全文获取类型
收费全文 | 12489篇 |
免费 | 3012篇 |
国内免费 | 4376篇 |
专业分类
测绘学 | 2420篇 |
大气科学 | 1966篇 |
地球物理 | 1975篇 |
地质学 | 7420篇 |
海洋学 | 2981篇 |
天文学 | 185篇 |
综合类 | 1069篇 |
自然地理 | 1861篇 |
出版年
2024年 | 83篇 |
2023年 | 298篇 |
2022年 | 749篇 |
2021年 | 918篇 |
2020年 | 787篇 |
2019年 | 784篇 |
2018年 | 739篇 |
2017年 | 687篇 |
2016年 | 737篇 |
2015年 | 865篇 |
2014年 | 821篇 |
2013年 | 1069篇 |
2012年 | 1147篇 |
2011年 | 1119篇 |
2010年 | 1123篇 |
2009年 | 1050篇 |
2008年 | 1132篇 |
2007年 | 996篇 |
2006年 | 1103篇 |
2005年 | 822篇 |
2004年 | 652篇 |
2003年 | 407篇 |
2002年 | 466篇 |
2001年 | 447篇 |
2000年 | 324篇 |
1999年 | 154篇 |
1998年 | 62篇 |
1997年 | 50篇 |
1996年 | 31篇 |
1995年 | 26篇 |
1994年 | 23篇 |
1993年 | 18篇 |
1992年 | 25篇 |
1991年 | 15篇 |
1990年 | 12篇 |
1989年 | 7篇 |
1988年 | 6篇 |
1987年 | 14篇 |
1986年 | 6篇 |
1985年 | 10篇 |
1984年 | 13篇 |
1983年 | 13篇 |
1982年 | 8篇 |
1981年 | 4篇 |
1979年 | 9篇 |
1976年 | 3篇 |
1964年 | 3篇 |
1957年 | 5篇 |
1954年 | 9篇 |
1928年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
991.
992.
结合课题组前期的研究成果,通过对墙体中不同材料的本构模型、墙体中裂缝、多种材料的联结以及墙体边界条件的研究与探讨,运用通用有限元程序ANSYS对密肋复合墙体进行非线性有限元分析;并在试验结果与有限元模拟的基础上,依据极限平衡理论,建立起来复合墙体的斜截面抗剪极限承载力公式。理论分析与试验研究表明:复合墙体非线性有限元模型能够较好地模拟墙体内力和变形发展的全过程,描述裂缝的形成和扩展,对于实际工程和科学研究具有足够的精度;墙体斜截面抗剪承载力公式与实测值吻合较好,具有一定的精度,满足工程设计需要。 相似文献
993.
东南沿海地区的断裂与地震 总被引:1,自引:0,他引:1
中国东部,相对来说东南沿海地区的地震活动较为频繁,断裂构造也十分发育。地震活动与断裂构造有非常密切的关系,震中与断裂构造的空间分布也关系密切。通过对东南沿海大量震例的调查和研究,分析三组断裂与地震的关系,得出东南沿海地区东西向、北东向和北西向的三组断裂构造,分别构成了区内的衰减构造、控震构造和发震构造,形成了东南沿海陆缘构造活动带。 相似文献
994.
Introduction In the probability analysis method of seismic risk considering time-space inhomogeneity of seismic activity and adopted commonly in China (State Seismological Bureau, 1996) (called in-homogeneous distribution model for short), the division of seismic statistical regions, delimitation of potential seismic sources and estimation of seismicity parameters are the main links that affect significantly the estimation of ground motion parameters of a site. HUANG and WU (2005) studied … 相似文献
995.
Introduction The northwest of China includes Tarim, Junggar and Qaidam basins, and Kunlun, Tianshan, Altun and Qilian mountains, as well as the north part of the Tibetan Plateau. For a long time, the study of lithosphere structures and dynamics in this area has been a popular topic in geoscience, and has yielded many results. For example, TANG (1994) and LI et al (1998) suppose that the tectonic structure of Tarim Basin is various with geological periods, which changes many times betwee… 相似文献
996.
