全文获取类型
收费全文 | 103篇 |
免费 | 10篇 |
国内免费 | 56篇 |
专业分类
测绘学 | 3篇 |
大气科学 | 3篇 |
地球物理 | 17篇 |
地质学 | 82篇 |
海洋学 | 48篇 |
天文学 | 4篇 |
综合类 | 9篇 |
自然地理 | 3篇 |
出版年
2022年 | 1篇 |
2020年 | 1篇 |
2019年 | 2篇 |
2016年 | 1篇 |
2015年 | 4篇 |
2013年 | 1篇 |
2011年 | 8篇 |
2010年 | 2篇 |
2009年 | 6篇 |
2008年 | 3篇 |
2007年 | 1篇 |
2006年 | 6篇 |
2005年 | 3篇 |
2004年 | 13篇 |
2003年 | 9篇 |
2002年 | 17篇 |
2001年 | 9篇 |
2000年 | 7篇 |
1999年 | 9篇 |
1998年 | 12篇 |
1997年 | 6篇 |
1996年 | 9篇 |
1995年 | 5篇 |
1994年 | 2篇 |
1993年 | 8篇 |
1992年 | 7篇 |
1991年 | 8篇 |
1990年 | 2篇 |
1934年 | 2篇 |
1928年 | 1篇 |
1927年 | 1篇 |
1924年 | 3篇 |
排序方式: 共有169条查询结果,搜索用时 0 毫秒
51.
Die palaeozoischen Pflanzen der Provinz Suiyuan sind bisher sehr wenig bekannt. Die in der vorliegenden Arbeit beschriebenen Pflanzen stammen aus dem sogenannten "Tachingshan Range" namentlich aus den Localitaten Tungshengmao und Kumenyintien. Die Fundorte liegen also etwa an der Grenze 相似文献
52.
The fragment of fossil wood forming the main subject of this paper was collected by P. Teilhard de Chardin when he was sent to Sinkiang by the Geological Survey of China, with the Haardt-Citroen Expedition (1932). 相似文献
53.
澜沧江断裂带的新生代走滑运动学特点 总被引:9,自引:1,他引:9
通过对澜沧江断裂带北、中、南段新生代构造形迹的运动学解析,结合前人工作,论证了澜沧江断裂在新生代早期(古新世-中始新世末)、中期(晚始新世-渐新世末)、晚期(中新世-第四纪)的走滑运动序列为:中、南段,右行→左行→右行;北段,左行→左行→右行。研究表明,澜沧江断裂带早期主要表现为中、南段的右行逆冲和北段的左行逆冲,与同期发生的昌都-思茅地体颈缩事件相对应,其地球动力学背景与太平洋板块向西推挤作用以及扬子-华南板块与印度板块发生的强烈东西向碰撞挤压有关;中期,整个断裂发生左行逆冲,其地球动力学背景与南海盆地的扩张作用及其扬子-华南板块相对于印度板块北移所致的左行扭动相适应:晚期,整个断裂右行走滑,与太平洋构造域的南海盆地扩张终止,昌都思茅地体整体向南东逃逸相适应。 相似文献
54.
It may be safely presumed that few of us who have worked in the field as a geological surveyor would dissent in making an open confession of our unfortunate attitude towards igneous rocks particularly those of a massive form. These obstacles, as one is apt to regard them, are the unruly bodies 相似文献
55.
The Shengli I Point Bar on the Yellow River Delta: Three-Dimensional Structures and Their Evolution 总被引:3,自引:0,他引:3
ZHONG Jianhu SHEN Xiaohu NI Jinren WANG Guanmin WEN Zhifeng WANG Xibin WANG Haiqiao LI Li WU Kongyou LI Yong HONG MeiEarth Resource Information College Petroleum University of Chin Dongyin Shandong Earth Science Department Zhejiang University Hangzhou Zhejiang Center for Environment Science Peking University Beijing 《《地质学报》英文版》2002,76(4):463-477
Point bars are well developed on the Yellow River delta, among which the Shengli I point bar is the most typical. The point bar, being about 4 km in length and several tens to more than 100 meters in width, is located on the south side of the Shengli Bridge in Kenli County, Dongying, Shandong. It is a typical fine-grained point bar with silt, which is predominant, some clay and minor plant debris and clay boulders. The Shengli I point bar has complicated 3-D structures. Firstly, in a plane view, it comprises mainly eight sedimentary units, bar edge, bar ridge, bar platform, bar plain, bar channel, bar gully, bar pond and bar bay, developing side by side and superimposed one by one in a complex way. Secondly, its vertical structures are very complex due to the partial superimposition of the 8 sedimentary units. Besides hydatogenesis, very intensive wind erosion, eolian, ice and meltwater actions are also visible on the Shengli I point bar. The complex form is made even more complicated because of the abo 相似文献
56.
