全文获取类型
收费全文 | 3909篇 |
免费 | 1145篇 |
国内免费 | 1516篇 |
专业分类
测绘学 | 642篇 |
大气科学 | 550篇 |
地球物理 | 871篇 |
地质学 | 2759篇 |
海洋学 | 794篇 |
天文学 | 31篇 |
综合类 | 368篇 |
自然地理 | 555篇 |
出版年
2024年 | 32篇 |
2023年 | 84篇 |
2022年 | 278篇 |
2021年 | 317篇 |
2020年 | 214篇 |
2019年 | 298篇 |
2018年 | 241篇 |
2017年 | 246篇 |
2016年 | 241篇 |
2015年 | 291篇 |
2014年 | 247篇 |
2013年 | 381篇 |
2012年 | 352篇 |
2011年 | 337篇 |
2010年 | 344篇 |
2009年 | 338篇 |
2008年 | 355篇 |
2007年 | 352篇 |
2006年 | 323篇 |
2005年 | 297篇 |
2004年 | 223篇 |
2003年 | 148篇 |
2002年 | 162篇 |
2001年 | 134篇 |
2000年 | 94篇 |
1999年 | 67篇 |
1998年 | 26篇 |
1997年 | 27篇 |
1996年 | 14篇 |
1995年 | 9篇 |
1994年 | 8篇 |
1993年 | 7篇 |
1992年 | 12篇 |
1991年 | 11篇 |
1990年 | 12篇 |
1989年 | 3篇 |
1988年 | 6篇 |
1987年 | 3篇 |
1986年 | 2篇 |
1985年 | 2篇 |
1982年 | 2篇 |
1979年 | 2篇 |
1973年 | 2篇 |
1957年 | 2篇 |
1954年 | 6篇 |
1949年 | 1篇 |
1944年 | 2篇 |
1937年 | 4篇 |
1934年 | 1篇 |
1933年 | 3篇 |
排序方式: 共有6570条查询结果,搜索用时 31 毫秒
101.
柯坪塔格推覆构造几何学、运动学及其构造演化 总被引:29,自引:1,他引:29
大量野外构造地质调查和深部构造解释表明柯坪塔格推覆构造由多组倒转复式背斜、复式箱状背斜构成的推覆体及其前缘逆冲断裂组成 ,由寒武系—第四系组成的推覆体由北向南逆—斜冲 ,平面上构成向南凸出的弧形推覆构造 ;普昌断裂由各不相连的逆冲斜冲断裂段组成 ,而不是完整的一条走滑断层 ,各推覆体前缘逆冲断裂与各推覆体的普昌断裂段共同构成统一的前缘逆冲斜冲逆冲断裂和推覆构造系统 ;普昌断裂段以西的推覆体具有向东抬升、向西倾覆的鼻状构造特征 ,普昌断裂段以东的推覆体具有向西抬升、向东倾覆的鼻状构造特征 ,普昌基底隆起带是巴楚隆起隐伏在柯坪塔格推覆构造之下的部分。各推覆体前缘断裂在深部均归并于统一的寒武系底部的滑脱面 ,其南浅北深 ,东浅西深 (普昌隆起带以西 )或西浅东深 (普昌隆起带以东 ) (6 10km ) ,埋深较大区发育多组滑脱面。柯坪塔格推覆构造的形成时期为晚第四纪 ,为现今活动的推覆构造系统。文中认为各推覆体向南西的倾覆端基底滑脱面和中新生界内部的滑脱面没有贯通 ,是未来 6级以上地震的发震构造部位。 相似文献
102.
Introduction The rock medium shows mainly elastic character under low-temperature, low-pressure and external force for short duration, yet it shows rheologic property under high-temperature, high-pressure and long-time external force. It is reasonable that the rapid earthquake generating process lasted for tens seconds is analyzed by the elastic theory. As for the earthquake generating process for hundreds or thousand years, nevertheless, the rheologic property of rock must be taken into accou… 相似文献
103.
