全文获取类型
收费全文 | 1554篇 |
免费 | 391篇 |
国内免费 | 617篇 |
专业分类
测绘学 | 238篇 |
大气科学 | 212篇 |
地球物理 | 226篇 |
地质学 | 1175篇 |
海洋学 | 297篇 |
天文学 | 16篇 |
综合类 | 146篇 |
自然地理 | 252篇 |
出版年
2024年 | 14篇 |
2023年 | 52篇 |
2022年 | 174篇 |
2021年 | 144篇 |
2020年 | 109篇 |
2019年 | 147篇 |
2018年 | 114篇 |
2017年 | 110篇 |
2016年 | 100篇 |
2015年 | 96篇 |
2014年 | 90篇 |
2013年 | 113篇 |
2012年 | 131篇 |
2011年 | 129篇 |
2010年 | 161篇 |
2009年 | 123篇 |
2008年 | 153篇 |
2007年 | 114篇 |
2006年 | 118篇 |
2005年 | 79篇 |
2004年 | 70篇 |
2003年 | 38篇 |
2002年 | 42篇 |
2001年 | 40篇 |
2000年 | 28篇 |
1999年 | 15篇 |
1998年 | 6篇 |
1997年 | 10篇 |
1996年 | 7篇 |
1995年 | 2篇 |
1994年 | 2篇 |
1993年 | 5篇 |
1992年 | 3篇 |
1991年 | 3篇 |
1990年 | 5篇 |
1989年 | 5篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1985年 | 1篇 |
1984年 | 1篇 |
1983年 | 1篇 |
1979年 | 1篇 |
1976年 | 1篇 |
1954年 | 3篇 |
排序方式: 共有2562条查询结果,搜索用时 218 毫秒
91.
副高边缘暴雨的多普勒雷达回波特征 总被引:7,自引:4,他引:7
利用常规观测资料和多普勒雷达探测资料,对2003-2004年湖南省4次副高边缘暴雨的天气形势和雷达回波特征进行了分析研究。结果表明:4次暴雨过程的副高位置适当,高空有低槽,中低层有低空急流和低涡切变线,地面上有冷锋。在基本反射率图上,低槽暴雨有S-N向的窄带回波特征、冷式切变线暴雨有准W—E向的积层回波特征、暖式切变线有NE—SW向的积层回波特征,但每一次暴雨过程不尽相同。在多普勒速度图上常出现低空急流、冷暖平流、冷锋、逆风区以及高层大风核等特征,并常是几种特征同时出现,有利于强降水产生。 相似文献
92.
南海珠江深水扇系统的微观内幕结构研究 总被引:1,自引:0,他引:1
本文首次探索在以二维地震资料为主的条件下开展深水扇系统的微观内幕研究。结果表明:在珠江口盆地白云凹陷中的南海珠江深水扇系统中能较好地由浅至深识别出多套地层(尤其是浅部地层)中存在的多种类型的深切谷、峡谷、水道,各有不同地质成因机制。能识别的典型扇体微观结构类型包括丘形体、席状体、水道化沉积及朵叶体等,往往分别指示某些特殊的沉积环境,并且最可能构成潜在的深水油气圈闭的良好储层。在二维地震资料条件下容易识别的深水扇系统微观内幕结构类型比较有限,在空间上追踪典型微观内幕结构也相对比较困难,但是若能全面认识区域构造及沉积背景,综合利用相关资料减少对地震反射结构解释的多解性,就有望对扇体的微观内幕结构进行深入剖析,深化对扇体的地质认识,从而指导油气勘探。 相似文献
93.
94.
地质图空间数据库的建立对于基础地质图件的快速更新、信息资源共享以及基础地质科学研究具有重要意义。全国1∶100万地质图空间数据库(2005年版本)是以1∶50万地质图数据库为基础,充分吸收近年来1∶25万、1∶5万区域地质调查的新资料新成果,应用当代最先进的地质科学理论、现代信息技术和先进制图学理论,使用中国自主开发的MapGIS平台,结合ArcGIS、Access等软件进行研究建立的。数据库包括地理底图库、地质图库、元数据库、外挂岩石地层库,数据量约1.6GB。数据库管理系统具有较强的图幅检索、查询、自动成图、自动生成图例等功能。 相似文献
95.
