全文获取类型
收费全文 | 1630篇 |
免费 | 42篇 |
国内免费 | 21篇 |
专业分类
测绘学 | 52篇 |
大气科学 | 94篇 |
地球物理 | 345篇 |
地质学 | 581篇 |
海洋学 | 109篇 |
天文学 | 343篇 |
综合类 | 16篇 |
自然地理 | 153篇 |
出版年
2022年 | 8篇 |
2021年 | 8篇 |
2020年 | 23篇 |
2019年 | 22篇 |
2018年 | 31篇 |
2017年 | 23篇 |
2016年 | 31篇 |
2015年 | 25篇 |
2014年 | 37篇 |
2013年 | 72篇 |
2012年 | 49篇 |
2011年 | 68篇 |
2010年 | 87篇 |
2009年 | 91篇 |
2008年 | 78篇 |
2007年 | 63篇 |
2006年 | 58篇 |
2005年 | 57篇 |
2004年 | 50篇 |
2003年 | 63篇 |
2002年 | 52篇 |
2001年 | 27篇 |
2000年 | 39篇 |
1999年 | 25篇 |
1998年 | 20篇 |
1997年 | 22篇 |
1996年 | 21篇 |
1995年 | 23篇 |
1994年 | 27篇 |
1993年 | 25篇 |
1992年 | 23篇 |
1990年 | 21篇 |
1989年 | 23篇 |
1988年 | 26篇 |
1987年 | 21篇 |
1986年 | 20篇 |
1985年 | 34篇 |
1984年 | 32篇 |
1983年 | 27篇 |
1982年 | 22篇 |
1981年 | 36篇 |
1980年 | 24篇 |
1979年 | 16篇 |
1978年 | 15篇 |
1977年 | 20篇 |
1976年 | 14篇 |
1975年 | 11篇 |
1974年 | 19篇 |
1973年 | 16篇 |
1971年 | 8篇 |
排序方式: 共有1693条查询结果,搜索用时 31 毫秒
121.
122.
123.
The problem of current channelling: A critical review 总被引:1,自引:0,他引:1
Alan G. Jones 《Surveys in Geophysics》1983,6(1-2):79-122
The notion that currents induced ‘elsewhere’, by external source fields, could wend their way in a frequency-independent ohmic-like manner through a region of interest has been the cause of many recent disputes within the geomagnetic induction community. In particular, two-dimensional (2D) models of the Rhinegraben, and of the region known as the ‘Eskdalemuir anomaly’ in southern Scotland, have been dismissed as erroneous by those who believe that the observations are more correctly interpreted as due to the effects of ‘channelled’ currents rather than ‘induced’ currents. In this review, attention is paid primarily to consider under what circumstances any perturbation of current flow, which may manifest itself as a ‘DC-like’ channelled current, could cause a ‘problem’ for those wishing to interpret their observations. Various concepts are introduced, particularly the ratio of 3D/2D current channelling numbers for the induction problem, which is shown to be the ratio of the length of the 3D body to the skin depth in the host medium. It is stressed that the worker must analyse his data by adequate statistical techniques, and that the simplest physical models possible, that describes the observations, must be sought. Finally, suggestions are made for further work to be undertaken. 相似文献
124.
The Abee E4 enstatite chondrite breccia consists of clasts (many rimmed by metallic Fe, Ni), dark inclusions and matrix. The clasts and matrix were well equilibrated by thermal metamorphism, as evidenced by uniform mineral compositions, recrystallized chondrules, low MnO content of enstatite and high abundance of orthoenstatite. The clasts acquired their metal-rich rims prior to this metamorphic episode. The occurrence in Abee of relatively unmetamorphosed dark inclusions, clasts with nearly random magnetic orientations and a matrix with a uniform magnetic orientation [18,19] indicates that clast and matrix metamorphism occurred prior to the agglomeration of the breccia.The dark inclusions are an unusual kind of enstatite chondritic material, distinguished from the clasts and matrix by their relative enrichments in REE [21–23], low relative abundances of kamacite, total metallic Fe, Ni and silica, lower niningerite/(total sulfide) ratios, high relative abundances of oldhamite and martensite, smaller euhedral enstatite, more heterogeneous enstatite and metallic Fe, Ni, more calcic enstatite and more nickeliferous schreibersite.We propose the following model for the petrogenesis of the Abee breccia: The maximum metamorphic temperature of breccia parent material was?- 840°C (the minimum temperature of formation of Abee niningerite) and perhaps near 950–1000°C (the Fe-Ni-S eutectic temperature). Euhedral enstatite crystals in metallic Fe, Ni- and sulfide-rich areas grew at these metamorphic temperatures into pliable metal and sulfide. Breccia parent material was impact-excavated from depth, admixed with dark inclusions and rapidly cooled (700 to 200°C in about 2 hours) [15]. During this cooling, clast and matrix material acquired thermal remanent magnetization. Random conglomeration of clasts and unconsolidated matrix materials caused the clasts to have random magnetic orientations and the matrix areas to have net magnetic intensities of zero (due to the cancellation of numerous randomly oriented magnetic vectors of equal intensity in the matrix). A subsequent ambient magnetic field imparted a uniform net magnetic orientation to the matrix and caused the magnetic orientations of the clasts to be somewhat less random. The Abee breccia was later consolidated, possibly by shock or by shallow burial and very long-period/low-temperature (< 215°C) metamorphism. 相似文献
125.
