全文获取类型
收费全文 | 4083篇 |
免费 | 927篇 |
国内免费 | 637篇 |
专业分类
测绘学 | 193篇 |
大气科学 | 231篇 |
地球物理 | 1226篇 |
地质学 | 2675篇 |
海洋学 | 365篇 |
天文学 | 13篇 |
综合类 | 216篇 |
自然地理 | 728篇 |
出版年
2024年 | 24篇 |
2023年 | 66篇 |
2022年 | 113篇 |
2021年 | 162篇 |
2020年 | 190篇 |
2019年 | 194篇 |
2018年 | 176篇 |
2017年 | 226篇 |
2016年 | 229篇 |
2015年 | 198篇 |
2014年 | 248篇 |
2013年 | 330篇 |
2012年 | 229篇 |
2011年 | 246篇 |
2010年 | 201篇 |
2009年 | 266篇 |
2008年 | 271篇 |
2007年 | 276篇 |
2006年 | 279篇 |
2005年 | 211篇 |
2004年 | 218篇 |
2003年 | 186篇 |
2002年 | 159篇 |
2001年 | 131篇 |
2000年 | 112篇 |
1999年 | 105篇 |
1998年 | 109篇 |
1997年 | 101篇 |
1996年 | 71篇 |
1995年 | 72篇 |
1994年 | 54篇 |
1993年 | 30篇 |
1992年 | 35篇 |
1991年 | 27篇 |
1990年 | 19篇 |
1989年 | 19篇 |
1988年 | 18篇 |
1987年 | 8篇 |
1986年 | 7篇 |
1985年 | 7篇 |
1984年 | 7篇 |
1983年 | 2篇 |
1982年 | 3篇 |
1981年 | 4篇 |
1980年 | 4篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1954年 | 2篇 |
排序方式: 共有5647条查询结果,搜索用时 15 毫秒
951.
A new Mazon-Creek-type fossil specimen is described as Sumixam maximus gen. and sp. nov., assigned to the taxon Archaeorthoptera Béthoux and Nel, 2002 (composed of Orthoptera and some fossil relatives): it exhibits one of the diagnostic character states of this taxon, which is the fusion of CuA (emerging from M + CuA) with CuP, or a branch of it. A more precise taxonomic assignment is out of reach. The new taxon exhibits a fusion of the anterior branch of MA with RP, and a point of divergence of MA and MP located near the point of divergence of CuA (from M + CuA), but lack a branching of CuPa. This unique combination of character states is probably derived with respect to a number of contemporaneous species. Sumixam maximus gen. and sp. nov. is most likely the closest known relative of the panorthopterans, which include all the recent Archaeorthoptera. 相似文献
952.
PHILIP J. ASHWORTH GREGORY H. SAMBROOK SMITH JAMES L. BEST JOHN S. BRIDGE STUART N. LANE IAN. A. LUNT ARNOLD J. H. REESINK CHRISTOPHER J. SIMPSON ROBERT E. THOMAS 《Sedimentology》2011,58(7):1860-1883
The depositional stratigraphy of within‐channel deposits in sandy braided rivers is dominated by a variety of barforms (both singular ‘unit’ bars and complex ‘compound’ bars), as well as the infill of individual channels (herein termed ‘channel fills’). The deposits of bars and channel fills define the key components of facies models for braided rivers and their within‐channel heterogeneity, knowledge of which is important for reservoir characterization. However, few studies have sought to address the question of whether the deposits of bars and channel fills can be readily differentiated from each other. This paper presents the first quantitative study to achieve this aim, using aerial images of an evolving modern sandy braided river and geophysical imaging of its subsurface deposits. Aerial photographs taken between 2000 and 2004 document the abandonment and fill of a 1·3 km long, 80 m wide anabranch channel in the sandy braided South Saskatchewan River, Canada. Upstream river regulation traps the majority of very fine sediment and there is little clay (< 1%) in the bed sediments. Channel abandonment was initiated by a series of unit bars that stalled and progressively blocked the anabranch entrance, together with dune deposition and stacking at the anabranch entrance and exit. Complete channel abandonment and subsequent fill of up to 3 m of sediment took approximately two years. Thirteen kilometres of ground‐penetrating radar surveys, coupled with 18 cores, were obtained over the channel fill and an adjacent 750 m long, 400 m wide, compound bar, enabling a quantitative analysis of the channel and bar deposits. Results show that, in terms of grain‐size trends, facies proportions and scale of deposits, there are only subtle differences between the channel fill and bar deposits which, therefore, renders them indistinguishable. Thus, it may be inappropriate to assign different geometric and sedimentological attributes to channel fill and bar facies in object‐based models of sandy braided river alluvial architecture. 相似文献
953.