由中国石油学会石油地质专业委员会、中国地质学会石油地质专业委员会、北京石油学会、国家自然科学基金委地学部、国土资源部油气资源战略研究中心和中国石油大学共同主办的“第四届油气成藏机理与油气资源评价国际学术研讨会”,于2006年10月14日-16日在中国北京顺利召开。共有260余位代表参加了这次大会,他们分别来自俄罗斯、加拿大、澳大利亚、英国、挪威、德国、韩国以及国内的18个科研院所和34个油田公司。这次大会提交的会议论文和摘要116篇,其中大会主题报告28篇,分会交流34篇。[第一段] 相似文献
96.
2005年9~10月渭河流域中、下游发生持续性降雨过程,致使渭河下游形成了自1981年以来最大的洪水。本文分析了降雨洪水成因、特点和对下游河道的影响,并提出了几点认识和建议。 相似文献
97.
The development and utilization of water and land resources in the Shiyang River basin are the highest among the inland rivers
in northwestern China. Using GIS and the landscape structure analysis program FRAGSTATS, landscape metrics of a study area
in the lake-district in Minqin Oasis in the lower reaches of Shiyang River basin were calculated and analyzed based on TM
images from 1987 to 2001 at class level and landscape level, respectively. Transformation matrix of the landscape mosaics
was also examined. The driving forces of landscape changes were analyzed, including the dynamics of runoff and groundwater
resources and their exploitation, and influences of policies and market economy. The results showed that: (1) Patch number
of farmland and desert decreased, but their mean patch area increased, indicating that reclamation and desertification was
very serious in the study area. Contagion index for oasis increased and edge density and landscape diversity were reduced.
(2) Farmland and desert areas have enlarged by 1,520.46 and 4,941.27 hm2, respectively. This increase was at the cost of woodland and grassland, which shrank by 1,520.46 and 4,941.27 hm2, respectively. (3) The net utilization of surface water decreased by 50% in the last 10 years, and dropped to 22.3 × 106 m3 in the later 1990s. Exploitation of groundwater increased remarkably, up to 80 × 106 m3 per year in the last 5 years. (4) The capability of the economic structure to withstand pressures of the market economy has
depressed distinctly because of the simplified planting pattern, which is dominated by salinity-enduring cash crops, such
as cotton. Based on the above analysis, strategies of ecological reconstruction in the lake-district were suggested. 相似文献
98.
99.
100.
HAN Kunying ZHANG Heng DING Xiaozhong REN Liudong SHI Chenglong PANG Jianfeng 《《地质学报》英文版》2020,94(4):1093-1116
On the southwestern margin of the Yangtze Block, the Dongchuan Group consists of slightly metamorphosed sedimentary rocks, including silty slate, argillaceous slate, clayey slate, arkose, dolomite, and minor volcanic rocks. To date, it is still a controversy over the depositional age and stratigraphic sequence of the Dongchuan Group. In this study, we analyzed five samples of meta-sedimentary rocks and one sample of meta-tuff from the Yinmin, Luoxue and Etouchang Formations of the Dongchuan Group in the Yuxi region for detrital zircon U-Pb ages and Lu-Hf isotope. The detrital zircon ages of the meta-sediments vary from 3073 to 1703 Ma, mainly clustered at three periods, from 1889 to 1840, 2490 to 2008 and 2878 to 2844 Ma. The youngest age peak of all the samples is ~1859 Ma, with the εHf(t) values of the zircons ranging from-20.3 to +4.3 and more than 90% being negative, indicating that the Paleoproterozoic crustal accretion on the southwestern margin of the Yangtze Block was dominated by reworking of the ancient crustal materials involved in the assembly and breakup of the Columbia supercontinent. Another important age range is between 2490 Ma and 2008 Ma, with εHf(t) values from-14.7 to +8.9 and 70% of them are negative, suggesting that the magmatism in the source area was also dominated by reworking and recycling of the ancient crustal materials, with minor juvenile mantle substances added. The detritus was probably derived from the Paleoproterozoic crystalline basement in the southern Yuxi region. The oldest peak age is ~2847 Ma and the εHf(t) values are from-7.7 to +7.0 with 50% of both positive and negative values, demonstrating a possible ~2.85 Ga ancient continental nucleus on the southwestern margin of the Yangtze Block and substantial growth in juvenile crust materials during this period. Besides, the weighted average age of the zircons from the meta-tuff of the Etouchang Formation is 1677 ± 14 Ma. Combining the previous research data and this study, we can constrain the depositional age of the Dongchuan Group in central Yunnan Province to the period from the late Paleoproterozoic to early Mesoproterozoic, slightly earlier than that of the Dongchuan Group in the Dongchuan area near to the southwestern Sichuan Province. The depositional age of the Dongchuan Group is older than that of the Kunyang Group. 相似文献