全文获取类型
收费全文 | 22687篇 |
免费 | 3076篇 |
国内免费 | 4381篇 |
专业分类
测绘学 | 1150篇 |
大气科学 | 3747篇 |
地球物理 | 4930篇 |
地质学 | 11017篇 |
海洋学 | 3170篇 |
天文学 | 2058篇 |
综合类 | 1779篇 |
自然地理 | 2293篇 |
出版年
2024年 | 88篇 |
2023年 | 290篇 |
2022年 | 948篇 |
2021年 | 1188篇 |
2020年 | 1084篇 |
2019年 | 1108篇 |
2018年 | 1402篇 |
2017年 | 1307篇 |
2016年 | 1365篇 |
2015年 | 1013篇 |
2014年 | 1298篇 |
2013年 | 1372篇 |
2012年 | 1303篇 |
2011年 | 1417篇 |
2010年 | 1356篇 |
2009年 | 1275篇 |
2008年 | 1164篇 |
2007年 | 1218篇 |
2006年 | 1056篇 |
2005年 | 632篇 |
2004年 | 547篇 |
2003年 | 625篇 |
2002年 | 679篇 |
2001年 | 632篇 |
2000年 | 539篇 |
1999年 | 668篇 |
1998年 | 557篇 |
1997年 | 570篇 |
1996年 | 478篇 |
1995年 | 486篇 |
1994年 | 431篇 |
1993年 | 343篇 |
1992年 | 306篇 |
1991年 | 199篇 |
1990年 | 182篇 |
1989年 | 171篇 |
1988年 | 127篇 |
1987年 | 100篇 |
1986年 | 77篇 |
1985年 | 64篇 |
1984年 | 65篇 |
1983年 | 56篇 |
1982年 | 57篇 |
1981年 | 41篇 |
1980年 | 34篇 |
1979年 | 40篇 |
1978年 | 20篇 |
1977年 | 20篇 |
1975年 | 24篇 |
1973年 | 18篇 |
排序方式: 共有10000条查询结果,搜索用时 62 毫秒
881.
882.
大兴安岭伊勒呼里山早白垩世碱长花岗岩年龄、地球化学特征及其地质意义 总被引:1,自引:1,他引:0
对大兴安岭伊勒呼里山早白垩世碱长花岗岩进行了岩相学、地球化学、LA-ICP-MS锆石U-Pb定年研究。伊勒呼里山地区碱长花岗岩主量元素具有富Si、富碱,贫Mg、Ca的特征;微量元素亏损Sr、P、Eu、Ti,富集K、Rb、Th等不相容元素,元素地球化学特征表明,岩体为铝质A型花岗岩(A/CNK=0.88~1.21,A/NK=0.94~1.49)。测年结果显示,粗中粒碱长花岗岩的锆石年龄为140.3±1.0Ma,细中粒碱长花岗岩锆石年龄为137.9±0.8Ma,均形成于早白垩世。结合区域研究资料,伊勒呼里山地区碱长花岗岩岩体的形成与蒙古-鄂霍茨克洋闭合后的岩石圈伸展密切相关,其岩浆源区可能为地壳物质的部分熔融。 相似文献
883.
E. Yu. Golubkova E. A. Kushim A. B. Kuznetsov A. S. Yanovskii A. V. Maslov S. D. Shvedov Yu. V. Plotkina 《Doklady Earth Sciences》2018,479(1):300-304
The stratigraphic distribution of microfossils and macroscopic fossil biota in Vendian deposits of the South Ladoga region (northwestern East European Platform) is analyzed. In the sequence of the Shotkusa- 1 well, three taxonomically heterogeneous microfossil assemblages are distinguished: two of them refer to the Redkinian age (Starorusskaya Fm.) and one to the Kotlinian age (Vasileostrovskaya Fm.). Deposits of the Starorusskaya Fm. contain Redkinian biota of macroscopic fossils, of which the most characteristic representatives are Chuaria circularis, Doushantuophyton lineare, Morania zinkovi, Orbisiana simplex, and Redkinia spinosa. These new findings expand the paleontological characteristics of Upper Vendian deposits, also providing additional criteria for distinguishing the Redkinian horizon in the northwestern East European Platform. 相似文献
884.
S. Yu. Sokolov 《Doklady Earth Sciences》2018,480(2):715-719
The tectogenesis of the Atlantic Ocean segments is complicated by the axial difference in spreading half-velocities, which causes additional shear displacements between the lithospheric blocks along the transform faults. The intensity of these processes and density of the fault zones iis related to the presence of “cold” sublithospheric lenses along the MAR at a depth of 500 km. 相似文献
885.
