全文获取类型
收费全文 | 1828篇 |
免费 | 373篇 |
国内免费 | 588篇 |
专业分类
测绘学 | 74篇 |
大气科学 | 529篇 |
地球物理 | 439篇 |
地质学 | 1017篇 |
海洋学 | 247篇 |
天文学 | 48篇 |
综合类 | 187篇 |
自然地理 | 248篇 |
出版年
2024年 | 3篇 |
2023年 | 30篇 |
2022年 | 74篇 |
2021年 | 96篇 |
2020年 | 62篇 |
2019年 | 83篇 |
2018年 | 90篇 |
2017年 | 92篇 |
2016年 | 98篇 |
2015年 | 84篇 |
2014年 | 121篇 |
2013年 | 96篇 |
2012年 | 88篇 |
2011年 | 88篇 |
2010年 | 88篇 |
2009年 | 96篇 |
2008年 | 91篇 |
2007年 | 84篇 |
2006年 | 48篇 |
2005年 | 60篇 |
2004年 | 61篇 |
2003年 | 79篇 |
2002年 | 61篇 |
2001年 | 68篇 |
2000年 | 80篇 |
1999年 | 128篇 |
1998年 | 116篇 |
1997年 | 96篇 |
1996年 | 81篇 |
1995年 | 85篇 |
1994年 | 74篇 |
1993年 | 60篇 |
1992年 | 53篇 |
1991年 | 39篇 |
1990年 | 34篇 |
1989年 | 22篇 |
1988年 | 11篇 |
1987年 | 12篇 |
1986年 | 16篇 |
1985年 | 8篇 |
1984年 | 3篇 |
1983年 | 7篇 |
1982年 | 7篇 |
1981年 | 4篇 |
1980年 | 4篇 |
1979年 | 1篇 |
1978年 | 5篇 |
1977年 | 1篇 |
1976年 | 1篇 |
排序方式: 共有2789条查询结果,搜索用时 218 毫秒
991.
992.
韩家岩体与天井山金矿空间上密切相关.对韩家岩体的成因存在不同看法:依据“斑状”外貌,有人主张是燕山期花岗斑岩;依据隐约可见的片麻状构造,有人认为是晋宁期灵山岩体.鉴于其具有重要的找矿指示意义,本文通过岩石学、岩石地球化学、同位素年代学等方面的研究,认为韩家岩体是由灵山岩体蚀变而成的绢英岩.天井山金矿中的金多以自然金形式产于石英大脉的晚期裂隙中,并与石英-绢云母-含铁碳酸盐-硫化物细脉共生.研究表明,这些裂隙与绢英岩体顶部的石英网脉带贯通,两者具有相同蚀变矿物组合和流体来源.据此,本文认为与绢英岩化有关的岩浆-构造-蚀变作用是天井山金矿的核心成矿事件.由于韩家绢英岩体具有区域尺度的找矿标志,这对天井山矿区及其外围进一步找矿具有重要的指导意义. 相似文献
993.
Separating the effects of climate change and human activities on runoff over different time scales in the Zhang River basin 总被引:2,自引:0,他引:2
Sidong Zeng Jun Xia Hong Du 《Stochastic Environmental Research and Risk Assessment (SERRA)》2014,28(2):401-413
Most studies on separating the effects of climate change and human activities on runoff are mainly conducted at an annual scale with few analyses over different time scales, which is especially essential for regional water resources management. This paper investigates the impacts of climate change and human activities on runoff changes at annual, seasonal and monthly time scales in the Zhang River basin in North China. Firstly, the changing trends and inflection point are analyzed for hydro-climatic series over different time scales. Then the hydrological modeling based method and sensitivity based method are used to separate the effects. The results show that the effect of climate change is stronger than that of human activities on annual runoff changes. However, the driving factors on runoff are different at seasonal scale. In the wet season, the effect of human activities on runoff, accounting for 57 %, is stronger than that of climate change, while in the dry season climate change is the dominant factor for runoff reduction and the contribution rate is 72 %. Furthermore, the effects of climate change and human activities on monthly runoff changes are various in different months. The separated effects over different time scales in this study may provide more scientific basis for the water resources adaptive management over different time scales in this basin. 相似文献
994.
