全文获取类型
收费全文 | 11421篇 |
免费 | 2020篇 |
国内免费 | 2616篇 |
专业分类
测绘学 | 709篇 |
大气科学 | 2302篇 |
地球物理 | 3023篇 |
地质学 | 5549篇 |
海洋学 | 1280篇 |
天文学 | 671篇 |
综合类 | 1049篇 |
自然地理 | 1474篇 |
出版年
2024年 | 57篇 |
2023年 | 161篇 |
2022年 | 486篇 |
2021年 | 573篇 |
2020年 | 480篇 |
2019年 | 607篇 |
2018年 | 665篇 |
2017年 | 612篇 |
2016年 | 694篇 |
2015年 | 613篇 |
2014年 | 721篇 |
2013年 | 695篇 |
2012年 | 689篇 |
2011年 | 785篇 |
2010年 | 708篇 |
2009年 | 677篇 |
2008年 | 631篇 |
2007年 | 591篇 |
2006年 | 479篇 |
2005年 | 405篇 |
2004年 | 345篇 |
2003年 | 342篇 |
2002年 | 334篇 |
2001年 | 298篇 |
2000年 | 331篇 |
1999年 | 409篇 |
1998年 | 341篇 |
1997年 | 346篇 |
1996年 | 286篇 |
1995年 | 253篇 |
1994年 | 298篇 |
1993年 | 217篇 |
1992年 | 173篇 |
1991年 | 138篇 |
1990年 | 110篇 |
1989年 | 79篇 |
1988年 | 99篇 |
1987年 | 53篇 |
1986年 | 49篇 |
1985年 | 42篇 |
1984年 | 37篇 |
1983年 | 34篇 |
1982年 | 35篇 |
1981年 | 28篇 |
1980年 | 9篇 |
1979年 | 14篇 |
1978年 | 6篇 |
1975年 | 4篇 |
1958年 | 7篇 |
1954年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 62 毫秒
41.
Ferromanganese crusts were found in carbonates of tectonostratigraphic units located in the northern and southern areas of the eastern External Subbetic of the Betic Cordilleras (SE Spain). The crusts are associated with four stratigraphic discontinuities of the Jurassic pelagic swells sequences: D1 (Late Carixian-Early Domerian), D2 (Middle Toarcian-Early Bajocian), D3 (Middle Bathonian-Middle Oxfordian), D4 (Early Tithonian-Late Albian). Two main textural types of crusts are distinguished. Type I crusts are thin and characterized by the presence of goethite, quartz, albite and phyllosilicates. Moreover, they show Si, Al, Mg, Na, Ti and K contents close to the European Shale Composite contents and Fe/Mn ratios (>350) higher than type II crusts. Type II crusts occur as thicker banded laminae and/or macrooncoids. They consist mainly of goethite and Mn-oxyhydroxides, which are enriched in REE, Co, Ni and Cu and show a strong Ce positive anomaly. After stratigraphical, mineralogical and geochemical data, the crust formation would be produced by the exposition of bottom sediments during long periods to a thin layer of oxidizing sea and porewater enriched in metallic elements. The textural and compositional variations between crusts can be explained by taking into account the bathymetric conditions. In shallower swells, the precipitation of a thick layer of banded type II crusts and in deeper areas, thin type I crusts were formed. Organic influence was only important in crusts from D3 of the northern area where textural evidence indicates the existence of seasonal periodically alternation between organism accretion and fine sedimentation. These were preceded and followed by phases in which the inorganic precipitation of oxides prevailed together with the fine sedimentation. 相似文献
42.
Origin of Fe-Ti Oxide Ores in Mafic Intrusions: Evidence from the Panzhihua Intrusion, SW China 总被引:12,自引:0,他引:12
Pang Kwan-Nang; Zhou Mei-Fu; Lindsley Donald; Zhao Donggao; Malpas John 《Journal of Petrology》2008,49(2):295-313
Economic concentrations of Fe–Ti oxides occur as massive,conformable lenses or layers in the lower part of the Panzhihuaintrusion, Emeishan Large Igneous Province, SW China. Mineralchemistry, textures and QUILF equilibria indicate that oxidesin rocks of the intrusion were subjected to extensive subsolidusre-equilibration and exsolution. The primary oxide, reconstructedfrom compositions of titanomagnetite in the ores and associatedintergrowths, is an aluminous titanomagnetite (Usp40) with 40wt % FeO, 34 wt % Fe2O3, 16·5 wt % TiO2, 5·3 wt% Al2O3, 3·5 wt % MgO and 0·5 wt % MnO. This compositionis similar to the bulk composition of the oxide ore, as inferredfrom whole-rock data. This similarity strongly suggests thatthe ores formed from accumulation of titanomagnetite crystals,not from immiscible oxide melt as proposed in earlier studies.The occurrence of oxide ores in the lower parts of the Panzhihuaintrusion is best explained by settling and sorting of densetitanomagnetite in the ferrogabbroic parental magma. This magmamust have crystallized Fe–Ti oxides relatively early andabundantly, and is likely to have been enriched in Fe and Tibut poor in SiO2. These features are consistent with fractionationof mantle-derived melts under relatively high pressures (10kbar), followed by emplacement of the residual magma at 5 kbar.This study provides definitive field and geochemical evidencethat Fe–Ti oxide ores can form by accumulation in ferrogabbro.We suggest that many other massive Fe–Ti oxide depositsmay have formed in a similar fashion and that high concentrationsof phosphorus or carbon, or periodic fluctuation of fO2 in themagma, are of secondary importance in ore formation. KEY WORDS: ELIP; Fe–Ti oxide ore; layered intrusion; Panzhihua; QUILF 相似文献
43.
