全文获取类型
收费全文 | 1987篇 |
免费 | 467篇 |
国内免费 | 535篇 |
专业分类
测绘学 | 201篇 |
大气科学 | 342篇 |
地球物理 | 606篇 |
地质学 | 1136篇 |
海洋学 | 256篇 |
天文学 | 64篇 |
综合类 | 160篇 |
自然地理 | 224篇 |
出版年
2024年 | 13篇 |
2023年 | 34篇 |
2022年 | 131篇 |
2021年 | 160篇 |
2020年 | 116篇 |
2019年 | 141篇 |
2018年 | 164篇 |
2017年 | 146篇 |
2016年 | 122篇 |
2015年 | 145篇 |
2014年 | 136篇 |
2013年 | 154篇 |
2012年 | 150篇 |
2011年 | 160篇 |
2010年 | 124篇 |
2009年 | 106篇 |
2008年 | 91篇 |
2007年 | 89篇 |
2006年 | 68篇 |
2005年 | 51篇 |
2004年 | 62篇 |
2003年 | 61篇 |
2002年 | 81篇 |
2001年 | 64篇 |
2000年 | 60篇 |
1999年 | 50篇 |
1998年 | 46篇 |
1997年 | 35篇 |
1996年 | 39篇 |
1995年 | 14篇 |
1994年 | 38篇 |
1993年 | 29篇 |
1992年 | 23篇 |
1991年 | 12篇 |
1990年 | 12篇 |
1989年 | 10篇 |
1988年 | 8篇 |
1987年 | 8篇 |
1986年 | 4篇 |
1985年 | 3篇 |
1984年 | 6篇 |
1983年 | 2篇 |
1982年 | 8篇 |
1980年 | 5篇 |
1977年 | 1篇 |
1974年 | 1篇 |
1964年 | 1篇 |
1958年 | 1篇 |
1954年 | 2篇 |
1949年 | 1篇 |
排序方式: 共有2989条查询结果,搜索用时 31 毫秒
81.
虹口乡八角庙出露完整的映秀—北川断裂带剖面断层岩,高分辨率磁化率测试揭示出多个具有高磁化率特征的断层岩带。系统的岩石磁学分析证明一层褐色断层岩相对围岩具有最大的磁化率值,存在新生成的磁铁矿和拥有相似的天然剩磁(NRM)和非磁滞剩磁(ARM)强度衰减过程。高磁化率特征是含铁顺磁性矿物受到断层滑移过程产生摩擦生热作用生成磁铁矿所致。同时断层岩还获得了热剩磁,记录了地震活动磁学信息。结合汶川地震科学钻探项目1号孔(WFSD-1)磁化率和岩石磁学研究结果,说明映秀—北川断裂带包含多层具有高磁化率特征的断层岩,暗示了多次强震的发生。具有高磁化率特征的断层岩可以作为判定地震活动的标志之一。 相似文献
82.
为了探索鲣鱼(Katsuwonus pelamis)鱼头眼窝肉中的DHA(C22:6n3)和EPA(C20:5n3)的抗抑郁活性效果,采用现代食品分离技术分离提取鲣鱼眼窝肉中的DHA和EPA,并对其抗抑郁活性效果进行研究。研究结果发现,当DHA和EPA剂量分别为50,100和300mg/kg时,能够对强迫游泳实验和悬尾实验的小鼠产生抗抑郁作用,其中低剂量(50mg/kg)表现为最活跃。DHA和EPA还能够对引起头抽动综合征的5-羟色胺小鼠产生轻微的增强作用。通过高效液相色谱-电化学法同时测定小鼠大脑区域内主要的单胺类神经递质及其代谢产物。本实验发现,与用压力媒介物处理的小鼠相比,DHA和EPA能够显著增加主要神经递质5-羟色胺和去肾上腺素在小鼠海马体、下丘脑及皮质层中的浓度,并减少5-羟色胺的代谢。DHA和EPA能够在预测抗抑郁特性的动物模型中(强迫游泳实验,悬尾实验)明确其具有抗抑郁活性效果,具有潜在的生物医学应用前景和环保效应。 相似文献
83.
