全文获取类型
收费全文 | 79篇 |
免费 | 4篇 |
国内免费 | 14篇 |
专业分类
大气科学 | 9篇 |
地球物理 | 21篇 |
地质学 | 18篇 |
海洋学 | 19篇 |
天文学 | 23篇 |
综合类 | 2篇 |
自然地理 | 5篇 |
出版年
2022年 | 1篇 |
2021年 | 1篇 |
2020年 | 1篇 |
2018年 | 1篇 |
2017年 | 1篇 |
2016年 | 1篇 |
2014年 | 1篇 |
2013年 | 2篇 |
2012年 | 1篇 |
2011年 | 2篇 |
2010年 | 3篇 |
2009年 | 3篇 |
2008年 | 6篇 |
2007年 | 5篇 |
2006年 | 2篇 |
2005年 | 6篇 |
2004年 | 5篇 |
2003年 | 6篇 |
2002年 | 2篇 |
2001年 | 9篇 |
2000年 | 3篇 |
1999年 | 7篇 |
1998年 | 5篇 |
1996年 | 1篇 |
1995年 | 1篇 |
1994年 | 1篇 |
1988年 | 2篇 |
1986年 | 4篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1980年 | 4篇 |
1979年 | 2篇 |
1978年 | 1篇 |
1976年 | 2篇 |
1975年 | 1篇 |
1972年 | 1篇 |
排序方式: 共有97条查询结果,搜索用时 15 毫秒
81.
82.
山东海阳所麻粒岩向过渡榴辉岩转化的变质动力学过程及其构造意义 总被引:2,自引:2,他引:0
在山东半岛东南端的乳山海阳所,角闪岩和长英质片麻岩呈互层产出,在某些角闪岩层的中心残留有弱变形的麻粒岩和强变形的过渡榴辉岩(斜长石榴辉岩)团块,在弱变形的麻粒岩团块中发育有窄的(〈1cm)剪切条带,沿着这些剪切条带和强变形过渡榴辉岩团块中,原麻粒岩被转化为含斜长石的过渡榴辉岩。变形和流体在这一转化过程中加速了元素扩散和迁移的速度,在变形强和有流体加入的部位麻粒岩向榴辉岩转化的程度明显增强,麻粒岩相 相似文献
83.
INTRODUCTIONCollisionofIndiawithAsiaappearstohavebroughtaboutlargetectonicdeformationofAsia,especiallyEastAsia(Tapponnieretal.,1986).Post-Cretaceousdeformation(translationand/orrotation)ofSimaoandIndochinablocks,whicharelocatedatthesouthernsideofRedRiverfault(RRF),hasbeenreportedfromCretaceouspaleomagneticin-vestigations(Yangetal.,l995;HuangandOpdyke,l993IYangandBesse,1993).AlsoinSouthChinablock(SCB)locatedatnorthsideoftheRRF,localdeformationofsomeregionsneartheRRFhasbeendocum… 相似文献
84.
Xu Hui Zhang Weiping Lang Xuxing Guo Xia Ge Wenzhong Dang Renqing Takao Takeda 《大气科学进展》2000,17(3):403-412
During the Meiyu period in June and July of 1998, intensified field observations have been carried out for the project “Huaihe
River Basin Energy and Water Cycle Experiment (HUBEX)”. For studying Meiyu front and its precipitation in Huaihe River basin,
the present paper has performed analysis on the middle and lower level wind fields in the troposphere by using the radar data
obtained from the two Doppler radars located at Fengtai district and Shouxian County.
From June 29 to July 3 in 1998, the continuous heavy precipitation occurred in Huaihe River basin around Meiyu front. The
precipitation process on July 2 occurred within the observation range of the two Doppler radar in Fengtai district and Shouxian
County. The maximum rainfall of the Meiyu front was over 100 mm in 24 h, so it can be regarded as a typical mesoscale heavy
precipitation process related to Meiyu front.
Based on the wind field retrieved from the dual Doppler radar, we find that there are meso-γ scale vertical circulations in
the vertical cross-section perpendicular to Meiyu front, the strong upward motion of which corresponds to the position of
the heavy rainfall area. Furthermore, other results obtained by this study are identical with the results by analyzing the
conventional synoptic data years ago. For example: in the vicinity of 3 km level height ahead of Meiyu front there exists
a southwest low-level jet; the rainstorm caused by Meiyu front mainly occurs at the left side of the southwest low-level jet;
and the Meiyu front causes the intensification of the low-level convergence in front of it.
This research was supported by Project HUBEX (Project Number: 49794030) which is funded by the National Natural Science Foundation
of China (NSFC). 相似文献
85.
