全文获取类型
收费全文 | 880篇 |
免费 | 111篇 |
国内免费 | 111篇 |
专业分类
测绘学 | 58篇 |
大气科学 | 95篇 |
地球物理 | 362篇 |
地质学 | 252篇 |
海洋学 | 154篇 |
天文学 | 110篇 |
综合类 | 21篇 |
自然地理 | 50篇 |
出版年
2024年 | 3篇 |
2023年 | 5篇 |
2022年 | 15篇 |
2021年 | 9篇 |
2020年 | 9篇 |
2019年 | 26篇 |
2018年 | 21篇 |
2017年 | 26篇 |
2016年 | 21篇 |
2015年 | 23篇 |
2014年 | 29篇 |
2013年 | 39篇 |
2012年 | 28篇 |
2011年 | 28篇 |
2010年 | 42篇 |
2009年 | 53篇 |
2008年 | 52篇 |
2007年 | 49篇 |
2006年 | 54篇 |
2005年 | 64篇 |
2004年 | 51篇 |
2003年 | 47篇 |
2002年 | 33篇 |
2001年 | 31篇 |
2000年 | 41篇 |
1999年 | 33篇 |
1998年 | 24篇 |
1997年 | 28篇 |
1996年 | 28篇 |
1995年 | 26篇 |
1994年 | 32篇 |
1993年 | 21篇 |
1992年 | 19篇 |
1991年 | 13篇 |
1990年 | 19篇 |
1989年 | 12篇 |
1988年 | 16篇 |
1987年 | 3篇 |
1986年 | 7篇 |
1985年 | 9篇 |
1984年 | 5篇 |
1983年 | 3篇 |
1982年 | 1篇 |
1981年 | 2篇 |
1980年 | 1篇 |
1978年 | 1篇 |
排序方式: 共有1102条查询结果,搜索用时 382 毫秒
81.
生物成因与无机成因文石的FTIR光谱区别 总被引:4,自引:1,他引:4
对16种贝壳交叉页片层中生物成因文石的FT IR谱进行测量,并与无机成因文石进行对比和统计分析后,首次发现生物成因与无机成因文石的FT IR光谱有明显可区分的特征,生物成因文石2ν带(面外弯曲振动)频率平均值为863.4 cm-1,而无机成因文石该带的平均值为855.5 cm-1,两者频率位移达7.9 cm-1。因此文石的2ν带可作为指纹带鉴别生物和无机成因文石。 相似文献
82.
成像光谱矿物识别和填图技术是中国国土资源调查和监测重点发展的高新技术之一。笔者以国土资源调查应用为主要目标,研究了成像光谱矿物识别和矿物填图技术实用化中的一些关键技术问题。分析了白云母和绿泥石两种重要蚀变矿物的光谱特征及光谱变异特征;以新疆东天山黄山地区的HyMap数据为例,对目前已较为系统化的成像光谱识别技术(如MNF变换、像元纯度指数PPI和N维可视化端元识别NDVI)在典型蚀变矿物识别和填图中的应用进行介绍。 相似文献
83.
84.
Earthquake codes have been revised and updated depending on the improvements in the representation of ground motions, soils and structures. These revisions have been more frequently seen in recent years. One of the key changes in earthquake codes has been performed on the design spectra. In this paper, the design spectra recommended by Turkish Earthquake Code and three other well known codes (Uniform Building Code, Eurocode 8, and International Building Code) are considered for comparison. The main purpose of this study is to investigate the differences caused by the use of different codes in the dynamic analysis and seismic verification of given types of buildings located at code defined different sites. The differences in expressions and some important points for elastic and inelastic spectra defined by the codes are briefly illustrated in tables and figures. Periods, base shears, lateral displacements and interstory drifts for the analyzed buildings located at code defined ground type are comparatively presented. 相似文献
85.
