全文获取类型
收费全文 | 1092篇 |
免费 | 140篇 |
国内免费 | 142篇 |
专业分类
测绘学 | 11篇 |
大气科学 | 5篇 |
地球物理 | 226篇 |
地质学 | 678篇 |
海洋学 | 260篇 |
天文学 | 4篇 |
综合类 | 29篇 |
自然地理 | 161篇 |
出版年
2024年 | 4篇 |
2023年 | 12篇 |
2022年 | 3篇 |
2021年 | 21篇 |
2020年 | 29篇 |
2019年 | 39篇 |
2018年 | 37篇 |
2017年 | 35篇 |
2016年 | 35篇 |
2015年 | 27篇 |
2014年 | 34篇 |
2013年 | 88篇 |
2012年 | 53篇 |
2011年 | 54篇 |
2010年 | 49篇 |
2009年 | 51篇 |
2008年 | 64篇 |
2007年 | 67篇 |
2006年 | 59篇 |
2005年 | 73篇 |
2004年 | 50篇 |
2003年 | 43篇 |
2002年 | 44篇 |
2001年 | 42篇 |
2000年 | 49篇 |
1999年 | 32篇 |
1998年 | 49篇 |
1997年 | 28篇 |
1996年 | 33篇 |
1995年 | 22篇 |
1994年 | 20篇 |
1993年 | 25篇 |
1992年 | 23篇 |
1991年 | 11篇 |
1990年 | 10篇 |
1989年 | 11篇 |
1988年 | 3篇 |
1987年 | 4篇 |
1986年 | 6篇 |
1985年 | 9篇 |
1984年 | 7篇 |
1983年 | 2篇 |
1982年 | 8篇 |
1981年 | 5篇 |
1977年 | 2篇 |
1976年 | 1篇 |
1973年 | 1篇 |
排序方式: 共有1374条查询结果,搜索用时 250 毫秒
101.
Impact of natural reforestation on floodplain sedimentation in the Dragonja basin,SW Slovenia 总被引:4,自引:0,他引:4
S. D. Keesstra 《地球表面变化过程与地形》2007,32(1):49-65
Changes in floodplain sediment dynamics have profound effects on riverine habitats and riparian biodiversity. Depopulation due to socio‐economic changes in the Dragonja catchment (91 km2) in southwestern Slovenia resulted in the abandonment of agricultural fields, followed by natural reforestation since 1945. This profoundly changed the water and sediment supply to the streams, as well as floodplain sediment deposition. This paper presents a reconstruction of the development of the Dragonja floodplain due to these land use changes during the last 60 years. The reconstruction is based on dating of floodplain sediments using 137Cs profiles, measurement of actual sedimentation rates using artificial grass sedimentation mats, and linking this information to the present‐day hydrological behaviour of the river. The sedimentation mats showed that floodplain sedimentation was restricted to peak flows of considerable magnitude. Due to the reforestation, the return period of such high flows increased from 0·31 year in the period 1960–1985 to 0·81 year between 1986 and 2003, with commensurate changes in sedimentation rates. At the 1·5 m river terrace (formed about 60 years ago), 137Cs‐based sedimentation rates (1960–1986) were roughly twice the rates inferred from the artificial grass mats (2001–2003). This finding matches the increase in the return period for larger peak events during the 1986–2003 period, which caused fewer major inundations at this level. Conversely, sedimentation rates determined for the lowest terrace at 0·5 m were similar for both techniques (and periods) because the return periods of the peak events responsible for sediment deposition at this lower level did not change much over the period 1986–2003. Copyright © 2006 John Wiley & Sons, Ltd. 相似文献
102.
L. Audin I. Manighetti P. Tapponnier F. Métivier E. Jacques P. Huchon 《Geophysical Journal International》2001,144(2):391-413
A detailed geophysical survey of the Ghoubbet Al Kharab (Djibouti) clarifies the small-scale morphology of the last submerged rift segment of the propagating Aden ridge before it enters the Afar depression. The bathymetry reveals a system of antithetic normal faults striking N130°E, roughly aligned with those active along the Asal rift. The 3.5 kHz sub-bottom profiler shows how the faults cut distinct layers within the recent, up to 60 m thick, sediment cover on the floor of the basin. A large volcanic structure, in the centre of the basin, the 'Ghoubbet' volcano, separates two sedimentary flats. The organization of volcanism and the planform of faulting, with en echelon subrifts along the entire Asal–Ghoubbet rift, appear to confirm the westward propagation of this segment of the plate boundary. Faults throughout the rift have been active continuously for the last 8400 yr, but certain sediment layers show different offsets. The varying offsets of these layers, dated from cores previously retrieved in the southern basin, imply Holocene vertical slip rates of 0.3–1.4 mm yr−1 and indicate a major decrease in sedimentation rate after about 6000 yr BP, and a redistribution of sediments in the deepest troughs during the period that preceded that change. 相似文献
103.
