全文获取类型
收费全文 | 776篇 |
免费 | 181篇 |
国内免费 | 429篇 |
专业分类
测绘学 | 108篇 |
大气科学 | 134篇 |
地球物理 | 91篇 |
地质学 | 699篇 |
海洋学 | 115篇 |
天文学 | 4篇 |
综合类 | 69篇 |
自然地理 | 166篇 |
出版年
2024年 | 15篇 |
2023年 | 30篇 |
2022年 | 54篇 |
2021年 | 70篇 |
2020年 | 60篇 |
2019年 | 57篇 |
2018年 | 47篇 |
2017年 | 66篇 |
2016年 | 42篇 |
2015年 | 56篇 |
2014年 | 45篇 |
2013年 | 81篇 |
2012年 | 68篇 |
2011年 | 61篇 |
2010年 | 68篇 |
2009年 | 59篇 |
2008年 | 93篇 |
2007年 | 57篇 |
2006年 | 86篇 |
2005年 | 59篇 |
2004年 | 50篇 |
2003年 | 30篇 |
2002年 | 31篇 |
2001年 | 26篇 |
2000年 | 11篇 |
1999年 | 9篇 |
1998年 | 6篇 |
1997年 | 5篇 |
1996年 | 12篇 |
1995年 | 3篇 |
1994年 | 4篇 |
1993年 | 3篇 |
1992年 | 3篇 |
1991年 | 3篇 |
1990年 | 3篇 |
1989年 | 5篇 |
1988年 | 1篇 |
1987年 | 3篇 |
1983年 | 3篇 |
1957年 | 1篇 |
排序方式: 共有1386条查询结果,搜索用时 15 毫秒
971.
港珠澳大桥人工岛对水沙动力环境的影响 总被引:1,自引:0,他引:1
为了评估港珠澳大桥人工岛建设对周边海区水沙动力环境的影响,针对人工岛设计及工程海区水沙特性,建立了整体潮流泥沙物理模型,系统研究了人工岛建设引起的动力地貌演变效应。试验结果表明,受岛体阻水影响,潮流在人工岛两端分别形成双向绕流,流速明显增大,并在岛桥结合部与岛隧结合部发育局部冲刷坑;人工岛背水面同时存在多个大小不一的强紊动小尺度回流,并具有不断形成、发育、发展到消亡的周期性变化过程。受人工岛自身位置、形态、尺度以及工程海区地形、水流、泥沙等因素影响,港珠澳大桥东、西两个人工岛引起的动力地貌演变效应,既在变化规律上具有较好的一致性,又在影响形式与程度上存在明显的差异性。 相似文献
972.
973.
974.
萍乡矿区位于萍乐坳陷带的西端,上三叠统安源组是该区主要含煤地层.成煤前的构造决定了沉积盆地的范围;可采煤层的赋存与同沉积构造密切相关,主要赋存于沉降幅度较大的同沉积向斜中及同沉积断层的下降盘;沉积后构造对煤层的控制作用主要表现在推覆构造对煤层的破坏和保存两方面. 相似文献
975.
应用数诸天气学的方法,对风湿病发生时的气象条件和天气系统进行分析归纳,得出成都地区风湿发生的高峰期主要是春末夏初,秋末冬初,风湿的发生主要与气象因子中的相对湿度,温度及其变化有很大的关系。成都地区与风湿发作的有关天气系统有西南低涡、南支槽、蒙古高压、高原低涡、高原切变线等,且在冷锋过境或持续低温阴雨的天气形势下会诱发风湿病发作,由此可通过数据统计的方法和天气学的方法来预测风湿病发病期,为预防风湿病提供依据。 相似文献
976.