The complex permittivity of targeted objects is an important factor that influences its microwave radiation and scattering characteristics. In the quantitative research of microwave remote sensing, the study of the dielectric properties of the vegetation to establish the relationship between its specific physical parameters and complex permittivity is fundamental. In this study, six categories of vegetation samples were collected at the city of Zhangye, a key research area of the Heihe watershed allied telemetry experimental research. The vector network analyzer E8362B was used to measure the complex permittivity of these samples from 0.2 to 20 GHz by the coaxial probe technique. The research focused mainly on the corn leaves, and an empirical model was established between the gravimetric moisture and the real/imaginary parts of complex permittivity at the main frequency points of microwave sensors. Furthermore, the empirical model and the classical Debye-Cole model were compared and verified by the measured data collected from the Huailai County of Hebei Province. The results show that the newly-established empirical model is more accurate and more practical as compared to the traditional Debye-Cole model. 相似文献
995.
The oxygen isotopic values of aquatic plant cellulose and carbonates in Lake Caohai sediments were measured using a continuous flow isotopic ratio mass spectrometer(CF-IRMS).Because of predictable oxygen isotopic fractionation between cellulose and its source water,the oxygen isotopic composition of paleo-lake water has been established quantitatively.Combined oxygen isotopic values of cellulose and carbonates were used in the‘Craig’equation to determine paleotemperatures and their variation in the lake during the past 500 years.Results show that the paleotemperature trend correlates well with meteorological records from Weining.There are four notable cold intervals at Lake Caohai over the past 500 years,namely 1540–1570AD,1670–1715AD,1780–1870AD and 1900–1930AD,and the former three cold intervals have been observed in the conventional Little Ice Age(LIA).These cold periods at Lake Caohai correspond well with those recorded from tree ring,peat,and ice core data from adjacent regions,particularly temperature those inferred fromδ18O of peat cellulose from Hongyuan Southwestern China.The trend in paleotemperature variations at Lake Caohai are also consistent with both the change of Indian summer monsoon,derived fromδ18O values of a stalagmite in Dongge,and a recorded shift in solar activity.The findings of this study illustrate that coupled analysis ofδ18O values of cellulose and carbonates from lake sediments may be used as a paleotemperature proxy.These results also provide further evidence of the existence of LIA in southwestern China. 相似文献
996.
997.
根据当前欧盟征收国际航空碳税政策的国际环境,介绍欧盟航空碳税的历史沿革、具体政策、二氧化碳排放监测方法,就各国反应及其国际影响进行分析.欧盟航空碳税可能会导致全球航空业成本增加,并最终转嫁给消费者;欧盟航空碳税对发达国家航空公司影响较小,而对发展中国家的航空公司影响较大.鉴于欧盟航空碳税对中国航空业的影响,建议尽早制定相关的碳排放标准,维护中国应有的发展权与话语权. 相似文献
998.
999.
1000.
岩溶关键带及其碳循环研究进展 总被引:1,自引:0,他引:1
岩溶关键带的范畴包含了大气-(降水)-植被-土壤-裂隙-基岩-水组成的“碳-水-钙”循环强烈的表层岩溶带以及岩溶管道-洞穴-地下河-隔水层组成的巨大岩溶地下空间,岩溶关键带碳循环是岩溶地球系统科学研究的前沿方向。总结概括了岩溶地球系统科学发展至今的岩溶关键带范畴内碳循环及其对大气CO2源汇效应的研究成果,包括早期碳运移模型、当前主流的区域岩溶碳汇量的计算方法和结果以及“生物碳泵”的新发现等,讨论了当前岩溶碳循环研究框架过于单一或不一致以及碳周转时间尺度等问题,提出应对岩溶关键带碳输入、赋存以及碳输出的各个环节做出系统化监测,通过联网在线高分辨率监测站点的建设以及“3S”技术实现点位到区域的研究,使岩溶碳汇在全球碳循环模型中的重要性更具说服力。 相似文献