全文获取类型
收费全文 | 429篇 |
免费 | 13篇 |
国内免费 | 12篇 |
专业分类
测绘学 | 12篇 |
大气科学 | 46篇 |
地球物理 | 113篇 |
地质学 | 117篇 |
海洋学 | 100篇 |
天文学 | 36篇 |
综合类 | 4篇 |
自然地理 | 26篇 |
出版年
2023年 | 2篇 |
2021年 | 7篇 |
2020年 | 8篇 |
2019年 | 11篇 |
2018年 | 9篇 |
2017年 | 17篇 |
2016年 | 17篇 |
2015年 | 12篇 |
2014年 | 17篇 |
2013年 | 14篇 |
2012年 | 15篇 |
2011年 | 24篇 |
2010年 | 24篇 |
2009年 | 18篇 |
2008年 | 15篇 |
2007年 | 19篇 |
2006年 | 16篇 |
2005年 | 23篇 |
2004年 | 9篇 |
2003年 | 18篇 |
2002年 | 9篇 |
2001年 | 16篇 |
2000年 | 10篇 |
1999年 | 5篇 |
1998年 | 11篇 |
1997年 | 9篇 |
1996年 | 12篇 |
1995年 | 6篇 |
1993年 | 7篇 |
1992年 | 7篇 |
1991年 | 4篇 |
1990年 | 4篇 |
1989年 | 3篇 |
1988年 | 4篇 |
1987年 | 4篇 |
1985年 | 5篇 |
1984年 | 2篇 |
1983年 | 2篇 |
1982年 | 4篇 |
1981年 | 3篇 |
1980年 | 3篇 |
1979年 | 6篇 |
1978年 | 5篇 |
1977年 | 2篇 |
1975年 | 2篇 |
1974年 | 3篇 |
1973年 | 2篇 |
1971年 | 2篇 |
1962年 | 1篇 |
1955年 | 1篇 |
排序方式: 共有454条查询结果,搜索用时 62 毫秒
21.
This work develops the theory of measuring fracture frequency with curved scanlines, as a direct development of work done by others on straight scanlines. Various possible shapes for curved scanlines range between triangular and rectangular, with circular as a reasonable preliminary selection. The discrepancy among different selections decreases with increasing roughness amplitude of the scanline. Analytic solutions for average fracture frequency are given for circular scanlines through single and multiple fracture sets. Results for single fracture sets are plotted. The analytic solution for the general situation of any shape scanline through multiple fracture sets is given. Analytic solutions are given and plotted for circular scanlines through a fracture fabric ellipsoid. A circular scanline spanning 180 degrees yields a global fracture frequency of statistical significance. 相似文献
22.
Overburden deformation associated with halokinesis in the Southern North Sea: implications for the origin of the Silverpit Crater 总被引:1,自引:0,他引:1
Ken Thomson 《Visual Geosciences》2004,9(1):39-47
Gravitational collapse in response to the creation of salt swells and diapirs is a common phenomenon within regions such as the Southern North Sea. Although collapse faulting and slumping of linear salt swell flanks has previously been documented, the existence of concentric collapse structures surrounding diapirs and isolated salt lows is a recently recognised feature. 3-D seismic data from the Southern North Sea demonstrates that concentric collapse faulting around both diapirs and subcircular salt lows is common. The recognition of concentric collapse structures formed in response to salt withdrawal, and adjacent inflation, provides an alternative mechanism for the origin of the proposed Silverpit impact crater. 相似文献
23.
24.
25.
Several studies have suggested that geostatistical techniques could be employed to reduce overall transactions costs associated
with contracting for soil C credits by increasing the efficacy of sampling protocols used to measure C-credits. In this paper,
we show how information about the range of spatial autocorrelation can be used in a measurement scheme to reduce the size
of the confidence intervals that bound estimates of the mean number of C-credits generated per hectare. A tighter confidence
interval around the mean number of C-credits sequestered could increase producer payments for each hectare enrolled in a contract
to supply C-credits. An empirical application to dry land cropping systems in three regions of Montana shows that information
about the spatial autocorrelation exhibited by soil C could be extremely valuable for reducing transactions costs associated
with contracts for C-credits but the benefits are not uniform across all regions or cropping systems. Accounting for spatial
autocorrelation greatly reduced the standard errors and narrowed the confidence intervals associated with sample estimates
of the mean number of C-credits produced per hectare. For the payment mechanism considered in this paper, tighter confidence
intervals around the mean number of C-credits created per hectare enrolled could increase producer payments by more than 100
percent under a C-contract. 相似文献
26.