The wave characteristics of Pc5 magnetic pulsations are analyzed with data of OGO-5, ISEE-1 and -2 satellites. The toroidal modes (δBD >δBH) of Pc5 pulsations are observed at a higher magnetic latitude in the dawnside outer magnetosphere. The compressional and poloidal modes (δBz.dfnc; ~ δBH >δBD) of Pc5 pulsations are mostly observed near the magnetic equator in the duskside outer magnetosphere. This L.T. asymmetry in the occurrence of dominant modes of Pc5's in space can be explained by the velocity shear instability (Yumoto and Saito, 1980) in the magnetospheric boundary layer, where Alfvénic signals in the IMF medium are assumed to penetrate into the magnetospheric boundary layer along the Archimedean spiral. The asymmetrical behaviour of Pc5 pulsation activity on the ground across the noon meridian can be also explained by the ionospheric screening effect on the compressional Pc5 magnetic pulsations. The compressional modes with a large horizontal wave number in the duskside magnetosphere are expected to be suppressed on the ground throughout the ionosphere and atmosphere. 相似文献
86.
Takashi Murayama Takao Aoki Hitoshi Nakai Kazuyuki Hakamada 《Planetary and Space Science》1980,28(8):803-813
An empirical formula has been constructed using the results of correlative analyses to determine in what form the AL index, as a measure of the intensity of the westward auroral electrojet, depends on interplanetary parameters. The formula thus obtained shows that AL is mainly determined by BsV2 where Bs is the southward component of the IMF and V is the solar wind velocity, and is modulated in a characteristic way by the combined effect of the east-west component of the IMF and the tilt angle of the Earth's dipole axis toward the Sun-Earth line. In contrast, effects of the solar wind density and the IMF variability were found to be insignificant.Implications of the empirical formula are discussed mainly in relation to the problem of the location in the dayside magnetosphere of the region where the reconnection process to initiate the substorm takes place. 相似文献
87.
Takao Eguchi 《Physics of the Earth and Planetary Interiors》1983,33(4):318-327
The overall pattern of the recent tectonic stress field in the eastern part of the Eurasian plate is inferred from the geological features of large transcurrent and reverse faults, graben structures and from focal mechanism solutions of shallow earthquakes. NE-SW striking trajectory lines, of maximum horizontal tectonic stress axis (σ Hmax), are estimated at the north of Tibet and mainland China, but its strike turns to easterly near the eastern margin of the Eurasian plate. This suggests that the main origin of the σ Hmax in East Eurasia is due to a compressive stress regime along, the Himalayan belt, Tibet and the Japan Trench (and also the Sakhalin and Nankai Trough). This tectonic stress field seems to provide some influence on the extensional tectonics in the Shansi region, Baikal, and also in the Okinawa Trough where the N-S opening has been confirmed. The systematic view of the tectonic stress field in East Eurasia, makes it possible to appreciate the fundamental background of a number of complicated intra-plate tectonics. 相似文献
88.
Effect of dietary docosahexaenoic acid on lipogenesis and lipolysis in black sea bream, Acanthopagrus schlegeli 总被引:2,自引:0,他引:2
JI Hong OM Ahamd Dau YOSHIMATSU Takao UMINO Testuy NAKAGAWA Heisuke FURUHASHI Makoto SAKAMOTO Shuichi 《海洋学报(英文版)》2007,26(1):112-121
1 IntroductionIt is well known that varying dietary fatty acidprofile affects the tissue fatty acid composition and e-ven the growth performance in fish ( Bell et al.,2002; Figueiredo -Silva et al., 2005; Harel andPlace, 2003; Schulz et al., 2005; Tocher et al.,2003). Docosahexaenoic acid (DHA), an importantessential fatty acid for marine species, has the effectnot only on the fatty acid profile of fish body tissue,but also on biological and physiological conditions(Ishizaki et al., 2000; … 相似文献
89.
Eguchi Takao Fujinawa Yukio Fujita Eisuke Iwasaki Sin-Iti Watabe Isao Fujiwara Hiroyuki 《Marine Geophysical Researches》1998,20(2):73-94
We installed a real-time operating regional observation network of Ocean-Bottom-Seismometers, connected to an electro-optical fiber communication cable, at the Sagami trough subduction zone, just south of the Tokyo metropolitan area, central Japan. The network, called ETMC, has six seismic observation sites at approximately 20 km spacing. In addition, there are three tsunami observation sites along the ETMC network to monitor the propagation process of tsunamis around the Sagami trough region.The on-line data from the ETMC has been improving the detection capability of smaller-magnitude earthquakes even at areas close to the margin of the trough. The ETMC data analyzing system, which has a function of real-time digital filtering for each seismic channel, can read the arrival times of P- and S-waves precisely, constraining well the automatic on-line hypocenter locations. The network has been providing useful information regarding the bending and downgoing process of the Philippine sea plate at the Sagami trough subduction zone.The pressure sensors of the installed network have a detection capability of tsunami wave trains with an amplitude of less than 1 cm. For example, the sensors recorded the full time history of tsunami wave trains, with mm order resolution, originating from a tsunami earthquake with 5.7 MW and the tsunami magnitude of 7.5 occurred near Tori Shima (Tori Is.) of the Izu-Bonin Is. arc on September 4, 1996. The maximum amplitude of the tsunami signals on the trough-floor was approximately 1 cm (P-P), in contrast with approximately 20 cm (0-P) at a coastal site on Izu-Oshima, near the trough. Also, the pressure sensors observed tsunamis due to a large tsunami earthquake (7.1 MW) at the northern New Guinea, on July 17, 1998. 相似文献
90.