全文获取类型
收费全文 | 1726篇 |
免费 | 368篇 |
国内免费 | 687篇 |
专业分类
测绘学 | 216篇 |
大气科学 | 223篇 |
地球物理 | 289篇 |
地质学 | 1313篇 |
海洋学 | 319篇 |
天文学 | 30篇 |
综合类 | 155篇 |
自然地理 | 236篇 |
出版年
2024年 | 11篇 |
2023年 | 44篇 |
2022年 | 117篇 |
2021年 | 107篇 |
2020年 | 87篇 |
2019年 | 131篇 |
2018年 | 107篇 |
2017年 | 103篇 |
2016年 | 117篇 |
2015年 | 103篇 |
2014年 | 106篇 |
2013年 | 132篇 |
2012年 | 150篇 |
2011年 | 138篇 |
2010年 | 177篇 |
2009年 | 127篇 |
2008年 | 162篇 |
2007年 | 133篇 |
2006年 | 128篇 |
2005年 | 109篇 |
2004年 | 88篇 |
2003年 | 62篇 |
2002年 | 71篇 |
2001年 | 70篇 |
2000年 | 49篇 |
1999年 | 29篇 |
1998年 | 18篇 |
1997年 | 27篇 |
1996年 | 17篇 |
1995年 | 15篇 |
1994年 | 6篇 |
1993年 | 5篇 |
1992年 | 7篇 |
1991年 | 2篇 |
1990年 | 5篇 |
1989年 | 4篇 |
1988年 | 5篇 |
1987年 | 2篇 |
1986年 | 2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2781条查询结果,搜索用时 31 毫秒
921.
Palaeoflood hydrological study is a frontal subject of global change study. Using sedimentology, geomorphology and OSL dating methods, the typical palaeoflood slackwater deposits were studied in the Qishuihe River valley. The results showed that five flooding episodes with 21 palaeoflood events occurred during 4300–4250 a B.P., 4250–4190 a B.P., 4190–4100 a B.P., 4100–4000 a B.P. and 3100–3010 a B.P., respectively, during the Holocene period. The palaeoflood peak discharges were calculated with hydrological models. With a combination of the gauged flood, historical flood and palaeoflood hydrological data, the archives of flood events were extended to over 10,000 years in the Qishuihe River valley, and the flood frequency–peak discharge relationship curve was established accurately. These research results played important roles in mitigating flood hazard, hydraulic engineering and also the development of water resources in the semiarid Weihe River basin. 相似文献
922.
923.
924.
泾河中游龙山文化晚期特大洪水水文学研究 总被引:21,自引:3,他引:18
通过对泾河流域广泛深人的考察,在泾河中游彬县至永寿基岩峡谷河段发现典型的全新世古洪水平流沉积剖面,进行了古洪水沉积学和水文学研究.对于采集的全新世地层剖面序列样品,进行粒度成分、磁化率、烧失量、CaCO3,含量等分析,从沉积学角度证明了研究剖面所夹洪水沉积物具有平流沉积特征,为典型的洪水平流沉积物.根据地层学对比和剖面自身龙山文化晚期陶片、烧土等文化遗物分析,确定泾河在4200-4000 a BP发生了特大洪水事件,并利用沉积学和水文学原理恢复其水位,计算出古洪水洪峰流量为19490~22040 m3/s.同时,通过恢复现代大洪水、洪峰流量与流域面积关系对这种方法和古洪水洪峰流量计算结果进行了验证.不仅延长泾河洪水水文数据序列到万年尺度,而且为沿泾河的水利水电和交通工程建设及沿岸地区城镇的防洪减灾提供了重要的基础数据,具有重要的科学意义和应用价值. 相似文献
925.
GEOLOGICAL AND GEOMORPHIC EXPRESSIONS OF LATE QUATERNARY STRIKE-SLIP ACTIVITY ON JINTA NANSHAN FAULT IN NORTHERN EDGE OF QING-ZANG BLOCK
下载免费PDF全文
![点击此处可从《地震地质》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Jinta Nanshan Fault is an important fault in northeast front of Qing-Zang Plateau, and it is crucial for determining the eastern end of Altyn Tagh Fault. However, there is still debate on its significant strike-slip movement.
