全文获取类型
收费全文 | 97篇 |
免费 | 20篇 |
国内免费 | 55篇 |
专业分类
测绘学 | 11篇 |
大气科学 | 25篇 |
地球物理 | 22篇 |
地质学 | 41篇 |
海洋学 | 44篇 |
综合类 | 24篇 |
自然地理 | 5篇 |
出版年
2024年 | 1篇 |
2023年 | 1篇 |
2022年 | 4篇 |
2021年 | 5篇 |
2020年 | 4篇 |
2019年 | 4篇 |
2018年 | 5篇 |
2017年 | 7篇 |
2016年 | 4篇 |
2015年 | 6篇 |
2014年 | 3篇 |
2013年 | 2篇 |
2012年 | 9篇 |
2011年 | 5篇 |
2010年 | 16篇 |
2009年 | 8篇 |
2008年 | 7篇 |
2007年 | 4篇 |
2006年 | 16篇 |
2005年 | 3篇 |
2004年 | 3篇 |
2003年 | 4篇 |
2002年 | 2篇 |
2001年 | 2篇 |
2000年 | 3篇 |
1999年 | 5篇 |
1998年 | 2篇 |
1997年 | 5篇 |
1996年 | 2篇 |
1995年 | 7篇 |
1994年 | 3篇 |
1993年 | 5篇 |
1991年 | 2篇 |
1990年 | 2篇 |
1989年 | 1篇 |
1988年 | 1篇 |
1987年 | 4篇 |
1986年 | 1篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1976年 | 1篇 |
排序方式: 共有172条查询结果,搜索用时 750 毫秒
131.
The structure of current speed and the variability of volume transports of the Kuroshio in the Tokara-kaikyo and Osumi-kaikyo are discussed on the basis of data of KER in the period from 1977 to 1984. The average geostrophic transport through these two straits is estimated to be 24. 5×106 m3/s and only 1/12 of the transport is through the Osumi-kaiky5. Countercurrents on both sides of the Kuroshio trunk are observed in the Tokara-kaikyo. Calculation indicates that the average geostrophic current speed is less than the GEK current speed, systematically. On the basis of the current measurements, the northward transports through the Taiwan Strait in winter and summer are estimated to be 1. 05×106and 3. 16×106m3/s, respectively. From Chu's data (1976) the average transport of the Kuroshio flowing into the East China Sea passing through the passage east of Taiwan is about 29. 3×106m3/s. From Miita and Ogawa's data (1984) the average transport through the Tsushima-kaikyo is 3. 6×106m3/s. Thus the volume 相似文献
132.
133.
Zhang Shimin Wang Dandan Liu Xudong Ren Junjie Luo Minghui Zhang Guohong Zhao Guocun Wang Rui Zhang Yingli 《中国地震研究》2008,22(3):334-347
A test drilling exploration was implemented across the northern segment of the Nankou-Sunhe fault in the Beijing plain, and a combined borehole section was built by sequence stratigraphy, lithologic facies analysis, magnetic susceptibilityand absolute chronology to investigate the episodic activities of the fault since 60 ka BP. The results show that the active stages of the fault are 60 ka to 47 ka BP, 36 ka to 28 ka BP, and 16 ka BP to present. Other intervals are relatively stable. The average vertical slip rate is 0.35 mm/a from 60 ka to 37 ka BP, 0 mm/a from 37 ka to 3:2 ka BP,0.78 mm/a from 32 ka to 12 ka BP,and 0.35 mm/a since 12 ka BP. Compared with the conventional analyses on lithology and sedimentary facies, the sequence stratigraphy method has certain advantages in the studies of borehole strata comparison and episodic activity of buried faults. 相似文献
134.
135.
