全文获取类型
收费全文 | 146篇 |
免费 | 27篇 |
国内免费 | 35篇 |
专业分类
测绘学 | 17篇 |
大气科学 | 10篇 |
地球物理 | 30篇 |
地质学 | 85篇 |
海洋学 | 22篇 |
天文学 | 13篇 |
综合类 | 14篇 |
自然地理 | 17篇 |
出版年
2022年 | 3篇 |
2021年 | 5篇 |
2020年 | 4篇 |
2019年 | 9篇 |
2018年 | 3篇 |
2017年 | 6篇 |
2016年 | 5篇 |
2015年 | 7篇 |
2014年 | 3篇 |
2013年 | 3篇 |
2012年 | 8篇 |
2011年 | 8篇 |
2010年 | 9篇 |
2009年 | 5篇 |
2008年 | 12篇 |
2007年 | 14篇 |
2006年 | 12篇 |
2005年 | 10篇 |
2004年 | 12篇 |
2003年 | 4篇 |
2002年 | 6篇 |
2001年 | 4篇 |
2000年 | 13篇 |
1999年 | 7篇 |
1998年 | 4篇 |
1997年 | 5篇 |
1996年 | 5篇 |
1995年 | 5篇 |
1994年 | 5篇 |
1993年 | 3篇 |
1991年 | 4篇 |
1990年 | 1篇 |
1989年 | 3篇 |
1979年 | 1篇 |
排序方式: 共有208条查询结果,搜索用时 31 毫秒
51.
FOCAL MECHANISM SOLUTION AND TECTONIC STRESS FIELD CHARACTERISTICS OF THE MIDDLE TIANSHAN MOUNTAINS,XINJIANG 下载免费PDF全文
ZHANG Zhi-bin ZHAO Xiao-cheng REN Lin 《地震地质》1979,42(3):595-611
The middle part of the Tianshan Mountains in Xinjiang is located in the north-central part of the Tianshan orogenic belt, between the rigid Tarim Basin and Junggar Basin. It is one of the regions with frequent deformation and strong earthquake activities. In this paper, 492 MS>2.5 earthquake events recorded by Xinjiang seismograph network from 2009 to 2018 were collected. The MS3.5 earthquake was taken as the boundary, the focal mechanism solutions of the earthquake events in this region were calculated by CAP method and FOCEMEC method respectively. At the same time the focal mechanism solutions of GCMT recorded historical earthquake events in this region were also collected. According to the global stress map classification standard, the moderate-strong earthquakes in the region are mainly dominated by thrust with a certain slip component, which are distributed near the combined belts of the Tarim Basin, Junggar Basin, Turpan Basin and Yili Basin with Tianshan Mountains. The thrust component decreases from south to north, while the strike-slip component increases. The spatial distribution characteristics of the tectonic stress field in the middle section of the Tianshan Mountains in Xinjiang are obtained by using the damped regional-scale stress field inversion method. The maximum principal compressive stress in axis the study area rotated in a fan shape from west to east, the NW direction in the western section gradually shifted to NE direction, its elevation angle is nearly horizontal, in the state of near horizontal compression. The minimum principal compressive stress axis is nearly EW, and the elevation angle is nearly vertical. Influenced by large fault zones such as Kashi River, Bolhinur, Nalati, Fukang, the southern margin of the Junggar and the north Beiluntai, the local regional stress field presents complex diversity. Under the influence of the northward extrusion of Pamir and Tarim blocks, the whole Tianshan is shortened by compression, but its shortening rate decreases from south to north and from west to east, the stress shape factor increases gradually from west to east, the intermediate principal compressive stress axis exhibits a change in compression to extension. There are some differences in the characteristics of tectonic stress field between the north and south of Tianshan Mountains. The regional maximum principal compressive stress axis is 15° north by east on the south side, while it is nearly NS on the north side. The deformation of the Tianshan Mountains and the two basins on both sides is obviously larger than that in the inside of the mountain. Changes in the crustal shortening rate caused by the rotation of the rigid Tarim block and Junggar block to the relatively soft Tianshan block, as well as the uplifts of Borokonu and Bogda Mountains, the comprehensive influence of the material westward expansion constitute the stress field distribution characteristics of the north and south sides of the middle section of Tianshan Mountains. The recent two MS6.6 earthquakes in the region caused the regional stress field to rotate counterclockwise. The post-earthquake stress field and the main source focal mechanism solution tend to be consistent. The seismic activity in the study area is week in the south and strong in the north. The focal depth is about 20km. Most strike-slip earthquakes occur near the junction belt of the Tianshan and Junggar Basin. 相似文献
52.