Alan P. Carr 《地球表面变化过程与地形》1983,8(3):293-296
The method described involves the use of an electro-optical distance measurer mounted on a theodolite. Observations are taken onto a series of acrylic reflectors, aligned at right angles to the line of sight, and slope distances and vertical and horizontal angles are recorded. From these data it is possible to obtain surface heights to an accuracy of ±0·5 cm at 200 m and to avoid any direct disturbance of the site under investigation. 相似文献
126.
Alan C. McKinnon 《Geoforum》1983,14(4):389-399
Over the past decade there has been a growing recognition by the business community, central government and local planners of the economic importance of warehousing. This importance can be measured in terms of the value of stock held in warehouses, their very rapid growth relative to other types of commercial property and the employment they create. This article reviews changes in business and planning attitudes to warehousing, accounts for the recent growth of warehouse floorspace in England and examines the spatial distribution of this growth. 相似文献
127.
Alan D. Ziegler Edwin P. Maurer Justin Sheffield Bart Nijssen Eric F. Wood Dennis P. Lettenmaier 《Climatic change》2005,72(1-2):17-36
We use diagnostic studies of off-line variable infiltration capacity (VIC) model simulations of terrestrial water budgets
and 21st-century climate change simulations using the parallel climate model (PCM) to estimate the time required to detect
predicted changes in annual precipitation (P), evapotranspiration (E), and discharge (Q) in three sub-basins of the Mississippi River Basin. Time series lengths on the order of 50–350 years are required to detect
plausible P, E, and Q trends in the Missouri, Ohio, and Upper Mississippi River basins. Approximately 80–160, 50, and 140–350 years, respectively,
are needed to detect the predicted P, E, and Q trends with a high degree of statistical confidence. These detection time estimates are based on conservative statistical
criteria (α = 0.05 and β = 0.10) associated with low probability of both detecting a trend when it is not occurring (Type
I error) and not detecting a trend when it is occurring (Type II error). The long detection times suggest that global-warming-induced
changes in annual basin-wide hydro-climatic variables that may already be occurring in the three basins probably cannot yet
be detected at this level of confidence. Furthermore, changes for some variables that may occur within the 21st century might
not be detectable for many decades or until the following century – this may or may not be the case for individual recording
station data. The long detection times for streamflow result from comparatively low signal-to-noise ratios in the annual time
series. Finally, initial estimates suggest that faster detection of acceleration in the hydrological cycle may be possible
using seasonal time series of appropriate hydro-climatic variables, rather than annual time series. 相似文献
128.
129.
The impact of geographical indication on the revitalisation of a regional economy: a case study of 'Boseong' green tea 总被引:1,自引:0,他引:1
Geographical indications are legal signs which identify a good as originating in a specific country or region, where the reputation of the product is attributable to its geographical roots. South Korea has operated with a geographical indication system since 1999. This research analyses the regional impacts of geographical indications using the case study of 'Boseong' green tea. The results show that geographical indication has enhanced the image of the product, leading to increased production and the stimulation of tea-related industries. We argue that geographical indication can be used as an effective policy to cope with trade liberalisation. 相似文献
130.
On 19 September 2003, 40 landslides of 140–18 000 m3 volume occurred within 2·5 km2 on the slopes of Dooncarton Mountain (Republic of Ireland) during a storm that may have exceeded 90 mm within 90 minutes. The landslides were investigated to determine the reasons for such a high density of slope failures. All of the landslides were surveyed within four months, and nine of them were investigated in detail. The six largest landslides, all peat failures, accounted for 57% of the more than 100 000 m3 of material displaced during the event. A consistent sequence of superficial materials was found on the failed hillslopes, including an extensive iron pan at the base of a buried soil horizon 0·3 m below the base of the peat. Morphologically, almost all of the landslides occurred on steep planar slopes or around sharp convexities, with the latter failures developing retrogressively upslope. The only significant relationship found from analysis of 371 subsurface pipes and 142 seepage cracks (defined here as contiguous fissures conducting concentrated subsurface flow) across all the failures was that the thinner the peat cover, the deeper the pipes and seepage cracks occurred below the base of peat. It is concluded that most of the landslides were probably caused by a combination of excess water pressures in the buried soil horizon and the thinner overburden of peat or peaty soil associated with the steeper slope segments. Pipes and seepage cracks formed on the iron pan probably existed prior to the failure event and may have contributed to the high water pressures as rainwater inputs exceeded their discharge capacities. One large peat slide was probably triggered by excess water pressures developed within and between artificial tine cuts. The properties of the blanket peat were generally of little consequence in the occurrence of the landslides, but relict desiccation cracks and other structural weaknesses through the peat mass were probably highly significant. Although several aspects of the peat failures correspond to previously published examples, the context of these failures in terms of the topography and upland catena is distinctive. Copyright © 2007 John Wiley & Sons, Ltd. 相似文献