Min Wang Zhengkang Shen Zhijun Niu Zusheng Zhang Hanrong Sun Weijun Gan Qi Wang Qun Ren 《中国科学D辑(英文版)》2003,46(2):25-40
We obtain the preliminary result of crustal deformation velocity field for the Chinese continent by analyzing GPS data from the Crustal Motion Observation Network of China (CMONOC), particularly the data from the regional networks of CMONOC observed in 1999 and 2001. We delineate 9 technically active blocks and 2 broadly distributed deformation zones out of a dense GPS velocity field, and derive block motion Euler poles for the blocks and their relative motion rates. Our result reveals that there are 3 categories of deformation patterns in the Chinese continent. The first category, associated with the interior of the Tibetan Plateau and the Tianshan orogenic belt, shows broadly distributed deformation within the regions. The third category, associated with the Tarim Basin and the region east of the north-south seismic belt of China, shows block-like motion, with deformation accommodated along the block boundaries only. The second category, mainly associated with the borderland of the Tibetan Plateau, such as the Qaidam, Qilian, Xining (in eastern Qinghai), and the Diamond-shaped (in western Sichuan and Yunnan) blocks, has the deformation pattern between the first and the third, i.e. these regions appear to deform block-like, but with smaller sizes and less strength for the blocks. Based on the analysis of the lithospheric structures and the deformation patterns of the regions above, we come to the inference that the deformation modes of the Chinese continental crust are mainly controlled by the crustal structure. The crust of the eastern China and the Tarim Basin is mechanically strong, and its deformation takes the form of relative motion between rigid blocks. On the other hand, the northward indentation of the Indian plate into the Asia continent has created the uplift of the Tibetan Plateau and the Tianshan Mountains, thickened their crust, and raised the temperature in the crust. The lower crust thus has become ductile, evidenced in low seismic velocity and high electric conductivity observed. The brittle part of the crust, driven by the visco-plastic flow of the lower crust, deforms extensively at all scales. The regions of the second category located at the borderland of the Tibetan Plateau are at the transition zone between the regions of the first and the third categories in terms of the crustal structure. Driven by the lateral boundary forces, their deformation style is also between the two, in the form of block motion and deformation with smaller blocks and less internal strength. 相似文献
104.
105.
106.
ZhangBingshan TangLiangjie JinZhijun DaiJunsheng ZhangMingli ZhangBingshan 《中国地质大学学报(英文版)》2003,14(1):65-72
The purpose of this paper is to analyze the regional fault systems of Qaidam basin and ad-jacent orogenic belts. Field investigation and seismic interpretation indicate that five regional fault sys-tans occurred in the Qaidam and adjacent nment.qin belts, controlling the development and evolution of the Qaidam basin. These fault systems are: (1)north Qaidam-Qilian Mountain fault system; (2) south Qaidam-East Kunhm Mountain fault system;(3)Altun strike-slip fault system; (4) Elashan strike-slip fault system, and (5) Gansen-Xiaochaidan fault system. It is indicated that the fault systems controlled the orientation of the Qaidam basin, the formation and distribution of secondary faults within the basin,the migration of depocenters and the distribution of hydrocarbon accmnulation belt. 相似文献
107.
ChenJianguo ChenZhijun WangQuanming FangYiping 《中国地质大学学报(英文版)》2003,14(3):250-256
The spatial database management system of China geological survey extent is a social service system. Its aim is to help the government and the whole social public to expediently use the spatial database, such as querying, indexing, mapping and product outputting. The management system has been developed based on MAPGIS6. x SDK and Visual C , considering the spatial database contents and structure and the requirements of users. This paper introduces the software structure, the data flow chart and some key techniques of software development. 相似文献
108.
109.
正电子断层扫描仪与PET图像重建概述 总被引:2,自引:0,他引:2
概述了PET(Positron emission tomography,正电子断层扫描仪)及其图像重建的基本原理、方法与临床使用,介绍了常用的图像重建FBP(滤波反投影,Filtered Back-Projection)算法和OSEM(有序子集最大似然法,Ordered Subset Expectation Maximization)算法,描述了如何通过PET的临床协议中的参数选择以得到满意的重建效果。此外,对PET的准三维重建也做了一些简介。 相似文献
110.