全文获取类型
收费全文 | 22486篇 |
免费 | 4216篇 |
国内免费 | 5478篇 |
专业分类
测绘学 | 1632篇 |
大气科学 | 4906篇 |
地球物理 | 5922篇 |
地质学 | 10518篇 |
海洋学 | 3453篇 |
天文学 | 834篇 |
综合类 | 2160篇 |
自然地理 | 2755篇 |
出版年
2024年 | 117篇 |
2023年 | 374篇 |
2022年 | 1006篇 |
2021年 | 1189篇 |
2020年 | 937篇 |
2019年 | 1099篇 |
2018年 | 1145篇 |
2017年 | 1147篇 |
2016年 | 1239篇 |
2015年 | 1127篇 |
2014年 | 1258篇 |
2013年 | 1449篇 |
2012年 | 1312篇 |
2011年 | 1399篇 |
2010年 | 1451篇 |
2009年 | 1344篇 |
2008年 | 1143篇 |
2007年 | 1187篇 |
2006年 | 944篇 |
2005年 | 882篇 |
2004年 | 591篇 |
2003年 | 641篇 |
2002年 | 631篇 |
2001年 | 643篇 |
2000年 | 733篇 |
1999年 | 1005篇 |
1998年 | 808篇 |
1997年 | 809篇 |
1996年 | 756篇 |
1995年 | 698篇 |
1994年 | 607篇 |
1993年 | 515篇 |
1992年 | 435篇 |
1991年 | 297篇 |
1990年 | 232篇 |
1989年 | 193篇 |
1988年 | 185篇 |
1987年 | 112篇 |
1986年 | 106篇 |
1985年 | 66篇 |
1984年 | 57篇 |
1983年 | 56篇 |
1982年 | 57篇 |
1981年 | 40篇 |
1980年 | 41篇 |
1979年 | 37篇 |
1978年 | 14篇 |
1977年 | 9篇 |
1974年 | 9篇 |
1958年 | 18篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
301.
基于BP人工神经网络的水体遥感测深方法研究 总被引:5,自引:0,他引:5
利用Landsat7ETM+遥感图像反射率和实测水深值之间的相关性,建立了动量BP人工神经网络水深反演模型,并对长江口南港河段水深进行了反演.结果表明:具有较强非线性映射能力的动量BP神经网络模型能较好地反演出长江口南港河段的水深分布情况;由于受长江口水体高含沙量的影响,模型对小于5 m的水深值反演精度较高,而对大于10 m的水深值反演精度较低. 相似文献
302.
氮浓度对四株海洋绿藻总脂含量和脂肪酸组成的影响 总被引:6,自引:0,他引:6
本文用NaNO3作为氮源,分别作了氮浓度的五个水平对2属(小球藻属、裂丝藻属)的四株绿藻的生长率、总脂含量及主要脂肪酸组成的影响。C19、C97和C102的脂肪含量随N浓度的改变而有较大变化,其中C102在1.6m mol/L时脂肪含量达到最大值(24.8%)。C95的脂肪含量随氮浓度变化不大。同时,由氮浓度引起的平均生长率μ与总脂含量之间无明显相关关系。四株绿藻的EPA(20∶5n-3)和PUFAs(polyunsaturated fatty acids)含量随培养基中氮浓度的改变有较大变化但因种而异。C95和C97均在中等氮浓度时EPA含量达到最大值,分别为23.8%和27.4%。C19和C102在高氮浓度(40mmol/L)获得EPA的最大值,分别为25.7%和26.6%。 相似文献
303.
INTRODUCTIONBystudyingchlorophyllandprimaryproductivityinocean ,eitherinthebig scaleorinthesmallscale ,theproductivitydistributionandvariationofmarineorganicmaterialinthetempo ralandspatialcanbeunderstood .Theseaareas ,situatinginthewesterntropicalPacific… 相似文献
304.
305.