In this paper, we study the Late Quaternary activity of Jinta Nanshan Fault and its geological and geomorphic expressions by interpreting aerial photographs and high-resolution remote sensing images, surveying and mapping of geological and geomorphic appearances, digging and clarifying fault profiles and mapping deformation characteristics of micro-topographies, then we analyze whether strike-slip activity exists on Jinta Nanshan Fault.
We get a more complete fault geometry than previous studies from most recent remote sensing images. Active fault traces of Jinta Nanshan mainly include 2 nearly parallel, striking 100°~90° fault scarps, and can be divided into 3 segments. West segment and middle segment form a left stepover with 2~2.5km width, and another stepover with 1.2km width separates the middle and east segment.
We summarize geomorphic and geologic evidence relating to strike slip activity of Jinta Nanshan Fault. Geomorphic expressions are as follows:First, fault scarps with alternating facing directions; second, sinistral offset of stream channels and micro-topographies; third, pull-apart basins and compressive-ridges at discontinuous part of Jinta Nanshan Fault. Geologic expressions are as follows:First, fault plane characteristics, including extremely high fault plane angle, unstable dip directions and coexistence of normal fault and reverse fault; second, flower structures.
Strike-slip rate was estimated by using geomorphic surface age of Zheng et al.(2013)and left-lateral offset with differential GPS measurements of the same geomorphic surface at field site in Fig. 4e. We calculated a strike-slip rate of (0.19±0.05)mm/a, which is slightly larger than or almost the same with vertical slip rate of (0.11±0.03)mm/a from Zheng et al.(2013).
When we confirm the strike-slip activity of Jinta Nanshan, we discuss its potential dynamic sources:First, eastern extension of Altyn Tagh Fault and second, strain partitioning of northeastward extension of Qilian Shan thrust belt. The first one is explainable when it came to geometric pattern of several E-W striking fault and eastward decreasing strike slip rate, but the former cannot explain why the Heishan Fault, which locates between the the Altyn Tagh Fault and Jinta Nanshan Fault, is a pure high angle reverse fault. The latter seems more explainable, because oblique vectors may indeed partition onto a fault and manifest strike-slip activity. 相似文献
926.
927.
为了更好满足地震计的振动测试需求,对振动台的波形失真度、横向运动比、台面不均匀度及稳定性等主要性能指标进行了测试分析.测试结果表明:该振动台具有较好的低频振动特性.利用低频标准套组对该振动台和中国计量科学研究院标准振动台进行比对分析,测试结果存在较小偏差. 相似文献
928.
929.
SHEN Jun ZHOU Lian FENG QingLai ZHANG MuHui LEI Yong ZHANG Ning YU JianXin GU SongZhu 《中国科学:地球科学(英文版)》2014,57(7):1583-1594
The change of the primary productivity across the Permian-Triassic boundary(PTB)remains controversial.In this study,records from two deep-water sections in South China(Xiakou and Xinmin sections)show the primary productivity decreased gradually from the latest Permian to the earliest Triassic,and five evolutionary stages Increase-Decrease-Recovery-RecessionStagnation)can be observed from Clarkina changxingensis-C.deflecta to Hindeodus parvus-Isarcicella isarcica zones.Primary productivity decreased abruptly from the base of C.meishanensis zone.Besides,for adjusting to the deterioration of the oceanic environment,the primary producers in the oceanic surface had changed to acritarch and cyanobacteria,which were more tolerant of stressful environment.Then the producers were under huge stagnation in the H.parvus-I.isarcica zone.The values of quantitative calculation of the primary productivity from the black rock series in the Dalong Formation were very high,corresponding to that of an upwelling area in modern ocean,which shows that the strata of the Dalong Formation in the study region are potential hydrocarbon source-rocks.This result may come from the fact that South China craton was located at the equatorial upwelling area during the Permian-Triassic transitions.But organic matter contents were different in various sections because they could be affected by redox conditions and diagenesis process after burial. 相似文献
930.