57.
Yao Guoquan Ma Zhixiong Ding Bingcan Prof. Senior Engineer River Harbour Department Nanjing Hydraulic Research Institute Nanjing Senior Engineer River Harbour Department Nanjing Hydraulic Research Institute Nanjing Engineer River Harbour Department Nanjing Hydraulic Research Institute Nanjing 《中国海洋工程》1993,(3)
This paper proposes ten types of improved floating breakwaters for experiment with regular waves, based on the experience in the development and manufacture of existing floating breakwaters both at home and abroad, and on the results of experimental studies on the hydraulic characteristics of several types of floating breakwaters. The wave heights before and behind the breakwaters are measured, the movements of floating breakwaters are observed and the chain forces of the floating breakwaters are measured. The paper studies and compares the hydraulic characteristics of the improved rectangular floating breakwaters of which the internal and external structures and their installation methods are changed. Finally the optimal type of structure is selected through experiments. 相似文献
58.
扬子陆核与陆缘新元古代岩浆事件对比及其构造意义——来自黄陵和汉南侵入杂岩ELA-ICPMS锆石U-Pb同位素年代学的约束 总被引:16,自引:12,他引:16
本文报道分别位于扬子克拉通核部和北缘的黄陵及汉南新元古代侵入杂岩体的惰性气体激光剥蚀-等离子体质谱(ELA-ICPMS)锆石U-Pb年代学研究及其构造意义分析.定年数据显示,黄陵地区的三斗坪、大老岭岩套分别形成于794±7和795±8Ma;晓峰浅成岩岩套形成于744±22Ma,不仅与震旦系莲沱组底部火山岩年龄相同,且同期热事件普遍记录于杂岩体内其它岩套.汉南杂岩体中五堵门岩体形成于789±10Ma,在分析误差范围内与三斗坪、大老岭岩套相同;天平河岩形成于863±10Ma,这是在扬子北缘首次识别出这期岩浆作用.在扬子陆核和北缘侵入杂岩中还分别发现了≈860Ma和945~931Ma的捕获锆石.此外,740Ma的后期热事件同样记录于汉南杂岩体,表明扬子陆块内部和北缘共同经历了790Ma的峰期中酸性岩浆作用和≈740Ma的后期强烈热改造事件,即事件具有克拉通范围的性质.与天平河岩体岩性相似、年龄相同的侵入岩体已在攀西多处地区发现,说明空间上860Ma岩浆作用在扬子北缘和西缘可能具延续性.作者认为,"晋宁期"具造山性质的构造运动开始的时间应以830Ma为限,于≈790Ma达到了以壳内物质重熔为主的大规模岩浆侵入事件的峰期,并在≈740Ma以短期内地壳运动由剧烈抬升向快速沉降的构造转换为造山作用结束的标志.本次研究成果为探讨扬子克拉通新元古代大规模岩浆作用与同期全球构造事件的相互关系提供了重要的同位素年代学约束. 相似文献
59.
60.
Liu Human Zhu Min Pan Keqi Yang Liping Tao Xiaxin Zhang Yuming Dong Ruishu Wang Liangmou and Du RuimingInstitute of Engineering Mechanics SSB Harbin China Institute of Geology SSB Beijing China Computer Application Department Harbin University of Architecture Engineering Harbin China 《中国地震研究》1996,(4)
In this paper,the structure of the intelligence-aided seismic zonation system IASHES and its validation are briefly introduced.Emphasis is placed on the two rank scheme of potential seismic source areas; an expert subsystem for estimating the seismicity trends of rank A source areas; an expert subsystem for delineation of rank B source areas; an expert subsystem for judgment of upper limit of magnitude of rank B source areas,and an improved procedure for determination of weighting factors of rank B source areas,which is specially suitable to ES(Expert systems). 相似文献