The results of studying Hg in an underwater hydrothermal system in the ocean using the Middle Valley of the Juan de Fuca ridge as an example are presented. A significant part of Hg is accumulated in the basalt fundament (Holes 858F, G), forming anomalously high concentrations (up to 29.30 ppm) in certain parts. The high Hg contents were established in metalliferous sediments (323 ppm) of the sedimentary cover (Hole 858D) and in sulfide deposits (up to 10.30 ppm). In other parts of the section, Hg content is 0.02–0.76 ppm (Holes 858B, D, F), background Hg contents in sediments—0.08–0.28 ppm and in basalts—0.17–0.31 ppm (Holes 855A, C, D). 相似文献
886.
V. L. Tauson R. G. Kravtsova V. V. Akimov S. V. Lipko A. M. Spiridonov A. E. Budyak I. Yu. Voronova O. Yu. Belozerova K. Yu. Arsentev 《Doklady Earth Sciences》2018,478(1):92-99
Pyrite crystals and ore-bearing shales of the Degdekan deposit were studied by means of XPS, SEM–EDX, EPMA, and AAS. Five peaks of carbon organic forms were identified, conforming to polymer compounds containing either double bonds of carbon or alkyne groups and compounds containing C–OH and C=O bonds, as well as, probably, small amounts of S-containing compounds and those with functional groups of carboxylic acids. Sulfate prevails over sulfite in pyrites; among the surface sulfide forms, disulfide prevails over monosulfide; the presence of polysulfide is registered. The occurrence of various chemical forms of sulfur on the surface might provide for concentrating of microelements including the noble metals (NMs) in their surface-bound forms. The regular behavior of NMs (Au, Pt, Pd, and Ru) depending on the grain sizes (specific surfaces) of pyrite crystals along with the narrow range of the ratios of structural and surface components of the concentrations of different NMs points to NM coprecipitation with pyrite during the same productive stage. No capture of NM-containing carbonaceous phases took place, which should violate the regularity of Au distribution in pyrites of the Sukhoi Log deposit. 相似文献
887.
V. Yu. Kuznetsov E. V. Tabuns G. A. Cherkashev V. E. Bel’tenev F. E. Maksimov K. A. Kuksa L. I. Lazareva S. B. Levchenkoa I. E. Zherebtsov 《Doklady Earth Sciences》2018,478(1):26-30
The results of 230Th/U dating and mineralogical–geochemical studies of sulfide ores from the Irinovskoe hydrothermal field and the Severo-Zapadnoe ore occurrence (Mid-Atlantic Ridge) are presented. Sulfides are represented primarily by copper–sulfide ores with 12–30% Cu content; sulfur- and zinc-sulfide ores are distributed less frequently. The analysis of a change in the composition of sulfides over time has made it possible to identify three stages of formation. Each stage assumes that mineral associations are changed from high-temperature (sulfur and copper sulfide) to medium temperature (Zn–Cu and Zn-sulfide) sulfide ores. The whole age range of formation of the hydrothermal deposits falls within the time interval of about 58000–8000 for the Irinovskoe field and 69000–11000 years ago for the Severo-Zapadnoe ore occurrence. 相似文献
888.
N. V. Zubkova I. V. Pekov D. A. Ksenofontov V. O. Yapaskurt D. Yu. Pushcharovsky E. G. Sidorov 《Doklady Earth Sciences》2018,479(1):339-341
The crystal structure (R = 0.0194) of arcanite β-K2SO4 was studied on a single crystal from exhalations of the Arsenatnaya fumarole, Tolbachik Volcano (Kamchatka, Russia). The mineral crystallizes at a temperature of ≥350–430°C and associates with langbeinite, aphthitalite, hematite, tenorite, johillerite, and others. Arcanite is orthorhombic, Pnma, a = 7.4763(2) Å, b = 5.77262(16) Å, c = 10.0630(3) Å, V = 434.30(2) Å3, Z = 4. Its structure contains isolated SO4 tetrahedra, whereas K cations center ten- and nine-fold polyhedra. 相似文献
889.
A. V. Maslov Yu. V. Erokhin A. Gerdes Yu. L. Ronkin K. S. Ivanov 《Doklady Earth Sciences》2018,482(2):1275-1277
Detrital zircons (DZs) from arkose sandstones of the Upper Riphean Zilmerdak Formation (Southern Urals) yielded ages in the range of 3039–964 Ma. Grains with Late Karelian and Early and Middle Riphean ages compose 35, 34, and 26% of the total number of the analyzed zircons, respectively. This is similar to the age spectra of the Vendian sandstones (Asha Group), but it differs significantly from the age distribution typical of the Riphean stratotype sandstones. 相似文献
890.