全文获取类型
收费全文 | 41320篇 |
免费 | 695篇 |
国内免费 | 317篇 |
专业分类
测绘学 | 959篇 |
大气科学 | 2944篇 |
地球物理 | 8001篇 |
地质学 | 14215篇 |
海洋学 | 3848篇 |
天文学 | 9741篇 |
综合类 | 74篇 |
自然地理 | 2550篇 |
出版年
2021年 | 404篇 |
2020年 | 401篇 |
2019年 | 453篇 |
2018年 | 940篇 |
2017年 | 843篇 |
2016年 | 1090篇 |
2015年 | 608篇 |
2014年 | 1001篇 |
2013年 | 2073篇 |
2012年 | 1132篇 |
2011年 | 1619篇 |
2010年 | 1470篇 |
2009年 | 1983篇 |
2008年 | 1645篇 |
2007年 | 1730篇 |
2006年 | 1587篇 |
2005年 | 1311篇 |
2004年 | 1270篇 |
2003年 | 1241篇 |
2002年 | 1193篇 |
2001年 | 1056篇 |
2000年 | 980篇 |
1999年 | 810篇 |
1998年 | 813篇 |
1997年 | 829篇 |
1996年 | 668篇 |
1995年 | 656篇 |
1994年 | 616篇 |
1993年 | 570篇 |
1992年 | 526篇 |
1991年 | 495篇 |
1990年 | 506篇 |
1989年 | 496篇 |
1988年 | 474篇 |
1987年 | 553篇 |
1986年 | 489篇 |
1985年 | 604篇 |
1984年 | 650篇 |
1983年 | 592篇 |
1982年 | 527篇 |
1981年 | 578篇 |
1980年 | 469篇 |
1979年 | 458篇 |
1978年 | 433篇 |
1977年 | 433篇 |
1976年 | 383篇 |
1975年 | 378篇 |
1974年 | 377篇 |
1973年 | 384篇 |
1971年 | 224篇 |
排序方式: 共有10000条查询结果,搜索用时 9 毫秒
411.
William C. Schwab Elazar Uchupi Robert D. Ballard Thomas K. Dettweiler 《Geo-Marine Letters》1989,9(3):171-178
SeaMARC side-scan sonographs and Argo video and photographic data suggest that the recent sedimentary environment of the floor
of the Tongue of the Ocean is controlled by an interplay of turbidity current flow from the south, sediment spill-over from
the carbonate platform to the east (windward side), and rock falls from the west carbonate escarpment (lee side). The spill-over
forms a sandy sedimentary deposit that acts as a topographic obstruction to the turbidity current flow from the south. This
obstruction is expressed by the westward migration of a northwest-southeast oriented turbidity-current-cut channel. 相似文献
412.
413.
Gallo D. G. Kidd W. S. F. Fox P. J. Karson J. A. Macdonald K. Crane K. Choukroune P. Seguret M. Moody R. Kastens K. 《Marine Geophysical Researches》1984,6(2):159-185
During the Fall of 1979, a manned submersible program, utilizing DSRV ALVIN, was carried out at the intersection of the East Pacific Rise (EPR) with the Tamayo Transform boundary. A total of seven dives were completed in the vicinity of the EPR/Tamayo intersection depression and documented the geologic relationships that characterize the juxtaposition of these types of plate boundaries. The young volcanic terrain of the EPR axis can be traced into and across the Tamayo Transform valley but becomes buried by sedimentary talus that is being shed from sediment scarps along the unstable sediment slope that defines the north side of the intersection depression. Within 4 km of the transform boundary, the dominant trend (000°) of the fissures and faults that disrupt the rise-generated volcanics is markedly oblique to the regional direction of sea floor spreading (120°). Since no evidence was found to suggest that these structures accommodate significant amounts of strike-slip displacement, they are taken to reflect a distortion of the EPR extensional tectonic regime by a transform generated shear couple. The floor of the Tamayo Transform valley in this area is inundated by mass-wasted sediment, and the principal transform displacement zone is characterized at the surface by a narrow (<1.5 km) interval of fault scarps in sediment that trends parallel with the transform valley. Extrapolated to the west, this zone links with zones of transform deformation investigated during earlier submersible studies (CYAMEX and Pastouret, 1981). Evidence of low-level hydrothermal discharge was seen at one locality on the EPR axis and at another 8 km west of the axis at the edge of the zone of transform deformation. 相似文献
414.
The wavemaking capability and energy absorbing characteristics of a single submerged body, constrained to move horizontally in a surge mode, are examined. The body possesses both a vertical axis of symmetry and a horizontal plane of symmetry and is ‘thin’ in the sense that the body draft is small compared to the length. The behaviour of a single body subject to a constraint being placed upon the amplitude of its displacement and the properties of an array of interacting identical devices are also discussed. 相似文献
415.
The decline of the herring stocks and the gadoid outburst 总被引:2,自引:1,他引:2
416.
417.
The drainage pattern in the northeast and central Tufts Abyssal Plain is described in detail. Satellite navigation on the systematic survey has allowed precise location of the major channel systems of the northeast Pacific Ocean. Two hundred channel profiles were collected from the echograms showing the Moresby-Scott, Mukluk, and Horizon Channel Systems trending in either a southwestward or westward direction across this section of the Tufts Plain. The channel profiles illustrate the prominence of the higher and wider right-hand levee (facing downstream). The Moresby-Scott Channel System disperses in the form of several distributaries throughout the area studied, and is probably responsible for much of the sediment deposits. Unlike the Moresby-Scott, the Mukluk extends throughout the survey area as a solitary channel with one minor branch. The Horizon Channel crosses the Sedna Fracture Zone east of the Sedna Seamount and terminates in distributary fashion in the central portion of the Tufts Plain. The Moresby-Scott, Mukluk, and Horizon Channels form one major system which encompasses the entire northeast and central Tufts Abyssal Plain. 相似文献
418.
The Solomon Sea Plate was widely developed during late Oligocene, separating the proto-West Melanesian Arc from the proto-Trobriand Arc. Spreading in the Bismarck Sea and in the Woodlark Basin resulted from interaction between the Pacific and Australian Plates, specifically from the collision of the proto-West Melanesian Arc with north New Guinea, which occurred after arc reversal. This model explains the extensive Miocene, Pliocene, and Quaternary volcanism of the Papua New Guinea mainland as it related to southward subduction of the Trobriand Trough. Our interpreted plate motions are concordant with the geological evidence onshore and also with complex tectonic features in the Solomon Sea Basin Region. 相似文献
419.
420.