全文获取类型
收费全文 | 149篇 |
免费 | 7篇 |
国内免费 | 3篇 |
专业分类
测绘学 | 3篇 |
大气科学 | 11篇 |
地球物理 | 20篇 |
地质学 | 53篇 |
海洋学 | 10篇 |
天文学 | 23篇 |
综合类 | 2篇 |
自然地理 | 37篇 |
出版年
2024年 | 2篇 |
2023年 | 1篇 |
2022年 | 1篇 |
2021年 | 5篇 |
2019年 | 3篇 |
2018年 | 5篇 |
2017年 | 5篇 |
2016年 | 6篇 |
2015年 | 1篇 |
2014年 | 3篇 |
2013年 | 8篇 |
2012年 | 7篇 |
2011年 | 13篇 |
2010年 | 8篇 |
2009年 | 9篇 |
2008年 | 7篇 |
2007年 | 9篇 |
2006年 | 5篇 |
2005年 | 7篇 |
2004年 | 4篇 |
2003年 | 4篇 |
2002年 | 2篇 |
2001年 | 4篇 |
2000年 | 5篇 |
1999年 | 4篇 |
1998年 | 3篇 |
1994年 | 3篇 |
1992年 | 3篇 |
1991年 | 1篇 |
1990年 | 1篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1986年 | 5篇 |
1985年 | 2篇 |
1984年 | 3篇 |
1983年 | 2篇 |
1982年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1976年 | 2篇 |
1974年 | 1篇 |
排序方式: 共有159条查询结果,搜索用时 15 毫秒
61.
Greater Mekong Subregion: From Geographical to Socio‐Economic Integration edited by Omkar L. Shrestha and Aekapol Chongvilaivan (eds). Institute of Southeast Asian Studies,Singapore, 2013, pp. xvi + 270 (ISBN 978‐981‐4379‐68‐7) 下载免费PDF全文
Victor R. Savage 《Singapore journal of tropical geography》2015,36(2):276-278
62.
63.
64.
We analyze earthquakes occurring in and around the Rotorua and Kawerau geothermal systems, Taupo Volcanic Zone, New Zealand. The two data sets contain 504 and 1875 shallow (≤ 20 km deep) earthquakes, respectively, and span the 21 year period between 1984 and 2004. The arrival time data for these earthquakes are first used to calculate 1-D P- and S-wave seismic velocity models and accompanying station correction terms for both areas. In order to address the non-uniqueness of the joint hypocenter-velocity model estimation problem, we analyze suites of 1000 velocity models computed from random initial models. The final velocity models are well constrained, particularly at depths between 4 and 15 km, and consistent with the results obtained in previous seismic refraction studies of the central Taupo Volcanic Zone. Using a combination of cross-correlation-derived and catalog-based arrival times, we relocate subsets of the Rotorua and Kawerau data sets. In Rotorua, the relocated earthquakes cluster near the geothermally active parts of Rotorua City and beneath the Mount Ngongotaha rhyolite dome. Earthquake clusters and alignments reveal seismogenic structures in the mid-crust whose positions and geometries are consistent with previously published fault mechanisms and known near-surface faults. In Kawerau, the earthquakes within the geothermal field align along northeast-trending lineations, consistent with the predominant alignment of surface-mapped faults in the area. 相似文献
65.
66.
Lydia A. Olaka Eric O. Odada Martin H. Trauth Daniel O. Olago 《Journal of Paleolimnology》2010,44(2):629-644
Sequences of paleo-shorelines and the deposits of rift lakes are used to reconstruct past climate changes in East Africa.
These recorders of hydrological changes in the Rift Valley indicate extreme lake-level variations on the order of tens to
hundreds of meters during the last 20,000 years. Lake-balance and climate modeling results, on the other hand, suggest relatively
moderate changes in the precipitation-evaporation balance during that time interval. What could cause such a disparity? We
investigated the physical characteristics and hydrology of lake basins to resolve this difference. Nine closed-basin lakes,
Ziway-Shalla, Awassa, Turkana, Suguta, Baringo-Bogoria, Nakuru-Elmenteita, Naivasha, Magadi-Natron, Manyara, and open-basin
Lake Victoria in the eastern branch of the East African Rift System (EARS) were used for this study. We created a classification
scheme of lake response to climate based on empirical measures of topography (hypsometric integral) and climate (aridity index).
