全文获取类型
收费全文 | 2958篇 |
免费 | 441篇 |
国内免费 | 520篇 |
专业分类
测绘学 | 275篇 |
大气科学 | 341篇 |
地球物理 | 579篇 |
地质学 | 1343篇 |
海洋学 | 399篇 |
天文学 | 55篇 |
综合类 | 206篇 |
自然地理 | 721篇 |
出版年
2024年 | 10篇 |
2023年 | 33篇 |
2022年 | 94篇 |
2021年 | 117篇 |
2020年 | 124篇 |
2019年 | 175篇 |
2018年 | 118篇 |
2017年 | 137篇 |
2016年 | 144篇 |
2015年 | 166篇 |
2014年 | 142篇 |
2013年 | 195篇 |
2012年 | 164篇 |
2011年 | 174篇 |
2010年 | 138篇 |
2009年 | 171篇 |
2008年 | 177篇 |
2007年 | 175篇 |
2006年 | 162篇 |
2005年 | 151篇 |
2004年 | 137篇 |
2003年 | 104篇 |
2002年 | 98篇 |
2001年 | 94篇 |
2000年 | 94篇 |
1999年 | 91篇 |
1998年 | 72篇 |
1997年 | 83篇 |
1996年 | 72篇 |
1995年 | 53篇 |
1994年 | 51篇 |
1993年 | 47篇 |
1992年 | 26篇 |
1991年 | 17篇 |
1990年 | 36篇 |
1989年 | 24篇 |
1988年 | 11篇 |
1987年 | 16篇 |
1986年 | 9篇 |
1985年 | 2篇 |
1984年 | 5篇 |
1983年 | 2篇 |
1982年 | 3篇 |
1981年 | 2篇 |
1980年 | 2篇 |
1971年 | 1篇 |
排序方式: 共有3919条查询结果,搜索用时 15 毫秒
11.
We study the morphology of the major rivers draining the Eastern Alps to test whether the active tectonics of this part of the orogen is reflected in the shape of channel profiles of the river network. In our approach we compare channel profiles measured from digital elevation models with numerically modelled channel profiles using a stream power approach. It is shown that regions of high stream power coincide largely with regions of highest topography and largest uplift rates, while the forelands and the Pannonian Basin are characterised by a significantly lower stream power. From stream power modelling we conclude that there is young uplift at the very east of the Eastern Alps, in the Bohemian Massif and in the Pohorje Range. The impact of the Pleistocene glaciations is explored by comparing properties of rivers that drain in proximal and distal positions relative to the ice sheet during the last glacial maximum. Our analysis shows that most knick points, wind gaps and other non-equilibrium features of catchments covered by ice during the last glaciations (Salzach, Enns) can be correlated with glacial processes. In contrast the ice free catchments of the Mur and Drava are characterized by channels in morphological equilibrium at the first approximation and are showing only weak evidence of the strong tectonic activity within these catchments. Finally, the channel profiles of the Adige and the divide between the upper Rhine and Danube catchments differ significantly from the other catchments. We relate this to the fact that the Adige and the Rhine respond to different base levels from the remainder of the Eastern Alps: The Adige may preserve a record from the Messininan base level change and the Rhine is subject to the base level lowering in the Rhine Graben. 相似文献
12.
In the geological record, hummocky dead-ice moraines represent the final product of the melt-out of dead-ice. Processes and rates of dead-ice melting in ice-cored moraines and at debris-covered glaciers are commonly believed to be governed by climate and debris-cover properties. Here, backwasting rates from 14 dead-ice areas are assessed in relation to mean annual air temperature, mean summer air temperature, mean annual precipitation, mean summer precipitation, and annual sum of positive degree days. The highest correlation was found between backwasting rate and mean annual air temperature. However, the correlation between melt rates and climate parameters is low, stressing that processes and topography play a major role in governing the rates of backwasting. The rates of backwasting from modern glacial environments should serve as input to de-icing models for ancient dead-ice areas in order to assess the mode and duration of deposition.A challenge for future explorations of dead-ice environments is to obtain long-term records of field-based monitoring of melt progression. Furthermore, many modern satellite-borne sensors have high potentials for recordings of multi-temporal Digital Elevation Models (DEMs) for detection and quantification of changes in dead-ice environments. In recent years, high-accuracy DEMs from airborne laser scanning altimetry (LiDAR) are emerging as an additional data source. However, time series of high-resolution aerial photographs remain essential for both visual inspection and high-resolution stereographic DEM production. 相似文献
13.