Bohdan Kíbek Ivana Sýkorov Jan Paava Vladimír Machovi
《International Journal of Coal Geology》2007,72(3-4):240-256
Marine black shales of the Lower Cambrian Niutitang Formation in southern China host Mo–Ni–platinum group elements (PGE) mineralization confined to a phosphate- and pyrite-rich stratiform body (max. 20-cm thick). The H/C atomic ratio, carbon isotopic composition, FTIR spectra of bulk organic matter, and spectra of extractable part of organic matter indicate similar sources and thermal evolution of organic matter in barren and mineralized black shales.The morphology and relative abundance of organic particles in barren and mineralized shales are different. In barren black shales, organic particles comprise only elongated bodies and laminae 2–10 μm across or elongated larger bodies (> 10 μm) with Rmax = 2.96–5.21% (Type I particles). Mineralized black shales contain Type I particles in rock matrix (90–95 vol%), small veinlets or irregular organic accumulations (Type II particles, 1–5 vol%) that display weak to well developed mosaic texture and a variable reflectance (Rmax = 3.55–8.65%), and small (< 1 to 5 μm) rounded or irregular Type III organic particles (1–4 vol%) distributed within phosphate nodules and sulphide rip-up clasts. Type III particles show similar reflectance as particles of Type I in rock matrix. Type I particles are interpreted as remnants of in situ bacterially reworked organic matter of cyanobacteria/algal type, Type II as solidified products or oil-derived material (migrabitumen), and Type III particles as remnants of original organic matter in phosphatized or sulphidized algal/microbial oncolite-like bodies. Equivalent vitrinite reflectances of Type I and III particles in barren and mineralized rocks are similar and correspond to semi-anthracite and anthracite. Micro-Raman spectra of organic particles in rocks display a wide belt in the area of 1600 cm− 1 (G belt) and approximately the same belt in the area of 1350 cm− 1 (D belt). The ratio of integrated areas of the two belts correlate with Rmax values.The Mo–Ni–PGE mineralized body is interpreted as to represent a remnant of phosphate- and sulphide-rich subaquatic hardground supplied with organic material derived from plankton and benthic communities as well as with algal/microbial oncolite-like bodies that originated in wave-agitated, shallow-water, nearshore environment. 相似文献
86.
87.
同时满足多个阻尼反应谱的人造地震动时程合成 总被引:1,自引:0,他引:1
应用M.Hirasawa和M.Watabe(1992)提出的方法,进行了相应的数学推导:即以满足某个阻尼比的反应谱的人造地震动作为初始时程,采用奇异值分解法,通过解线性方程组求出校正时程,并多次叠以逐步辐近 相似文献
88.
Identification method of weak seismic phases on the basis of wavelet packet transform 总被引:1,自引:0,他引:1
Xi-Qiang Liui Hui-Lan Zhou Zhi-Zhen Zheng Ping Shen Xuan-Hui Yang Yan-Lu Ma 《地震学报(英文版)》1998,11(4):431-439
This paper describes a sort of new method identifying seismic phase by the name of wavelet packet transform. Perfectness and
development of the wavelet packet transform is based upon the idea of its multiscale analysis. The method of wavelet packet
transform can depict the anomalous changes information of transient spectra of seismic wave onset, and come true the target
of identifying seismic phase especially weak seismic phase. Then this paper presents discriminating examples of simulating
digital signals and actual seismic phase. Compared with conventional seismic phase discrimination, studied results show that
the wavelet packet transform method is an available tool of weak signal analyses, and have unexampled merits and attractive
application foreground.
This research gets hold of Higher School Doctor Scientific Research Foundation (No. 157 WJ0704 9435611) and supported by the
National Natural Science Foundation (No. 49474211). 相似文献
89.
应用富时叶变换红外谱仪研究了三个启三绿柱石样(包括原样与热处理)。将3435cm^-1宽吸收带归属于与铁离子成键的水。谱图表明隧道水的大量脱去是在800℃以上的温度开始的,对于富碱样品,更可能是在1000℃以后开始。隧道中碱金属离子的阻塞作用是造成绿柱石隧道水难以失去的重要原因. 相似文献
90.
A numerical approach to the earthquake ground motion analysis is proposed for regions where no accelerograms are available. Using Haskell matrix techniques, the response spectra of a layered substratum for SV waves were calculated and then multiplied by the spectra corresponding to Brune's type pulses. The ground acceleration spectra were obtained for different angles of pulse incidence at the substratum base. The spectrum shape depends upon the substratum response and the pulse shape, while its level was related to the maximum ground acceleration corresponding to the expected maximum intensity. Transformation of the ground spectra into the time domain produced numerical accelerograms for horizontal and vertical components and for different angles of pulse incidence. Finally, a standard statistical procedure was applied to obtain the design response spectra used in engineering applications. 相似文献