全文获取类型
收费全文 | 71354篇 |
免费 | 1133篇 |
国内免费 | 659篇 |
专业分类
测绘学 | 1719篇 |
大气科学 | 5034篇 |
地球物理 | 14230篇 |
地质学 | 25286篇 |
海洋学 | 6188篇 |
天文学 | 16346篇 |
综合类 | 208篇 |
自然地理 | 4135篇 |
出版年
2022年 | 396篇 |
2021年 | 705篇 |
2020年 | 781篇 |
2019年 | 829篇 |
2018年 | 1899篇 |
2017年 | 1764篇 |
2016年 | 2241篇 |
2015年 | 1325篇 |
2014年 | 2178篇 |
2013年 | 3773篇 |
2012年 | 2283篇 |
2011年 | 3128篇 |
2010年 | 2609篇 |
2009年 | 3513篇 |
2008年 | 3260篇 |
2007年 | 3052篇 |
2006年 | 2879篇 |
2005年 | 2359篇 |
2004年 | 2257篇 |
2003年 | 2115篇 |
2002年 | 1931篇 |
2001年 | 1802篇 |
2000年 | 1720篇 |
1999年 | 1379篇 |
1998年 | 1471篇 |
1997年 | 1388篇 |
1996年 | 1102篇 |
1995年 | 1144篇 |
1994年 | 964篇 |
1993年 | 873篇 |
1992年 | 855篇 |
1991年 | 759篇 |
1990年 | 857篇 |
1989年 | 720篇 |
1988年 | 650篇 |
1987年 | 815篇 |
1986年 | 663篇 |
1985年 | 855篇 |
1984年 | 922篇 |
1983年 | 862篇 |
1982年 | 832篇 |
1981年 | 707篇 |
1980年 | 664篇 |
1979年 | 606篇 |
1978年 | 603篇 |
1977年 | 552篇 |
1976年 | 539篇 |
1975年 | 499篇 |
1974年 | 506篇 |
1973年 | 468篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
811.
812.
813.
David M. Smith 《Geoforum》1979,10(3):297-310
The problems of the inner city are a subject of growing concern in the advanced capitalist world. The level of social deprivation may be identified on a territorial basis, by mapping numerical indicators relating to various relevant conditions. However, the application of conventional geographical methodology with its emphasis on pattern identification and ecological analysis provides an inadequate foundation for the explanation of localized deprivation and for the design of remedial policy. Inner-city deprivation arises from the operation of the contemporary capitalist system, the understanding of which requires a holistic social-science perspective. 相似文献
814.
J. M. Hurst 《Geological Journal》1979,14(2):15-40
The middle Caradoc rocks of Salop are a mosaic of sedimentary facies deposited in nearshore environments. The uppermost Horderley Sandstone in the Onny Valley is interpreted as formed by migrating marine bars and proximal and distal stonn deposits. The time equivalent Chatwall Sandstone of the Chatwall district is interpreted as a beach sequence. The overlying Alternata Limestone is a product of both proximal and distal storm deposits, associated with marine bars, in which different faunal assemblages are mized. Correlation of local sections is difficult due to facies and faunal changes and non-deposition events. Based on a sedimentary model and palaeoecological information it is suggested that the Alternata Limestone in the Chatwall area is older than elsewhere, and that the base of the Cheney Longville Flags youngs southwards. Four faunal events are defined based on transect collecting, discriminant function and cluster analysis. These are the Howellites antiquior, Dalmanella lepta and Bancroftina robuste Associations and the Heterorthis alternata interregnum. 相似文献
815.
This paper presents palaeontological ages based on new nannofossil and foraminiferal studies from a range of sedimentary rocks from the provinces of West and East Kalimantan, Indonesia. The age of sedimentary rocks in Kalimantan, away from the main hydrocarbon exploration areas of the coastal regions, represents a major gap in our basic knowledge of the island of Borneo. The implications of these new results and existing and new correlations are reviewed and suggested. In particular, the base of the Tertiary section in the Kutai Basin is shown to be upper Middle Eocene in age, rather than Late Eocene as originally thought. The limestones of the Batu Belah member of the Ujoh Bilang Formation are dated as NP24–25, Late Oligocene, rather than Early Oligocene as earlier work had suggested. In the western part of the Mangkalihat Peninsula area the base of the Tertiary section is determined to be Late Oligocene. Various basement units from both East and West Kalimantan contained Late Jurassic to Late Cretaceous microfossils. 相似文献
816.
