全文获取类型
收费全文 | 867篇 |
免费 | 318篇 |
国内免费 | 289篇 |
专业分类
测绘学 | 108篇 |
大气科学 | 119篇 |
地球物理 | 274篇 |
地质学 | 589篇 |
海洋学 | 204篇 |
天文学 | 11篇 |
综合类 | 98篇 |
自然地理 | 71篇 |
出版年
2024年 | 13篇 |
2023年 | 34篇 |
2022年 | 56篇 |
2021年 | 73篇 |
2020年 | 64篇 |
2019年 | 72篇 |
2018年 | 75篇 |
2017年 | 67篇 |
2016年 | 65篇 |
2015年 | 62篇 |
2014年 | 53篇 |
2013年 | 75篇 |
2012年 | 80篇 |
2011年 | 82篇 |
2010年 | 75篇 |
2009年 | 67篇 |
2008年 | 73篇 |
2007年 | 91篇 |
2006年 | 70篇 |
2005年 | 62篇 |
2004年 | 27篇 |
2003年 | 27篇 |
2002年 | 31篇 |
2001年 | 36篇 |
2000年 | 19篇 |
1999年 | 8篇 |
1998年 | 3篇 |
1997年 | 1篇 |
1996年 | 4篇 |
1992年 | 1篇 |
1990年 | 3篇 |
1989年 | 1篇 |
1988年 | 2篇 |
1957年 | 1篇 |
1954年 | 1篇 |
排序方式: 共有1474条查询结果,搜索用时 15 毫秒
61.
There are abundant coal and coalbed methane(CBM)resources in the Xishanyao Formation in the western region of the southern Junggar Basin,and the prospects for CBM exploration and development are promising.To promote the exploration and development of the CBM resources of the Xishanyao Formation in this area,we studied previous coalfield survey data and CBM geological exploration data.Then,we analyzed the relationships between the gas content and methane concentration vs.coal seam thickness,burial depth,coal reservoir physical characteristics,hydrogeological conditions,and roof and floor lithology.In addition,we briefly discuss the main factors influencing CBM accumulation.First,we found that the coal strata of the Xishanyao Formation in the study area are relatively simple in structure,and the coal seam has a large thickness and burial depth,as well as moderately good roof and floor conditions.The hydrogeological conditions and coal reservoir physical characteristics are also conducive to the enrichment and a high yield of CBM.We believe that the preservation of CBM resources in the study area is mainly controlled by the structure,burial depth,and hydrogeological conditions.Furthermore,on the basis of the above results,the coal seam of the Xishanyao Formation in the synclinal shaft and buried at depths of 700-1000 m should be the first considered for development. 相似文献
62.
人工神经网络在爆破块度预测中的应用研究 总被引:1,自引:0,他引:1
利用人工神经网络模型对爆破块度进行预测,实验结果表明,该方法是完全可行的。通过对实验样本数据进行归一化处理后再对人工神经网络模型进行训练和预测,其预测精度会得到大大提高。 相似文献
63.
黄河高含沙量水体在弱潮陆相河口入海,80 %的泥沙在河口附近快速堆积。过去研究发现,黄河三角洲潮滩表层沉积物呈现非均匀固结状态。为了揭示该现象产生的机制,在黄河刁口流路三角洲叶瓣潮坪上,现场取土配置黄河口快速沉积形成的流体状堆积物,研究快速沉积的粉质海床土在波浪和潮波作用下的孔压响应及非均匀固结过程。利用静力触探、十字板剪切试验、孔隙水压力监测等原位测试手段,实时测定快速沉积的海床土强度和孔压变化过程。研究发现,快速沉积的粉质土在自重作用下的固结速度很快,正常固结完成后,强度随时间的发展依然不断增加,沿深度方向出现类似原状土体的固结非均匀现象和似超固结状态;在波浪和潮波作用下快速沉积粉质土孔压沿深度出现非均匀变化,在波浪作用下出现了超静孔压的积累。分析发现,该固结状态和强度沿深度方向非均匀变化是由于土体在潮波及潮波和波浪的联合作用下形成的;潮滩表层土体在波浪荷载长期作用下形成硬壳层。 相似文献
64.
以赣江流域峡山站以上为研究区域,利用栅格型数字高程数据,提取数字流域水系及其空间拓扑关系,在此基础上建立数字水文模型。赣江上游峡山站以上集水区域包含21198个空间分辨率为30s的栅格,采用就近移植法将降水数据及蒸发数据插值到每个栅格上,计算峡山站的径流过程。日模型中选取1978~1985年为参数率定期,1986~1987年为参数验证期,以多年径流量误差最小为目标函数。次洪模型中采用前16场洪水用于参数率定,后6场用于模拟验证,以洪水总量、洪峰流量、峰现时间按许可误差统计合格率最高和确定性系数最大为目标函数。结果显示,率定期16场洪水中14场合格,验证期6场洪水均合格,表明栅格型新安江模型模拟效果良好。 相似文献
65.
CHEN Guohui LU Shuangfang LI Jinbu WANG Weiming TIAN Shansi SHAN Junfeng HU Yingjie MAO Jinli HAN Xia 《《地质学报》英文版》2015,89(Z1):8-10
<正>1 Introduction There is a set of organic rich shale at E22S4sub-member in damnintun sag.The organic material is typically type I.In recent years,breakthrough was obtained in shale oil exploration.The wettability of organic and inorganic pore is different.As a result,the mobility of oil in organic and inorganic pore is different.So it’s necessary to distinguish 相似文献
66.
67.
68.
TTG(Tonalite-Trondhjemite-Granodiorite) gneisses,a major component of Precambrian continental crust,play a significant role in understanding the process and mechanism of the crustal evolution in the early periods of the Earth. In terms of field occurrence,there are two kinds of Archean TTGs in the NCC(North China Craton): intercalated and non-intercalated TTGs. In this contribution,we make a comprehensive comparison of these two types of TTGs from the typical areas(Lushan and Hengshan) in the NCC with an aim to constrain their petrogenesis. The results suggest that they have similar mineral assemblages of Pl + Qtz + Bt ± Amp ± Kfs but different field appearances and geochemical compositions,thus probably reflecting different source materials and tectonic settings. Differences in the contents of characteristic elements,such as Sr,REE and HFSE,suggest that the nonintercalated TTGs in Hengshan were generated at deeper levels than those of intercalated TTGs in Lushan. Constraints from element contents and geochemical modeling results are consistent with derivation from dual sources involving both garnet amphibolite and rutile-bearing eclogite residues for the non-intercalated TTGs in Hengshan,whereas the compositions of intercalated TTGs in Lushan indicate that they were formed by partial melting with amphibolite to garnet-amphibolite residues. Moreover,accumulation of plagioclase is also required in the petrogenesis of intercalated TTGs in Lushan,at least for part of them. In addition,the non-intercalated TTGs in Hengshan display distinctly higher Mg O,Mg#,Cr and Ni values and lower SiO_2 average contents compared to the intercalated TTGs in Lushan. These features suggest that the former magma,at least a part,might have interacted with the mantle wedge during ascent. Considering all the above factors and in combination with the whole-rock Nd and zircon Hf isotopic data,it is suggested that the non-intercalated TTGs in Hengshan were produced by partial melting of subducted slab contaminated by the overlying mantle wedge at deeper levels and high pressures,whereas the intercalated TTGs in Lushan were generated by melting of the thickened lower crust at lower pressures and shallower depths. The tectonic settings of the two types of TTGs shed new light on the growth of the NCC. 相似文献
69.
70.