LUO Liancong QIN Boqiang ZHU Guangwei SUN Xiaojing HONG Dalin GAO Yajun XIE Rui 《中国科学D辑(英文版)》2006,49(Z1)
A wave flume experiment was conducted to study nutrient fluxes at water-sediment interface of Meiliang Bay under different hydrodynamic conditions. The results reveal that hydrodynamics has remarkable effects on nutrient fluxes in this area. With a bottom wave stress of 0.019 N m-2 (equivalent to disturbance caused by wind SE 5-7 m s-1 at the sediment sample site of Meiliang Bay), the fluxes of TN, TDN and NH4+-N were separately 1.92× 10-3, -1.81 × 10-4 and 5.28× 10-4 mg m-2 s-1(positive for upward and negative for downward), but for TP, TDP and SRP, the fluxes were 5.69 × 10-4, 1.68 × 10-4 and -1.29 × 10-4 mgm-2 s-1. In order to calculate the released amount of nutrients based on these results, statistic analysis on the long-term meteorological data was conducted.The result shows that the maximum lasting time for wind SE 5-7 m s-1 in this area is about 15 h in summer. Further calculation shows that 111 t TN, 32 t NH4+-N, 34 t TP and 10 t TDP can be released into water (the sediment area was 47.45% of the whole surface area), resulting in concentration increase of 0.025, 0.007, 0.007 and 0.002 mg L-1 separately. With stronger disturbance (bottom wave stress is 0.217 N m-2 which is equivalent to disturbance caused by wind SE 10-11 m s-1 at the same site), there has been significant increase of nutrient fluxes (1.16× 10-2, 6.76×10-3, 1.14× 10-2 and 2.14× 10-3 mgm-2 s-1 for TN, DTN and NH4+-N and TP). The exceptions were TDP with flux having a decrease (measured to be 9.54× 10-5 mgm-2 s-1 ) and SRP with flux having a small increase (measured to be 5.42 × 10-5 mgm-2 s-1). The same statistic analysis on meteorological data reveal that the maximum lasting time for wind SE 10-11 m s-1 is no more than 5 h. Based on the nutrient fluxes and the wind lasting-time, similar calculations were also made suggesting that 232 t TN, 134.9 t TDN, 228 t NH4+-N, 42.7 t TP, 2.0 t TDP and 1.1 t SRP will be released from sediment at this hydrodynamic condition resulting in the concentration increases of 0.050, 0.029, 0.049, 0.009, 0.0004 and 0.0002 mg L-1. Therefore in shallow lakes, surface disturbance can lead to significant increase of nutrient concentrations although some components in water column had negative flux with weak disturbance (e.g. TDN and SRP in this experiment). In this case, sediment looks to be a source of nutrients. These nutrients deposited in sediment can be carried or released into water with sediment resuspension or changes of environmental conditions at water-sediment interface, which can have great effects on aquatic ecosystem and is also the characteristics of shallow lakes. 相似文献
977.
978.
印度-亚洲大陆碰撞的时限 总被引:43,自引:6,他引:43
印度-亚洲大陆碰撞的起始时间是国际地学界争论的热点,至今尚无一致的认识,从主张晚白垩世(约70Ma)到主张始新世/渐新世之交(约34Ma)等各种观点都有。根据主碰撞带中具同碰撞性质的林子宗火山岩(40.84~64.47Ma)、南冈底斯花岗岩(47~52.5Ma,峰值50Ma左右)、白云母型强过铝花岗岩(56~50Ma),以及沉积学和地层学的综合证据,特别是横贯整个冈底斯带延伸达1500km的巨大区域性角度不整合的时间(约65Ma),认为印度-亚洲大陆开始碰撞的时间在西藏为65Ma左右,完成碰撞的时间在40/45Ma左右。 相似文献
979.
980.
DONG Guochen MO Xuanxue ZHAO Zhidan GUO Tieying WANG Liangliang CHEN Tao State Key Laboratory of Geological Processes Mineral Resources China University of Geosciences Beijing School of Earth Science Resources China University of Geosciences Beijing E-mail: moxx@cugb.edu.cn Hebei Bureau of Geology Mineral Exploration Development Shijiazhuang Hebei 《《地质学报》英文版》2005,79(6)
1 Introduction Mo et al. (2005) determined that magma mixing and mingling took place extensively in the Gangdisê magmatic belt around 50 Ma, and argued that magma mixing was genetically related to underplating of mantle-derived magmas beneath that belt. Underplating, as one of the major mechanisms for crustal growth, can occur in the environments of convergent plate boundaries, subduction and collision zones, and in intra-plate settings such as continental flood basalt provinces (Wilson, 19… 相似文献