Erwin E. Klaas Stanley N. Wiemeyer Harry M. Ohlendorf Douglas M. Swineford 《Estuaries and Coasts》1978,1(1):46-53
Eggs of barn owls (Tyto alba) were collected from 18 nests in offshore duck blinds on the Maryland side of the lower Potomac River estuary in 1972 and 1973 and analyzed for organochlorine residues. DDE was found in 100% of the clutches, PCBs in 89%, and dieldrin in 78%. Eggshell thickness was inversely correlated with concentrations of DDE, DDD, and dieldrin residues. Six of the 18 clutches had mean DDE residues above 5 ppm, and eggshell thickness in these six clutches was significantly less (P<0.001) than in the other 12 clutches. The owls produced 1.7 young per active nest in 1973. This rate is slightly below the reproductive rate needed to maintain a stable population. An estimated 15% of the population carried concentrations of organochlorine residues that may have been detrimental to their reproduction. Passerine birds, taken extensively as food by a small proportion of the population, are believed to have been the source of elevated concentrations of organochlorines in these barn owls. 相似文献
817.
M. T. Krupenin A. V. Maslov I. D. Tsybulenko R. A. Nafikov V. G. Petrishcheva 《Lithology and Mineral Resources》2000,35(3):267-277
A property of swelling on heating to yield firm lightweight granules has first been revealed for lowcarbonaceous shales (LCS)
from the Riphean stratotype in the Bashkirian Megaanticlinorium, Southern Urals. These granules possess all technological
properties of “keramzite” or claydite (an artificial, expanded clayey material) and can successfully substitute this material.
Moreover, the procedure of their manufacture, analogous to the manufacture of “shungizite” (an artificial carbonaceous-clayey
material) from Lower Proterozoic clayey rocks of Karelia, is more economical than that for keramzit. Productive beds of the
homogeneous LCS make up extended bodies tens of meters thick. At the present time, they can be used as cover rocks during
the exploitation of the Bakal siderite deposits. The LCS represent fine-grained quartz-chlorite-sericite aggregates (with
variable relationships between the major components), bearing fine-dispersed shungite in amounts of 0.5–1.0%. High-quality
raw material of this kind is characterized by a fine-dispersed admixture of a mixed-layer clayey material bearing montmorillonite
and vermiculite. Geological, lithological, mineralogical, and chemical prognostic criteria have been developed for the shungizite
raw material. It has been concluded that this construction material, new for the Urals, is promising for industrial use 相似文献
818.
819.
Ohne Zusammenfassung 相似文献
820.
The caves of the Umbria and Marche regions in central Italy are made up of three-dimensional maze systems that display different general morphologies due to the various geological and structural contexts. At the same time, the internal morphologies of the passages, galleries, and shafts present some similarity, with solutional galleries characterized by cupolas and blind pits, anastamotic passages, roof pendants, and phreatic passages situated at different levels. Some of these caves are still active, as is the case for Frassassi Gorge, Parrano Gorge, and Acquasanta Terme, with galleries that reach the phreatic zone, where there is a rising of highly mineralized water, rich in hydrosulfydric acid, and with erosion of limestone walls and the formation of gypsum. Elsewhere there are fossil caves, such as Monte Cucco and Pozzi della Piana, where large speleothems of gypsum are present 500 m or more above the regional water table. In all of these important karst systems it is possible to recognize basal input points through fracture and intergranular porosity networks at the base of the oxidizing zone in the core of the anticline, where mineralized water rises up from the Triassic evaporitic layers in small hydrogeological circuits. Different underground morphologies can derive from the presence of a water table related to an external stream or from the confined setting of the carbonate rocks, underlying low permeable sedimentary cover, where artesian conditions can occur. 相似文献