针对多传感器观测环境下带乘性噪声系统的逆向最优滤波与反褶积融合估计问题 ,本文提出了 1种基于极大似然准则的最优融合算法。该算法中各单传感器间并行计算 ,并且融合中心与单传感器处理中心间无反向通讯 ,因而执行效率较高。仿真表明 ,该融合算法产生的逆向滤波与反褶积比单传感器处理结果有较明显提高 相似文献
14.
南极冰层的冰量为24.5×106km3,占地球总冰量的90%以上,南极冰川进退控制着全球海平面变化和气候波动。酉部南极乔治王岛第四纪冰碛与湖积剖面记录了近12000a来南极曾于距今11000a,9000a和6100a出现过3次快速的冰消过程,近6000a来是一小幅度冷暖交替的气候波动过程。深圳湾北岸潮间带堆积是在近6000a以来发育的,堆积物的环境记录表明,海平面呈周期性升降变化,波动周期平均为670a,低海面时期发生于距今5500—4900a,3900—3600a,2400—2200a和1300—1200a。相邻低海面间则是海面上升时期,每一升降周期的海平面变化幅度为80cm左右,近100a的现代增温,海平面处于上升阶段,上升速率为2—3mm·a(-1)。 相似文献
15.
对南海南部ODP1143站氧同位素11-5e期大约2ka分辨率的粉红色Globigerinoides ruber进行分析,发现其冰期/间冰期旋回与代表全球冰量的底栖有孔虫氧同位素(δ^18O)的变化相反,即在间冰期时含量低,而冰期时高,与其他海区的记录相反。海水表层温度和温跃层深度转换函数结果以及碎壳率的变化显示,在一定的温度背景下,温跃层深度的变化可能是控制粉红色G.ruber冰期旋回的主要因素,而这段时期南海南部溶解作用的影响则不明显。 相似文献
16.
李国胜 《海洋地质与第四纪地质》1996,16(2):93-102
本文根据植物生态学分析方法,通过对艾比湖ZKooB孔中孢粉组合及植被生态的定量分析,阐述了北疆内陆干旱区冰消期以来的气候演化状况。孢粉组合特征及其植被生态的定量分析研究表明,受大气降水以及大气和土壤中相对湿度波动变化的影响,艾比湖地区的生态环境特征在最近15000a中至少经历了10次比较明显的波动变化,并且与全球气候变化过程基本符合,表明中国西部干旱半干旱地区晚更新世以的气候环境演化过程是在全球变 相似文献
17.
太湖表面定振波的数值计算和最大熵谱分析 总被引:1,自引:0,他引:1
利用水动力学方程对太湖表面的定振波进行计算,算得定振波周期约为452min,另外,利用1992年8月29-31日在太湖西山观测到的水位资料,采用最大熵谱法,分析太湖表面的定振波,得周期值约为450min。计算和分析的周期值基本吻合,取熵谱分析结果得太湖表面的单节点定振波周期值为450min。 相似文献
18.
A large number of 3D deep seismic surveys in the Faroe-Shetland Channel gives continuous coverage over most of the region. These surveys were designed primarily to image depths in excess of 4 km, use low frequency sources and are recorded at low temporal sample rates. However, commercial 3D data can generate highly detailed images of the seabed due to the high spatial sample rate, typically 12.5 m. This is particularly true in waters below 200 m. Despite geophysical artefacts, the images reveal that there are a number of sedimentary processes at work adjacent to and within this channel. On the West Shetland Shelf, iceberg scouring and moraines reflect the impact of glaciation. On the West Shetland slope there is clear evidence for down-slope processes, such as debris flows, linear erosion channels, basal fans and (one case) slope failure. Along-slope processes are also active as indicated by the presence of sediment waves and contourite mounds. On the floor of the basin, polygonal cracking can be observed. The most spectacular feature appears to be the Judd Deeps, a system of cliffs approximately 200 m high and 40 km across. Traditionally, seabed investigation has been performed using high-resolution surveys. This study shows that deep exploration data can also provide useful images of the seafloor. 相似文献
19.
以往认为宁波组沉积时期的古气候为寒冷干燥或冷凉干燥。本文依据北仑B_(12)孔的孢粉资料,阐明在这一冷期中曾有一次相对较暖的气候波动,据此又可分冷凉—温和—温凉三个阶段,湿度以略湿为主。此外,还讨论了本区在晚大理冰期温度、湿度的变化特点。 相似文献
20.