site, but not sampling week. 相似文献
100.
Naoto Ebuchi 《Journal of Oceanography》2006,62(2):171-183
Seasonal and interannual variations in the East Sakhalin Current (ESC) are investigated using ten-year records of the sea
level anomaly (SLA) observed by the TOPEX/POSEIDON (T/P) altimeter. The T/P SLA clearly documents seasonal and interannual
variations in the ESC along the east coast of Sakhalin Island, although sea ice masks the region from January to April. Estimates
of surface current velocity anomaly derived from T/P SLA are in good agreement with drifting buoy observations. The ESC is
strong in winter, with a typical current velocity of 30–40 cm s−1 in December, and almost disappears in summer. Southward flow of the ESC is confined to the shelf and slope region and consists
of two velocity cores. These features of the ESC are consistent with short-term observations reported in previous studies.
Analysis of the ten-year records of T/P SLA confirms that the structure of the ESC is maintained each winter and the seasonal
cycle is repeated every year, although the strength of the ESC shows large interannual variations. Seasonal and interannual
variations in the ESC are discussed in relation to wind-driven circulation in the Sea of Okhotsk, using wind stress and wind
stress curl fields derived from European Centre for Medium Range Weather Forecasts (ECMWF) reanalysis data and a scatterometer-derived
wind product. Seasonal and interannual variations of the anticyclonic eddy in the Kuril Basin are also revealed using T/P
SLA. 相似文献