以数字线划图的质量要求及检查验收为例,从质量要求、检查方法和质量评定几个方面分析GB/T 17941.1-2000和GB/T17941-2008,GB/T 18316-2001和GB/T 18316-2008两对新旧国标之间的差异和联系。从中得出结论:新国标继承了旧国标中合理的部分,如两级检查一级验收制度等;摒弃了不合理的内容,如基于缺陷扣分法的质量评定方法。质量要求和检查内容更为全面,检查方法更易操作和实现,质量评定更为科学合理,参加评定的质量元素内容更完整。 相似文献
136.
137.
Interbasin freshwater,heat and salt transport through the boundaries of the East and South China Seas from a variable-grid global ocean circulation model 总被引:23,自引:0,他引:23
It has long been recognized that the circulation in the East China Sea (ECS) and Japan/East Sea (JES) is closely related with that in Pacific, especially with the Kuroshio (e.g., Nitani[1], Hi-daka[2]). Based on current measurements in the Taiwan Strait a… 相似文献
138.
济阳盆地中生代构造特征与油气 总被引:56,自引:6,他引:56
济阳盆地中生代构造主要包括:印支期NW向压性构造(褶皱及逆断层)、消亡的NW向负反转半地垒及半地堑、燕山期ENE向压性构造(褶皱或逆断层)、SN向地垒。印支期NW向压性构造是华北板块同扬子板块的聚敛运动的产物,而NW向负反转地垒和地堑、ENE向压性构造及SN向地垒导源于郯庐断裂的左旋剪切作用,新生代郯庐断裂右旋剪切运动导致上述构造消亡并成为隐伏构造。中生代隐伏构造为济阳盆地深层勘探提供了潜山圈闭( 相似文献
139.
太平洋-印度洋贯穿流南海分支在卡里马塔海峡的十年观测回顾 总被引:5,自引:2,他引:3
Wei Zexun Li Shujiang Susanto R. Dwi Wang Yonggang Fan Bin Xu Tengfei Sulistiyo Budi Adi T. Rameyo Setiawan Agus Kuswardani A. Fang Guohong 《海洋学报(英文版)》2019,38(4):1-11
除印度尼西亚贯穿流之外,南海贯穿流也是太平洋向印度洋输送海水的重要分支。尽管基于数值模拟等方法的研究早已指出,南海分支在太平洋-印度洋洋际交换中有重要作用,但是直到2007年之前,南海分支在卡里马塔海峡处的观测几乎是空白。本文回顾了自2007年起,通过中印尼合作项目"南海-印度尼西亚海水交换及对鱼类季节性洄游的影响(SITE)"在卡里马塔海峡开展的近十年观测,以及在此基础上进一步开展的"印度尼西亚贯穿流海域水交换、内波和混合观测及其生态效应(TIMIT)"观测项目,并对SITE和TIMIT观测取得的成果进行了总结。 相似文献
140.
A review on the South China Sea western boundary current 总被引:7,自引:2,他引:5
The advances in understanding the South China Sea (SCS) western boundary current (SCSwbc) have been reviewed since the works of Dale (1956) and Wyrtki (1961) in the middle of the 20th century. The features of the pattern of SCSwbc and the oceanic phenomena associated with it are focused on. The current is driven mainly by monsoon over the SCS and partially by winds over the tropical Pacific governed by the island rule. The SCSwbc exhibits strong seasonal variation in its direction and patterns. In winter, the current is strong and flows southwestward along the South China shelf and slope from the east of Dongsha Islands to the northern central Vietnamese coast, then turns to the south along the central and southern Vietnamese coast, and finally partially exits the SCS through the Karimata Strait. In summer and early fall, the SCSwbc can be divided into three segments based on their characteristics. The southern segment is stable, flowing northward from the Karimata Strait up to about 11 N, where it separates from the coast forming an eastward offshore current. The separation of the current from Vietnamese coast induces some striking features, such as upwelling and cold sea-surface temperature. The middle segment off the central Vietnamese coast may have a bimodal behavior: northward coastal current and meandering current in early summer (June-July), and cyclonic gyre in later summer and early fall (August-September). The northern segment is featured by the summer SCS Warm Current on the South China shelf and a southwestward subsurface current along the continental slope. 相似文献