In this paper, we present a method to quantify the effectiveness of carbon mitigation options taking into account the `permanence' of the emissions reduction. While the issue of permanence is most commonly associated with a `leaky' carbon sequestration reservoir, we argue that this is an issue that applies to just about all carbon mitigation options. The appropriate formulation of this problem is to ask `what is the value of temporary storage?' Valuing temporary storage can be represented as a familiar economic problem, with explicitly stated assumptions about carbon prices and the discount rate. To illustrate the methodology, we calculate the sequestration effectiveness for injecting CO2 at various depths in the ocean. Analysis is performed for three limiting carbon price assumptions: constant carbon prices (assumes constant marginal damages), carbon prices rise at the discount rate (assumes efficient allocation of a cumulative emissions cap without a backstop technology), and carbon prices first rise at the discount rate but become constant after a given time (assumes introduction of a backstop technology). Our results show that the value of relatively deep ocean carbon sequestration can be nearly equivalent to permanent sequestration if marginal damages (i.e., carbon prices) remain constant or if there is a backstop technology that caps the abatement cost in the not too distant future. On the other hand, if climate damages are such as to require a fixed cumulative emissions limit and there is no backstop, then a storage option with even very slow leakage has limited value relative to a permanent storage option. 相似文献
27.
The use of microstructures for discriminating turbiditic and hemipelagic muds and mudstones
下载免费PDF全文
![点击此处可从《Sedimentology》网站下载免费的PDF全文](/ch/ext_images/free.gif)
The microstructures of turbiditic and hemipelagic muds and mudstones were investigated using a scanning electron microscope to determine whether there are microstructural features that can differentiate turbiditic from hemipelagic sedimentary processes. Both types of muddy deposits are, in general, characterized by randomly‐oriented clay particles. However, turbiditic muds and mudstones also characteristically contain aggregates of ‘edge‐to‐face’ contacts between clay particles with long‐axis lengths of up to 30 μm. Based on observations of the clay fabric of the experimentally‐formed muds settled from previously agitated muddy fluids, these types of aggregates, hereafter referred to as ‘aggregates of clay particles’, are interpreted as having been formed by the collision of component flocs in turbulent fluids. Furthermore, some aggregates of clay particles have ‘face‐to‐face’ contacts between clay particles; this is similar to face‐to‐face aggregates characteristically developed in fluid‐mud deposits that are commonly recognized only in turbiditic mudstones, indicating the possibility of a final stage of deposition under highly‐dense conditions, such as temporary fluid muds. In conjunction with earlier proposed lithofacies‐based and ichnofacies‐based criteria, aggregates of clay particles should be useful for the differentiation of turbiditic and hemipelagic muddy deposits, particularly with limited volumes of non‐oriented samples from deep‐water successions. 相似文献
28.
Glacial conditions that contribute to the regeneration of Fountain Glacier proglacial icing,Bylot Island,Canada
下载免费PDF全文
![点击此处可从《水文研究》网站下载免费的PDF全文](/ch/ext_images/free.gif)
Proglacial icings are one of the most common forms of extrusive ice found in the Canadian Arctic. However, the icing adjacent to Fountain Glacier, Bylot Island, is unique due to its annual cycle of growth and decay, and perennial existence without involving freezing point depression of water due to chemical characteristics. Its regeneration depends on the availability of subglacial water and on the balance between ice accretion and hydro‐thermal erosion. The storage and conduction of the glacial meltwater involved in the accretion of the icing were analyzed by conducting topographic and ground penetrating radar surveys in addition to the modelling of the subglacial drainage network and the thermal characteristics of the glacier base. The reflection power analysis of the geophysical data shows that some areas of the lower ablation zone have a high accumulation of liquid water, particularly beneath the centre part of the glacier along the main supraglacial stream. A dielectric permittivity model of the glacier – sediment interface suggests that a considerable portion of the glacier is warm based; allowing water to flow through unfrozen subglacial sediments towards the proglacial outwash plain. All these glacier‐related characteristics contribute to the annual regeneration of the proglacial icing and allow for portions of the icing to be perennial. Copyright © 2013 John Wiley & Sons, Ltd. 相似文献
29.