With reference to early Holocene lake levels, we found that lakes in the crest of the Ethiopian and Kenyan domes were most
sensitive to recording regional climatic shifts. Their hypsometric values fall between 0.23–0.29, in a graben-shaped basin,
and their aridity index is above unity (humid). Of the ten lakes, three lakes in the EARS are sensitive lakes: Naivasha (HI
= 0.23, AI = 1.20) in the Kenya Rift, Awassa (HI = 0.23, AI = 1.03) and Ziway-Shalla (HI = 0.23, AI = 1.33) in the Main Ethiopian
Rift (Main Ethiopian Rift). Two lakes have the graben shape, but lower aridity indices, and thus Lakes Suguta (HI = 0.29,
AI = 0.43) and Nakuru-Elmenteita (HI = 0.30, AI = 0.85) are most sensitive to local climate changes. Though relatively shallow
and slightly alkaline today, they fluctuated by four to ten times the modern water depth during the last 20,000 years. Five
of the study lakes are pan-shaped and experienced lower magnitudes of lake level change during the same time period. Understanding
the sensitivity of these lakes is critical in establishing the timing or synchronicity of regional-scale events or trends
and predicting future hydrological variations in the wake of global climate changes. 相似文献
67.
The potential of teleost scales as indicator tissues of recent dietary history was investigated in the estuarine fish, Notolabrus celidotus. Treatment fish were fed a 15N-enriched bivalve diet (δ15N = 108.8‰) for up to 90 days to examine integration of the dietary source signature in scale margin, regenerated scale, and
dorsal muscle tissues. Regenerated scales exhibited the greatest and most rapid enrichment in δ15N (to 53.4 ± 5.0‰) of the tissues examined. Scale margin δ15N signatures also increased significantly from 14.5‰ to 30.9 ± 6.0‰, while muscle tissue only increased by 2.8‰ after 90 days.
Dietary contribution models suggested that isotopic equilibration of dietary nitrogen would be most rapid in regenerated scales,
followed by scale marginal increments and then muscle. In conclusion, teleost scales hold considerable potential as novel,
nondestructive indicators of recent dietary history, yet currently face constraints from uncertainties in isotopic integration
mechanisms. 相似文献
68.
S. A. Penkett K. C. Clemitshaw N. H. Savage R. A. Burgess L. M. Cardenas L. J. Carpenter G. G. McFadyen J. N. Cape 《Journal of Atmospheric Chemistry》1999,33(2):111-128
Detailed studies have been made of the behaviour of gases and radicals involved in the production of oxidants at the Weybourne Atmospheric Observatory in both summertime and wintertime conditions. In June 1995 the range of meteorological conditions experienced varied such that ozone destruction was observed in clean northerly air flows reaching Weybourne down the North Sea from the Arctic, and ozone production was observed in varying degrees in air with different loadings of nitrogen oxides and other precursors. The transition point for ozone destruction to ozone production occurred at a nitric oxide concentration of the order of 50 pptv. Plumes of polluted air from various urban areas in the U.K. were experienced in the June campaign at Weybourne. Quantitative studies of ozone production in a plume from the Birmingham conurbation on 18 June 1995 showed that the measurement of ozone production agreed well with calculated production rates from the product of the nitric oxide and peroxy radical concentrations (r2=0.9). In wintertime conditions (October–November 1994) evidence was also found for oxidant production, defined as the sum of O3+NO2. At this time of year the peroxy radical concentrations (RO2) were much lower than observed in the summertime and the nitric oxide (NO) was much higher. There was still sufficient RO2 during the day, however, for a slow accumulation of oxidant. Confirmatory evidence for this comes from the diurnal co-variance of (O3+NO2) with PAN, an excellent tracer of tropospheric photochemistry. The same type of covariance occurs in summer between PAN and ozone. The results obtained in these series of measurements are pertinent to understanding the measures necessary to control production of regional photochemical air pollution, and to the production of ozone throughout the northern hemisphere in winter. 相似文献
69.
70.
Ann Savage 《Astrophysics and Space Science》1986,119(1):239-242
Several programmes are making use of UKST Sky Survey plates to identify southern radio sources. The fine-grain modern plates and accurate radio positions give a much improved identification rate. It seems that it will very soon be possible to determine whether or not there is a quasar redshift cut-off at z4. There is an urgent need for more accurate fundamental reference star positions in the South.Paper presented at the IAU Third Asian-Pacific Regional Meeting, held in Kyoto, Japan, between 30 September–6 October, 1984. 相似文献