53.
54.
藏北南羌塘陆块北缘晚三叠世弄佰组火山岩的特征及构造环境 总被引:1,自引:0,他引:1
藏北南羌塘陆块北缘发育一套晚三叠世火山岩,命名为弄佰组。该组火山岩以玄武岩为主。岩石化学成分以低TiO_2、FeO Fe_2O_3、K_2O为特征。∑REE介于162.91×10~(-6)383.4×10~(-6)之间,∑Ce/∑Y介于1.83~3.00之间,δEu介于0.47~0.97之间,平均为0.73,负Eu异常较明显。微量元素Sr、K、Rb、Ba、Th、Ce、Sm强烈富集,Ta、Nb、P、Ti、Cr相对亏损。岩石学和岩石地球化学特征表明弄佰组火山岩形成于消减带岛弧区。弄佰组火山岩出露于龙木错-双湖结合带的南侧,K-Ar同位素年龄值为223Ma±5Ma.与双湖带中蓝片岩和绿片岩相变质岩系的形成年龄(220~235Ma)基本一致,时空关系的紧密相连,说明其形成可能与晚三叠世龙木错-双湖古特提斯洋的南向俯冲消减事件有关。 相似文献
55.
56.
57.
ZHU Bingquan Dong Yunpeng CHANG Xiangyang ZHANG ZhengweiGuangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou Guangdong 《《地质学报》英文版》2000,74(2):236-240
Through lead isotope geochemical mapping in the Yunnan-Guizhou area geochemical steep zones (GSZ) have been established, which clearly reveal the junction relationship of the Cathaysian, Yangtze and Indo-China plates. GSZ are closey related to gravity Mono gradient zones and lithospheric thickness. The GSZ between the Yangtze and Cathaysian plates is consistent with the Shizong-Mile tectonic belt, where island arc basalts are well developed. The Yangtze-Indo-China GSZ is parallel to the Jingdong-Mojiang volcanic belt in rift-island arc environments. The evidence of geology, geophysics and geochemistry all indicates that Cathaysia was subducted towards the Yangtze plate and that the Yangtze plate was underthrust beneath the Indo-China, which took place from the Early Carboniferous to the Early Triassic. 相似文献
58.
TECTONIC EVOLUTION OF THE GARZE—LITANG PLATE JUNCTION, WITH PARTICULAR REFERENCE TO THE GOLD DEPOSITS 相似文献
59.
三联点构造地质变量的研究 总被引:1,自引:0,他引:1
地质变量的研究包括地质数据类型、地质变量类型、地质变量的选取原则和方法、地质变量变换的方法.着重对三联点构造的3个基础模型变量的选取及用数学统计方法处理变量提供思路并提出了应用前景. 相似文献
60.
地质调查剖面图的机助设计制图 总被引:1,自引:0,他引:1
地质模型和数学模型的建立是解决问题的关键,从而使“计算机辅助野外地质调查系统”更便利、高效地适用于野外地质工作。实测剖面图是地质调查中,经常用到的技术方法和手段,以利对地质现象更清楚的认识。三联点构造描述方法及剖面图制作,是计算机辅助地质调查中十分重要的研究内容。本文探讨了三联点构造野外描述的内容及顺序、构造级别的划分等。对此选择VisualC++为开发工具,设汁了实测剖面图子系统。分为数据录入模块、图形绘制模块及成果数据管理模块。同时介绍了实测剖面图的数据结构及图层划分,提出了实现数据录人模块和图形模块的方法。 相似文献