Influence of anthropogenic pressure and seasonal upwelling on coral reefs in Nha Trang Bay (Central Vietnam)
下载免费PDF全文
![点击此处可从《Marine Ecology》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Konstantin S. Tkachenko Temir A. Britayev Nguyen H. Huan Mikhail V. Pereladov Yuri Y. Latypov 《Marine Ecology》2016,37(5):1131-1146
The growing coastal development, dredging and dumping activities, overfishing and expansion of marine cage culture in Nha Trang Bay (NTB) of Central Vietnam since the beginning of the 2000s have resulted in a dramatic decrease of live coral cover. Surveys conducted in April–May 2013 and the same period in 2014 revealed that with an increase in distance from the outer part of the bay towards the mainland, the rivers’ influxes and dredged areas, coral cover decreased from 75% to 0.6% and species richness from 63 to 5, while the abundance of macroalgae increased from 0% to 56%. These changes correlate with differences in the concentration of suspended sediments on the same gradient. The abundance of the crown‐of‐thorns starfish Acanthaster planci and of the echinoid Diadema setosum significantly increased between the first estimation in 1998 and the survey in 2014, from 0 to 1.7 individuals (ind.) per 100 m?2 and from 50.8 to 94.5 ind. per 100 m?2, respectively, contributing to coral loss and intensive bioerosion of the reef framework in the bay. The large sizes of adult colonies of tabulate Acropora on the remote stations with negligible sedimentation and eutrophication loads were inconsistent with the assumptions that temperature‐induced coral bleaching or cyclones could be the major impacts in Nha Trang Bay. Analysis of the 16‐year thermal history of the bay did not reveal any instances in which the coral thermal bleaching threshold had been exceeded up to the present study. Seasonal upwelling, which occurs annually in the vicinity of Central Vietnam, may contribute to mitigation of thermal anomalies within NTB and to the maintenance of healthy coral communities on the remote reefs with relatively low anthropogenic impact. 相似文献
84.
为了预测鲣鱼(Katsuwonus pelamis)调理食品的货架期,将鲣鱼调理食品贮藏在25°C、30°C、35°C温度条件下,通过测定在贮藏期间菌落总数、挥发性盐基氮、过氧化值三个指标的变化,分别对这三个指标与贮藏时间、温度建立一级动力学模型,来预测鲣鱼调理食品的货架期。经计算得出,菌落总数预测模型中的活化能(Ea)及指前因子(k0)分别为30.96 k J/mol和2.06×103,挥发性盐基氮预测模型中的的活化能及指前因子分别为24.35 k J/mol和75.1,过氧化值预测模型中的活化能及指前因子分别为48.75 k J/mol和2.92×106。在32°C和37°C条件下验证动力学模型,结果表明相对误差分别为–5.52%和–6.45%,准确性较好。进一步推算得出,在18°C和23°C常温下贮藏鲣鱼调理食品,产品的货架期为209d和172d。 相似文献
85.
Hydrothermal Fluid Sources of the Fengjia Barite–fluorite Deposit in Southeast Sichuan,China: Evidence from Fluid Inclusions and Hydrogen and Oxygen Isotopes
下载免费PDF全文
![点击此处可从《Resource Geology》网站下载免费的PDF全文](/ch/ext_images/free.gif)
The Fengjia barite–fluorite deposit in southeast Sichuan is a stratabound ore deposit which occurs mainly in Lower Ordovician carbonate rocks. Here we present results from fluid inclusion and oxygen and hydrogen isotope studies to determine the nature and origin of the hydrothermal fluids that generated the deposit. The temperature of the ore‐forming fluid shows a range of 86 to 302 °C. Our detailed microthermometric data show that the temperature during mineralization of the fluorite and barite in the early ore‐forming stage was higher than that during the formation of the calcite in the late ore‐forming stage. The salinity varied substantially from 0.18% to 21.19% NaCl eqv., whereas the density was around 1.00 g/cm3. The fluid composition was mainly H2O (>91.33%), followed by CO2, CH4 and traces of C2H6, CO, Ar, and H2S. The dominant cation was Na+ and the dominant anion Cl‐, followed by Ca2+, SO42‐, K+, and Mg2+, indicating a mid–low‐temperature, mid‐low‐salinity, low‐density NaCl–H2O system. Our results demonstrate that the temperature decreased during the ore‐forming process and the fluid system changed from a closed reducing environment to an open oxidizing environment. The hydrogen and oxygen isotope data demonstrate that the hydrothermal fluids in the study area had multiple sources, primarily formation water, as well as meteoric water and metamorphic water. Combined with the geological setting and mineralization features we infer that the stratabound barite–fluorite deposits originated from mid–low‐temperature hydrothermal fluids and formed vein filling in the fault zone. 相似文献
86.
87.
88.
JIA Fudong ZHANG Changqing LIU Huan HUA Zhixin KONG Zhigang MENG Xuyang 《《地质学报》英文版》2018,92(2):864-865
正Objective Located near the intersection of Yangtze craton,TibetSanjiang orogen and Songpan-Ganzi orogen of Northwest Yunnan Province,the Mahuaping deposit is a unique large-scale tungsten-beryllium-fluorite ore deposit ever discovered in this area.In recent years,many studies have been carried out in Sanjiang Tethyan metallogenic belt and 相似文献
89.
90.