全文获取类型
收费全文 | 2331篇 |
免费 | 296篇 |
国内免费 | 260篇 |
专业分类
测绘学 | 630篇 |
大气科学 | 134篇 |
地球物理 | 198篇 |
地质学 | 982篇 |
海洋学 | 608篇 |
天文学 | 7篇 |
综合类 | 187篇 |
自然地理 | 141篇 |
出版年
2024年 | 13篇 |
2023年 | 38篇 |
2022年 | 73篇 |
2021年 | 76篇 |
2020年 | 94篇 |
2019年 | 130篇 |
2018年 | 65篇 |
2017年 | 145篇 |
2016年 | 125篇 |
2015年 | 123篇 |
2014年 | 146篇 |
2013年 | 148篇 |
2012年 | 184篇 |
2011年 | 164篇 |
2010年 | 111篇 |
2009年 | 111篇 |
2008年 | 135篇 |
2007年 | 117篇 |
2006年 | 128篇 |
2005年 | 90篇 |
2004年 | 83篇 |
2003年 | 75篇 |
2002年 | 78篇 |
2001年 | 66篇 |
2000年 | 51篇 |
1999年 | 55篇 |
1998年 | 42篇 |
1997年 | 46篇 |
1996年 | 47篇 |
1995年 | 23篇 |
1994年 | 29篇 |
1993年 | 23篇 |
1992年 | 15篇 |
1991年 | 11篇 |
1990年 | 7篇 |
1989年 | 6篇 |
1988年 | 2篇 |
1987年 | 3篇 |
1986年 | 5篇 |
1985年 | 2篇 |
1984年 | 2篇 |
排序方式: 共有2887条查询结果,搜索用时 250 毫秒
61.
In the Haushi-Huqf (Eastern Central Oman) as in other parts of the Arabian platform, a major sedimentary break is recorded between the Early Aptian carbonates (Shu'aiba Formation) and the Albian orbitolinid-rich marls (Nahr Umr Formation). The unconformity corresponds to a succession of events: (1) a brusque interruption of the regressive sequence of the Shu'aiba limestone (algae and small rudistid build-ups); (2) a stratigraphic gap related to the Late Aptian; (3) the development of a thick ferruginous crust (hardground) that covered the top surface of the Shu'aiba; the hardground is related to a forced flooding surface; (4) the Shu'aiba was rapidly drowned and buried under the Nahr Umr marls. Moreover, the Shu'aiba limestone was subject to faulting NW–SE-trending normal faults before lithification and formation of the ferruginous crust. The faulting episode is clearly dated: post-Early Aptian and pre-Albian. The signification of the faulting remains hypothetical. The syndiagenetic NW–SE normal faults may correspond to ‘en echelon’ faults, combined with transcurrent fault movements (for example the Haushi-Nafun Fault). The possible causes of these intra-platform transcurrent movements are discussed. To cite this article: C. Montenat, P. Barrier, C. R. Geoscience 334 (2002) 781–787. 相似文献
62.
J. Escuder Viruete R. Carbonell D. Martí M. J. Jurado A. Prez-Estaún 《Tectonophysics》2003,361(1-2):97-120
The 3-D seismic tomographic data are used together with field, core and well log structural information to determine the detailed 3-D architecture of fault zones in a granitic massif of volume 500×575×168 m at Mina Ratones area in the Albalá Granitic Pluton. To facilitate the integration of the different data, geostatistical simulation algorithms are applied to interpolate the relatively sparse structural (hard) control data conditioned to abundant but indirect 3-D (soft) seismic tomographic data. To effectively integrate geologic and tomographic data, 3-D migration of the velocity model from the time domain into the depth domain was essential. The resulting 3-D model constitutes an image of the fault zone architecture within the granitic massif that honours hard and soft data and provides an evaluation of the spatial variability of structural heterogeneities based on the computation of 3-D experimental variograms of Fracture Index (fault intensity) data. This probabilistic quantitative 3-D model of spatially heterogeneous fault zones is suitable for subsequent fluid flow simulations. The modeled image of the 3-D fault distribution is consistent with the fault architecture in the Mina Ratones area, which basically consists of two families of subvertical structures with NNE–SSW and ENE–WSW trends that displaces the surfaces of low-angle faults (North Fault) and follows their seismically detected staircase geometry. These brittle structures cut two subvertical dykes (27 and 27′ Dykes) with a NNE–SSW to N–S trend. The faults present high FI (FI>12) adjacent bands of irregular geometry in detail that intersect in space delimiting rhombohedral blocks of relatively less fractured granite (FI<6). Both structural domains likely correspond with the protolith and the damaged zone/fault core in the widely accepted model for fault zone architecture. Therefore, the construction of 3-D grids of the FI in granitic areas affected by brittle tectonics permits the quantitative structural characterization of the rock massif. 相似文献
63.
徐羹慧 《沙漠与绿洲气象(新疆气象)》2003,26(5):1-3,8
目前,业务平台、预报制作系统技术已成为气象台天气预报的关键技术,也是我国与发达国家技术发展的主要差距之一。本文从科学技术论的角度,研究气象台预报制作系统发展的历史及其发展的阶段性,归纳了技术发展的基本特征,提出了预报制作系统技术跨越式发展的应对措施。 相似文献
64.
GIS中的应用模型及其管理研究 总被引:47,自引:1,他引:47
本文通过对GIS模型库系统的研究,讨论了GIS应用模型的管理及GIS应用模型发展中的若干问题。 相似文献
65.
66.
扬子地块西缘灯影组层控铅锌矿床成因的地球化学论证 总被引:5,自引:0,他引:5
扬子地块西缘灯影组层控铅锌矿床成因的地球化学论证邵世才(有色总公司北京矿产地质研究所,北京100012)李朝阳(中国科学院地球化学研究所,贵阳550002)关键词层控铅锌矿床地球化学矿床成因扬子地块西缘1矿床地质特征扬子地块西缘灯影组铅锌矿床呈南北向... 相似文献
67.
INTRODUCTIONThestrataofMesoprotCrozoicandNeoproterozoicaredevelopedcompletelyinthesouthpartoftheNorthetnaplatformandconsistofthreesystems,inasCendingorder,Jixiaulan,QingbaikouanandSlman.BasedonadetailedinvestigationontheolltcropandthecomprehenSiveanalysis,wediscussthecharaCterofsequencestratigraphyandthecorrelationoftheMemo--Neoproterozoicinthearea.FnThRrsor~unCrsANDPARA~unCrsMeSO--NooprotffezoicRadonalfortigraphyThesouthernpartofNorthChinaplatformherereferstotheareasincluding… 相似文献
68.
69.
70.
未经蚀变的海相碳酸盐岩的碳,锶同位素组成代表了原始海水的同位素组成,在确定样品末经显著蚀变的基础上,本文测定了上扬子地区晚古生代7条剖面238个海相碳酸盐岩样品的碳、锶同位素组成,分布了它们的测试结果和演化曲线,为其他相关研究提供了可利用的基础参照数据。 相似文献