Miocene Bahean stratigraphy in the Longzhong Basin, northern central China and its implications in environmental change 总被引:1,自引:0,他引:1
LI Jijun ZHANG Jun SONG Chunhui ZHAO Zhijun ZHANG Yong WANG Xiuxi ZHANG Jianming CUI Qiaoyu 《中国科学D辑(英文版)》2006,49(12):1270-1279
Fossil mammal-riched Neogene strata are widely distributed in the southeast corner of the huge Longzhong Basin at Tianshui, Gansu Province, northern central China. Hipparion weihoense, a typical member of late Middle Miocene Bahean stage, was recently excavated at Yaodian along a well-exposed outcrop. Owing to the importance of the Bahean stage in the mammalian evolution and its potential for environmental change, we suggested a name of Yaodian Formation for the stratigra- phy, which is correlated to the Bahe Formation at Lantian, Shaanxi. High resolution paleomagnetic dating of the section shows that the Yaodian Formation covers the period between 11.67 Ma and 7.43 Ma, with the site bearing Hipparion weihoense being estimated at about 10.54―10.30 Ma, providing first magnetostratigraphic chronology for the Bahean Stage. The Yaodian Formation consists of fluvial channel deposits (11.67―10.40 Ma) at the bottom, floodplain deposits in the middle (10.40―9.23 Ma) and shallow lake sediments at the top (9.23―7.43 Ma). This upward fining sequence suggests that the relief in nearby mountain ranges such as West Qinling to the south and Huajia Ling to the north was greatly reduced after long-term denudation, fluvial transport capacity was low, and finally the drainage system was disintegrated, replaced with broad-shallow lakes in which only fine sediments like mud and marlite were deposited, indicating an old stage of development of a planation surface. A remarkable shift in ecology and climatic environment was found at 7.4―7.7 Ma when paleoclimate changed from early warm humid to late dry as indicated by sedimentary facies changed from early shallow lake sequence to late eolian red clays and a former coniferous-deciduous mixed forest was replaced by grassland, leading to great growth of Hipparion Fauna of Baodean stage in the region. Therefore, it is estimated that the present high relief of Qinling and drainage pattern did not come into being until Late Pliocene in response to intensive neotectonism and climate change. 相似文献
997.
Humid Little Ice Age in arid central Asia documented by Bosten Lake, Xinjiang, China 总被引:15,自引:0,他引:15
J. A. Holmes 《中国科学D辑(英文版)》2006,49(12):1280-1290
Short sediment cores retrieved from Bosten Lake, the largest inland freshwater lake in China, were used to explore humidity and precipitation variations in arid central Asia during the past millennium. The chronology of the cores was established using 137Cs, 210Pb and AMS 14C dating re- sults. Multi-proxy high-resolution analysis, including pollen ratios of Artemisia and Chenopodiaceae (A/C), carbonate content and grain size, indicates that the climate during the past millennium can be divided into three stages: a dry climate between 1000―1500 AD, a humid climate during the Little Ice Age (LIA) (c. 1500―1900 AD), and a warm dry period after 1900 AD. On centennial timescales, the climate change in northwestern China during the past 1000 years is characterized by oscillations between warm-dry and cold-humid climate conditions. All the proxies changed significantly and indi- cate increased precipitation during the LIA, including increased pollen A/C ratios and pollen concen- trations, decreased carbonate content and increased grain size. The humid period during the LIA re- corded by the Bosten Lake sediments is representative of arid central Asia and is supported by nu- merous records from other sites. During the LIA, the water runoff into the Keriya River and Tarim River in the Tarim Basin increased, while the ice accumulation in the Guliya ice core increased. Additionally, the lake levels of the Aral and Caspian Sea also rose, while tree-ring analysis indicates that precipita- tion increased. We hypothesize that both the lower temperature within China and the negative anomalies of North Atlantic Oscillation (NAO) during this period may have contributed to the humid climate within this area during LIA. 相似文献
998.
999.
东亚南北地震带大震活动性研究 总被引:6,自引:0,他引:6
根据中国南北地震带与青藏-印尼“歹”字型构造带在成因上的联系,提出东亚南北地震带的观点,认为该地震带包含蒙古、中国西部、缅甸和印尼苏门答腊地区。研究了该带大地震活动的同步性、主体活动区的有序转移、大地震之间的多次相关迁移与重复等特征,并划分出了该带的5个大震活跃幕:1887-1912年、1913-1937年、1938-1957年、1958-1976年、1977-2005年。苏门答腊2004年12月26日8.7级和2005年3月29日8.5级巨震标志着该地震带最近一次以主体活动区南移到苏门答腊为特征的活跃时段即将结束。尽管未来一、两年内地震带的中部存在发生7级地震的有利时段,但结合强震图像异常指标反映的孕震状况分析,未来7级地震危险区尚不明朗。 相似文献
1000.