954.
平原河网地区河流曲度及城市化响应 总被引:5,自引:0,他引:5
河流曲度是河流平面形态的重要表征指标,以平原河网地区典型区域——上海为例,分析了20世纪50年代中心城区高密度河网的河流曲度特征,诊断了近60年以来快速城市化对区域河网及河流曲度的影响。研究认为:①近60年来上海中心城区河网密度下降幅度达67.22%,高强度人类活动导致区域河网水系分枝结构与自然规律完全相反;②平原河网地区是顺直型河流的典型发育区域,研究初期上海中心城区顺直型河流占85.40%,进一步分析表明曲度小于1.1的河流比例高达70.57%,河流形态接近于直线型;③上海中心城区消亡河流以顺直型为主,其消亡速率约为较高曲度河流的12倍,采用加权平均曲度指标描述区域河网萎缩对河流曲度的影响具有更好的直观性和科学性;④上海城市河流综合整治实践中,工程水利的倾向性强于生态水利,60.9%的河流整治项目开展了裁弯取直工程措施。 相似文献
955.
Mixed carbonate-siliciclastic sedimentation is common in the Upper Permian-Lower Tri-assic in the western Sichuan(四川) basin.The extensional movement was strong in the Late Permian,resulting in differential uplifting of fault blocks.During this period,there was an extensive retrogres-sion.The Kangdian(康滇) ancient land progressive uplifted and enlarged,forming the major prove-nance of terrigenous clastics.In Changxingian age,mixed terrigenous-carbonate sedimentation was dis-tributed in the area between Dafeis... 相似文献
956.
957.
958.
在对汶泗河冲洪积平原水文地质条件和污染源现状进行阐述的基础上,对不同含水岩组无机组分指标进行了分析,表明浅层孔隙水和部分地区岩溶裂隙水无机组分含量大幅增高,深层孔隙水无机物含量则变化不大。在有机污染方面,浅层孔隙水有机物检出率26.8%,但含量很低,远未达到饮用水标准限值;岩溶裂隙水有机物检出率46.7%,检出率相对较高,局部地段有机物超标;深层孔隙水有机物基本未检出。该区地下水污染评价结果表明,浅层孔隙水和岩溶裂隙水无机污染呈面状污染特征,且污染程度较重,而有机污染则呈现点状污染特征,且污染程度总体较轻。对研究区地下水污染现状,提出了地下水安全供水对策。 相似文献
959.
Suhaila Abdul Hamid Mohd Ravi Che Salmah Hamady Dieng Abu Hassan Ahmad Tomomitsu Satho Fumio Miake 《湿地科学》2011,9(3):240-250
A field study was performed at rivers in Gunung Jerai forest reserve(Kedah,Malaysia) to assess seasonal changes in mayfly community structure and abundance in relation to altitude and water physicochemistry.Rivers at lower(Batu Hampar River) and higher(Teroi River) elevations were visited through dry and wet seasons in September 2007 to August 2008.Monthly visits were made to 20 sites on each river,and water and aquatic insects were sampled using D-pond aquatic nets.Water was warmer,more acid,and more turbid in Teroi River during wet season.Ammonia was the only nutrient exhibiting significant seasonal variations(greater during wet season).Chemical oxygen demand content was higher in Teroi River where biochemical oxygen demand content was low during wet season.Species richness was higher in Batu Hampar River,but displayed seasonal variations only in Teroi River.Among the eight families encountered,Baetidae was the commonest.Baetid abundance was usually high during wet season,and those belonging to the dominant genus(Baetis) were more abundant in Teroi River.Heptageniidae was the second commonest family;its predominant genus,Thalerospyrus was more abundant in Teroi River during dry season.Caenidae,Leptophlebiidae and Oligoneuriidae were only found in Batu Hampar River where their abundances peaked during dry season,i.e.,Habrophlebiodes sp.and Isonychia sp.Ephemerellidae and Teloganodidae occurred only in Teroi River,with the first found only during dry season.Mayflies were recorded under very distinct physicochemical conditions,illustrating their potential usefulness for assessing water quality.Caenids,leptophlebids,oligoneurids ephemerellids and teloganodids seem to be particularly sensitive to temperature,acidity,turbidity,chemical oxygen demand and biochemical oxygen demand,parameters that varied with river altitude. 相似文献
960.