全文获取类型
收费全文 | 17040篇 |
免费 | 1941篇 |
国内免费 | 3066篇 |
专业分类
测绘学 | 922篇 |
大气科学 | 2491篇 |
地球物理 | 3396篇 |
地质学 | 8461篇 |
海洋学 | 2347篇 |
天文学 | 1871篇 |
综合类 | 1000篇 |
自然地理 | 1559篇 |
出版年
2024年 | 115篇 |
2023年 | 322篇 |
2022年 | 739篇 |
2021年 | 966篇 |
2020年 | 856篇 |
2019年 | 890篇 |
2018年 | 1102篇 |
2017年 | 1032篇 |
2016年 | 1029篇 |
2015年 | 768篇 |
2014年 | 988篇 |
2013年 | 1036篇 |
2012年 | 1009篇 |
2011年 | 1104篇 |
2010年 | 993篇 |
2009年 | 942篇 |
2008年 | 888篇 |
2007年 | 923篇 |
2006年 | 825篇 |
2005年 | 434篇 |
2004年 | 376篇 |
2003年 | 432篇 |
2002年 | 499篇 |
2001年 | 454篇 |
2000年 | 341篇 |
1999年 | 364篇 |
1998年 | 285篇 |
1997年 | 308篇 |
1996年 | 258篇 |
1995年 | 256篇 |
1994年 | 232篇 |
1993年 | 182篇 |
1992年 | 164篇 |
1991年 | 110篇 |
1990年 | 95篇 |
1989年 | 111篇 |
1988年 | 79篇 |
1987年 | 63篇 |
1986年 | 57篇 |
1985年 | 46篇 |
1984年 | 42篇 |
1983年 | 41篇 |
1982年 | 41篇 |
1981年 | 26篇 |
1980年 | 24篇 |
1979年 | 29篇 |
1978年 | 17篇 |
1977年 | 17篇 |
1975年 | 22篇 |
1973年 | 17篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
71.
72.
73.
74.
基于GIS技术的三江平原热量资源评价 总被引:1,自引:0,他引:1
基于GIS技术,使用黑龙江省气象观测站和农垦、森工系统观测站的气温资料,以及数字高程模型(DEM)资料,运用趋势面分析法和线性内插法得到三江平原栅格化的热量资源数据。分析表明,三江平原纬度和高度因子对各项热量指标分布均有影响,经度因子主要影响年平均气温、4月平均气温、7月平均气温、≥0℃积温和≥10℃积温;佳木斯西部、双鸭山西部、鸡西大部热量资源较丰富,而青黑山、完达山、老爷岭和太平岭等地区热量资源相对较差。分析结果为合理开发利用三江平原热量资源提供了依据。 相似文献
76.
O. Yu. Bogdanova A. I. Gorshkov G. V. Novikov Yu. A. Bogdanov 《Geology of Ore Deposits》2008,50(6):462-469
The mineralogy and structural features of the main types of ferromanganese deposits—nodules, micronodules, Co-bearing crusts, crustlike nodules, and low-temperature hydrothermal manganese crusts and ferruginous ochers—are considered. The correlation between their mineral composition and structure is shown. The proposed classification of mineral types is based on characteristic assemblages of Fe and Mn minerals. 相似文献
77.
V. I. Ivashchenko M. Valkama K. Sundblad A. I. Golubev V. Yu. Alekseev 《Doklady Earth Sciences》2011,440(1):1307-1311
A wide application of modern precision research techniques to the studies of Pitkyaranta ores allowed us to find increased
contents of indium (to 0.33%), silver (447 g/t), gold (0.2–0.4 g/t), and palladium (0.2 g/t). A series of rare minerals previously
not found here was also discovered. Among ore minerals, these are roquesite, zavartskite, electrum, stutzite, altaite, bismite,
glaucodot, cervelleite, hedleyite, pavonite, cannonite, plantnerite, lindkvistite, ashoverite, etc. The discovery of roquesite
and electrum is the most important in terms of metallogeny. Roquesite (indium sulfide) is found in Karelia for the first time.
The highest indium contents in direct correlation to those of zinc are characteristic for polymetallic ores of the Pitkyaranta
ore fields with sphalerite as the concentrating mineral (to 0.5% of In). The predicted zinc resources are evaluated to ∼2.5
million t for the Pitkyaranta group of ore deposits, and to 400 000 t for the Hopunvaara region. Respectively, the resources
of indium amount to ∼2400 t (total) and 600 t for the Hopunvaara region. 相似文献
78.
The paper deals with results of general and systematic analysis of data from deep-sea drilling (360 stations) and a personal study carried out by the authors on the distribution and facies location of authigenic zeolites in the sedimentary mantle of the World Ocean.The scheme of zeolite distribution, compiled for the Holocene—Pleistocene, Miocene, Eocene and Cretaceous periods confirmed the previously established global stratification of zeolites. It showed that the main mass of phillipsite was formed during the Pleistocene—Holocene, while clinoptilolite was a predominant mineral in Eocene and Cretaceous rocks. Both zeolites were wide-spread in the Oligocene and Miocene. Facies location and paragenesis of associated minerals as well as the original material of their formation are different for phillipsite and clinoptilolite.The most probable reasons for vertical stratification of oceanic zeolites of global significance are changes of the character of volcanism in time and general evolution of sedimentation in the World Ocean. 相似文献
79.
G. T. Skublov Yu. B. Marin S. G. Skublov Yu. N. Tarasenko 《Geology of Ore Deposits》2008,50(7):535-550
Volkhovites—tektite-like glasses—have been detected in the Holocene glacial drift along the right bank of the Volkhov River. A cryptomagmatic model of their formation and pre-Holocene age of volkhovite melts, cinder, and frothed glasses has been suggested (Skublov et al., 2007). Four geochemical types of volkhovites are distinguished: (1) manganous (Mn, Fe, Cr, V, Si, Nb, Pb, H), (2) magnesian (Mg, Al, Ti, F, B), (3) potassic (K, Rb, Cs), and (4) calcic (Ca, REEs, Ba, U, Th, Ta, Hf, Y, Sc, Cl). In light of the geochemical data, volkhovites are regarded as natural silicate glasses of kimberlite-carbonatite composition. Their types are called kimberlitic (Mn type), kimberlitic-carbonatitic (Mg type), lamproitic-carbonatitic (K type), and carbonatitic (Ca type). Volkhovites are suggested to be indicators of undiscovered diamond mineralization of kimberlite or carbonatite (Chagatai) types. 相似文献
80.
Wei Yong Rong Zhaojin Zhong Jun Chai Lihui Yue Xin an Liu Libo Yu Sheng Zhu Rixiang Wan Weixing 《地球科学进展》2017,32(1):15-20
It has been 60 years since the space physics as new branch of geophysics started to grow in 1957 when the space age was opened by a small satellite called sputnik. The knowledge of Earth and planetary space has been significantly extended and deepened, but the questions we are facing today are more challenging. A consensus reached is that we have to regard the Earth (planet) as an integrated system including all spheres from the inner core to the magnetosphere, and we should try to investigate some questions standing on the ground of interdisciplinary study, especially those questions related to Earth’s (planetary) evolution. Space environment as the outer part of a planetary system, commonly exists in all planets but also exhibits strong diversity. Here, we introduce the short history of basic ideas and methods of comparative study, the advantages on understanding of some issues of global scale, and the prospect from comparative perspective. 相似文献