The mechanical denudation rates of 81 large lake basins (lake area > 500 km2) were determined from long-term river loads and erosion maps. Using the drainage area/lake area ratios the mean sedimentation rates of the lakes were calculated for a porosity of 0.3. The mean sedimentation rates of different lake types vary between 0.1 mm/a (glacial lakes, lowland) and 5.4 mm/a (mostly sag basin lakes). The calculated lifetimes of the lakes are based on the lake volumes and mean sedimentation rates, assuming steady-state conditions and solely clastic material. On average, glacial lakes in highlands and fault-related lakes show the shortest lifetimes (c. 70 ka), glacial lakes in lowlands and rift lakes have the longest lifetimes (c. 1 Ma). Some lakes remain unfilled for very long time spans due to rapid subsidence of their basin floors. The calculated lifetimes are compared with those derived from sediment core studies. Most core studies indicate lower mechanical sedimentation rates than the calculated ones because a major part of the incoming sediment is trapped in deltas. However, a number of lakes (e.g., the Great Lakes of North America) show the opposite tendency which is largely caused by extensive shoreline erosion and resuspension. The lifetimes of large glacial lakes often exceed the duration of interglacials. Hence, their lifetimes are restricted by glaciation and not by sediment infill. Rift lakes persist for long time periods which exceed the calculated lifetimes in some cases. Time-dependent subsidence, basin extension, as well as the impact of climate change are briefly described. 相似文献
104.
Cherts from the Yangla copper deposit, western Yunnan Province: geochemical characteristics and relationship with massive sulfide mineralization 总被引:4,自引:0,他引:4
Four layers of cherts were found for the first time in the Yangla copper deposit, western Yunnan Province. The cherts possessed
the following geochemical characteristics: 1 Low TiO2 and Al2O3 contents, but high ore-forming element (e.g. Cu, Au, Ag) contents; 2 low total REE contents and clear negative Eu anomalies
when normalized to chondrite similar to the REE contents and distribution patterns of associated massive sulfide ores; 3 silicon
isotopic compositions of cherts in the Yangla deposit being the same as cherts and geyserite of hot-water sedimentary origin;
4 lead and sulfur isotopic compositions of cherts in the Yangla deposit being similar to those of the massive sulfide ores
in the Yangla deposit; 5 Rb-Sr isochron age of cherts from the Yangla deposit being identical with that of host strata. Hence,
we conclude that the cherts in the Yangla deposit are of hot-water sedimentary origin, which have a close relationship with
the massive sulfide ores. The discovery of hydrothermal cherts from the Yangla copper deposit provides further evidence for
the hydrothermal exhalative origin of the massive sulfide deposits. 相似文献
105.
面对连云港市新浦区软土地基上施工的某住宅楼 ,施工时由于对北楼部分桩出现的缩颈及断裂未能妥善处理 ,造成楼房北倾的问题。经协商 ,及时采取了旋喷桩加固法加固北楼基础 :采用沉降法(切桩 )、纠偏 (使各承台均匀、协调、沉降 )、接桩、固封等措施 ,效果良好。 相似文献
106.
粤北大沟谷热水沉积钠长石岩岩石化学及稀土元素 总被引:3,自引:0,他引:3
大沟谷含金钠长石岩带上为层状下为脉状产于震旦系乐昌峡群片岩中,主要由钠长石岩及碳酸盐岩组成。钠长石岩多为块状及条带状构造。钠长石岩和片岩化学成分不同,钠长石岩相对富集Al2 O3 、TiO2 、MnO、Na2O、P2O5,而贫Fe2O3 、FeO、MgO、CaO、K2 O。在主要氧化物组成的直角坐标图上,钠长石岩和片岩位于不同的区域及具不同的变化趋势。钠长石岩稀土元素含量较低,在 12.5 6× 10 -6~ 5 5.6 6× 10 -6之间,具较低的La/Yb(1.82~ 6.42 )、La/Sm(0.96~ 2.99)、Gd/Yb(0.99~ 2.71)比值,较大的δEu异常范围 (0.41~ 0.8),弱的δCe异常。钠长石岩地质产状特征及稀土元素特征表明其主要是热水沉积形成的。 相似文献
107.
古岩溶及其成矿作用的研究是鄂东南多金属成矿带沉积学和矿床学工作的较薄弱环节之一。作者依据大量野外观测资料,提出识别该区古岩溶岩系的地层、构造、形态和岩石学等四种标志及其古岩溶岩系的成因分类方案,对古岩溶在时间、空间上发育之强度、多期性及其优先发育部位亦作了分析,并阐述岩浆活动对该区古岩溶发育的影响。最后对古岩溶岩系的生成环境,形成作用和时间进行初步探讨。 相似文献
108.
Susan Marriott 《地球表面变化过程与地形》1992,17(7):687-697
Samples of sediment collected from the Severn floodplain between Worcester and Gloucester following the severe flooding in January and February 1990, were analysed for their grain size distribution. The results show that most sand was deposited within 20 m of the channel bank, but that fine sand may contribute to flood sediment across the width of the floodplain. James' (1985) numerical model of overbank sedimentation attempts to predict the transfer of sediment to the floodplain during flooding. Geometrical and hydraulic data relating to the Severn flood are used as input for a computer program of James' (1985) model. The pattern of sediment concentrations predicted by the model was compared with that obtained from statistical analysis of the flood sediment. The patterns were found to be similar, so James' (1985) model was considered to predict in a relative sense the distribution of flood sediment. 相似文献
109.
湘西北下寒武统黑色页岩伴生元素研究新进展 总被引:16,自引:0,他引:16
湖南大庸慈利的镍钼多金属矿床是湘西北下寒武统黑色页岩中伴生元素镍钼及铂族元素等富集最好地段。该矿床中的硅岩应属典型的喷气岩;特殊的筒状富矿体,以及Ni、Mo、Cu、Zn、Se、As、Ba、Au、Ag、Pt族元素特殊组合;矿石中金属硫化物呈胶状产出,显示快速堆积特征。 相似文献
110.