The Simpevarp area is one of the alternative sites being considered for the deep geological disposal of high level radioactive waste in Sweden. In this paper, a coupled regional groundwater flow and reactive solute transport model of the Simpevarp area is presented that integrates current hydrogeological and hydrochemical data of the area. The model simulates the current hydrochemical pattern of the groundwater system in the area. To that aim, a conceptual hydrochemical model was developed in order to represent the dominant chemical processes. Groundwater flow conditions were reproduced by taking into account fluid-density-dependent groundwater flow and regional hydrogeologic boundary conditions. Reactive solute transport calculations were performed on the basis of the velocity field so obtained. The model was calibrated and sensitivity analyses were carried out in order to investigate the effects of heterogeneities of hydraulic conductivity in the subsurface medium. Results provided by the reactive transport model are in good agreement with much of the measured hydrochemical data. This paper emphasizes the appropriateness of the use of reactive solute transport models when water-rock interaction reactions are involved, and demonstrates what powerful tools they are for the interpretation of hydrogeological and hydrochemical data from site geological repository characterization programs, by providing a qualitative framework for data analysis and testing of conceptual assumptions in a process-oriented approach. 相似文献
44.
Wenchuan Earthquake: Way of thinking is changed 总被引:9,自引:0,他引:9
Yong Chen Li Li Juan Li Gang Li 《《幕》》2008,31(4):374-377
On 12 May, 2008, at 14:28:04 local time, an Ms 8.0 earthquake struck the Wenchuan County, Sichuan Province, in southwest China (Figure 1). This quake left about 70,000 people dead, 18,000 missing and over 370,000 injured. In the 75 days after the main shock, 20,000 aftershocks were recorded, which included 241 with Ms≥4.0, 205 with 4.0≤M≤4.9, 30 with 5.0≤Ms≤5.9, and 6 with Ms≥6.0. The largest aftershock took place 13 days after the main shock, in Qingchuan County, 110 km northeast of the epicenter of the quake (Chen, 2008). The losses from the quaketriggered geological disasters accounted for over a third of the total quake losses, which is extremely rare in the history of earthquake disasters. Secondary disasters, such as landslides, rockslides, landfalls, debris flows, etc., were widely distributed. Large numbers of buildings collapsed, including ones with steel reinforcing in the area of the epicenter. Infrastructure was badly damaged. In many areas, communications, and power and water supplies were cut off. The earthquake left over 35 large quake-dammed lakes, which threatened further disasters in the catchment areas. 相似文献
45.
46.
Fayun Liang Mingyi Zhao Chengrui Qin Yajie Jia Zhongwei Wang Guiping Yue 《Marine Georesources & Geotechnology》2020,38(1):114-121
AbstractThe construction of a 100-km road network is planned on a land reclamation area in the Oujiang Estuary in China. The embankment had a height of 4 m and a base width of 60 m. The reclamation area is newly filled by a 3-m dredger fill on a 48-m thick layer of marine clay. Estimation of the settlement of the future road network is difficult. To guide the construction of the road network, a 1/100-scale centrifuge model test was performed with a marine clay sample from the construction site to simulate the layered settlements and evaluate the drainage effect of prefabricated vertical drains in the dredger fill in the following 10 years. The results of the centrifuge modeling test are verified by 10-month in situ monitoring, which shows agreement between the centrifuge modeling test results and the in situ results. The test results indicate that additional time is needed to reinforce the newly added dredger fill by the surcharge preloading method to uplift the elevation of the reclamation area with dredger fill. 相似文献
47.
48.
Tetraploid induced by physical and chemical methods in Jinjiang oyster(Crassostrea rivularis) 总被引:1,自引:0,他引:1
Rong Shoubai Shi Shumei Mo Qirong Liu Shaeqiong Liang Ze Zhao Xiuzhu Tong Wangdong Li Shouwu Li Yimin 《海洋学报(英文版)》1994,13(2):275-283
TetraploidinducedbyphysicalandchemicalmethodsinJinjiangoyster(Crassostrearivularis)¥RongShoubai,ShiShumei,McQirong,LiuShaeqio... 相似文献
49.
冲绳海槽北部稀土元素沉积地球化学研究 总被引:4,自引:1,他引:4
本文对冲绳海槽北部海底表层沉积物和4个柱将苦芯沉积物样品的稀土元素沉积地球化学特征进行了系统的分析。研究结果表明:调查区表层沉积物REE的分布主要与沉积物的物质组成有关,特别是海洋生物沉积物组份的比例不仅影响REE总量的分布,而且影响标准化REE分布模式的形态。 相似文献
50.