Calcimicrobialites across the Permian-Triassic boundary in Huayingshan (华蓥山) region were investigated using the fluorescence microscopic measurements to understand the occurrence of organic matter. The microbialites are composed of micrite matrix and coarse spar cement. Abundant rhombic or magnetic needle-like carbonate minerals were observed adrift within the cement. The fluorescence microscopic measurement indicates the micrite matrix in microbialites shows the most abundant organic matter, with the rhombic or magnetic needle-like carbonate minerals and coarse spar cement coming to the 2nd and the 3rd, respectively. Organic matter is mainly preserved in the space between the grains of the micrite minerals but almost evenly distributed in the rhombic or magnetic needle-like carbonate minerals. As one of the common diagenesis types, dolomitization is observed to occur in the microbialites in Huayingshan. However, the carbonate cement in microbialites still has high content of element Sr as shown by the microprobe analysis, reflecting that the dolomitization might have happened in a restricted environment. Observation under the fluorescence microscope shows that dolomitization just led to the redistribution of organic matter in the grain space of dolomite minerals, inferring that the diagenesis has a slight effect on the preservation, and thus on the content of organic matter in the microbialites. 相似文献
306.
Lü Xixue 《中国地质大学学报(英文版)》2008,19(6):675-684
Jiyang (济阳) sag is an oil rich basin,consisting of Huimin (惠民),Dongying (东营),Zhanhua (沾化),and Chezhen (车镇) depressions.The elastic rock of Paleogene has undergone early and middle diagenetic stages and now the main clastic reservoir is in the middle diagenetic stage.Primary and secondary pores are developed in Paleogene sandstone,the latter is generated from the dissolution of feldspar and calcite cement in rocks owing to the organic acid from the maturated source rock,but the materials dissolved are different in different depressions.The reservoir secondary pores of Dongying depression are generated from the dissolution of calcite cement,the ones of Zhanhua and Huimin depressions from the dissolution of feldspar,the secondary pores of Chezhen depression from the dissolution of feldspar in upper section,and the dissolution of calcite cement in the lower section of Paleogene,respectively.The secondary pores are developed in two depths and the depth goes down from west to east,from south to north in Jiyang sag.The major controlling factors for secondary pore development are maturity and location of source rock.Lastly,the favorable reservoirs are evaluated according to reservoir buried depth,sedimentation,and diagenesis.The reservoir with high quality is located in the northern and central parts in Dongying depression; there are some good reservoirs in Gndao (孤岛),Gudong (孤东),and Gunan (孤南) areas in Zhanhua depression,and the favorable reservoirs are located in the north steep slope and the south gentle slope of Chezhen depression and central uplift,south gentle slope of Huimin depression. 相似文献
307.
308.
309.
310.
Early carbonate cements in the Yanchang Formation sandstones are composed mainly of calcite with relatively heavier carbon isotope (their δ^18O values range from -0.3‰- -0.1‰) and lighter oxygen isotope (their δ^18O values range from -22.1‰- -19.5‰). Generally, they are closely related to the direct precipitation of oversaturated calcium carbonate from alkaline lake water. This kind of cementation plays an important role in enhancing the anti-compaction ability of sandstones, preserving intragranular volume and providing the mass basis for later disso- lution caused by acidic fluid flow to produce secondary porosity. Ferriferous calcites are characterized by relatively light carbon isotope with δ^13C values ranging from -8.02‰ to -3.23‰, and lighter oxygen isotope with δ^18O values ranging from -22.9‰ to -19.7‰, which is obviously related to the decarboxylation of organic matter during the late period of early diagenesis to the early period of late diagenesis. As the mid-late diagenetic products, ferriferous cal- cites in the study area are considered as the characteristic authigenic minerals for indicating large-scaled hydrocarbon influx and migration within the clastic reservoir. The late ankerite is relatively heavy in carbon isotope with δ^13C values ranging from -1.92‰ to -0.84‰, and shows a wide range of variations in oxygen isotopic composition, with δ^18O values ranging from -20.5‰ to -12.6‰. They are believed to have nothing to do with decarboxylation, but the previously formed marine carbonate rock fragments may serve as the chief carbon source for their precipitation, and the alkaline diagenetic environment at the mid-late stage would promote this process. 相似文献