全文获取类型
收费全文 | 224篇 |
免费 | 9篇 |
国内免费 | 5篇 |
专业分类
测绘学 | 1篇 |
大气科学 | 3篇 |
地球物理 | 62篇 |
地质学 | 68篇 |
海洋学 | 57篇 |
天文学 | 25篇 |
综合类 | 2篇 |
自然地理 | 20篇 |
出版年
2024年 | 2篇 |
2021年 | 4篇 |
2019年 | 2篇 |
2018年 | 2篇 |
2017年 | 7篇 |
2016年 | 7篇 |
2015年 | 12篇 |
2014年 | 10篇 |
2013年 | 12篇 |
2012年 | 13篇 |
2011年 | 20篇 |
2010年 | 17篇 |
2009年 | 11篇 |
2008年 | 12篇 |
2007年 | 9篇 |
2006年 | 10篇 |
2005年 | 13篇 |
2004年 | 13篇 |
2003年 | 8篇 |
2002年 | 1篇 |
2001年 | 5篇 |
2000年 | 5篇 |
1998年 | 4篇 |
1997年 | 2篇 |
1996年 | 2篇 |
1995年 | 2篇 |
1994年 | 3篇 |
1993年 | 4篇 |
1992年 | 1篇 |
1989年 | 3篇 |
1988年 | 3篇 |
1987年 | 2篇 |
1986年 | 1篇 |
1984年 | 1篇 |
1983年 | 2篇 |
1982年 | 2篇 |
1981年 | 2篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1978年 | 1篇 |
1977年 | 1篇 |
1976年 | 2篇 |
1972年 | 1篇 |
1969年 | 1篇 |
排序方式: 共有238条查询结果,搜索用时 218 毫秒
211.
Tatsuo Matsuda Kentaro Omura Ryuji Ikeda Takashi Arai Kenta Kobayashi Koji Shimada Hidemi Tanaka Tomoaki Tomita Satoshi Hirano 《Tectonophysics》2004,378(3-4):143
An 1800-m-deep borehole into the Nojima fault zone was drilled at Nojima-Hirabayashi, Japan, after the 1995 Hyogo-ken Nanbu (Kobe) earthquake. Three possible fracture zones were detected at depths of about 1140, 1300, and 1800 m. To assess these fracture zones in this recently active fault, we analyzed the distributions of fault rocks, minerals, and chemical elements in these zones. The central fault plane in the shallowest fracture zone was identified by foliated blue-gray gouge at a depth of 1140 m. The degree of fracturing was evidently greater in the hanging wall than in the footwall. Minerals detected in this zone were quartz, orthoclase, plagioclase, and biotite, as in the parent rock (granodiorite), and also kaolinite, smectite, laumontite, stilbite, calcite, ankerite, and siderite, which are related to hydrothermal alteration. Biotite was absent in both the hanging wall and footwall across the central fault plane, but it was absent over a greater distance from the central fault plane in the hanging wall than in the footwall. Major element compositions across this zone suggested that hydrothermal alteration minerals such as kaolinite and smectite occurred across the central fault plane for a greater distance in the hanging wall than in the footwall. Similarly, H2O+ and CO2 had higher concentrations in the hanging wall than in the footwall. This asymmetrical distribution pattern is probably due to the greater degree of wall–rock fracturing and associated alteration in the hanging wall. We attributed the characteristics of this zone to fault activity and fluid–rock interactions. We analyzed the other fracture zones along this fault in the same way. In the fracture zone at about 1300 m depth, we detected the same kinds of hydrothermal alteration minerals as in the shallower zone, but they were in fewer samples. We detected relatively little H2O+ and CO2, and little evidence for movement of the major chemical elements, indicating little past fluid–rock interaction. In the fracture zone at about 1800 m depth, H2O+ and CO2 were very enriched throughout the interval, as in the fracture zone at about 1140 m depth. However, smectite was absent and chlorite was present, indicating the occurrence of chloritization, which requires a temperature of more than 200 °C. Only smectite can form under the present conditions in these fracture zones. The chloritization probably occurred in the past when the fracture zone was deeper than it is now. These observations suggest that among the three fracture zones, that at about 1140 m depth was the most activated at the time of the 1995 Hyogo-ken Nanbu (Kobe) earthquake. 相似文献
212.
Satoshi Nakagawa 《GeoJournal》2004,61(3):255-262
This study examines recent changes in the structure of migration and population by gender in the Extended Bangkok Region (EBR)
taking the influences of economic globalization into consideration. The EBR is understood here to consist of three concentric
zones, namely the Bangkok Metropolis (BM), the Vicinity and the Extended Urban Region (EUR). The spatial policy of the Thai
government has encouraged investors to build manufacturing factories outside the BM. Consequently the industrial structure
of the BM has turned strongly into service-dominated while the Vicinity and the EUR have attracted factories mainly owned
by foreign capitals. Light industries and electronics industries, both of which set up relatively earlier, concentrated on
the Vicinity, the adjacent provinces to the BM, while heavy and petrochemical industries are recently have developed in the
outer regions, the EUR. Service sectors and light industries as well as electronics industries prefer females to males to
employ as workers. As a consequence the population structures of the BM and the Vicinity became female-dominant while male
workers were likely to gather in the EUR attracted by heavy and petrochemical industries. The gender imbalance in the population
in the areas in concern may have been one of the consequences of the economic globalization of Thailand. The Thai government
supported the economic globalization through its investment promotion policy, but it seems that the government did not assume
the policy resulted in such gender imbalance. It can be suggested that in the future this gender imbalance may cause changes
in family formation behaviors of the Thai population.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
213.
Srivastava Nandita Gonzalez Walter D. Gonzalez Alicia L.C. Masuda Satoshi 《Solar physics》1998,183(2):419-434
Intense geomagnetic storms with DST index -100 nT were recorded on 9 March and 11 March 1993 associated with solar activity on 6 March and 9-10 March, respectively. In this paper, we discuss the characteristic features of the solar origins of the two events that gave rise to coronal and interplanetary disturbances and as a consequence produced strong geomagnetic activity at the Earth. The source of the activity in one case is attributed to a major 3M7.0 flare that occurred on 6 March 1993 and in the other case, to two large filament disruptions on the disk during 9-10 March, 1993. Both these sources were found to be located near changing or varying low-latitude coronal holes. They were also located close to the heliospheric currents sheets. Distinct X-ray activity was observed for both the events as observed by the Yohkoh SXT telescope. The detailed evolution and a comparison of these events on the basis of Yohkoh soft X-ray observations are presented here. 相似文献
214.
A framework for economic loss estimation due to seismic transportation network disruption: a spatial computable general equilibrium approach 总被引:4,自引:4,他引:0
This paper presents a framework for assessing the economic impact of disruption in transportation that can relate the physical
damage to transportation networks to economic losses. A spatial computable general equilibrium (SCGE) model is formulated
and then integrated with a transportation model that can estimate the traffic volumes of freight and passengers. Economic
equilibrium under a disruption in the transportation network is computed subject to the condition that the adjustment of labor
and capital inputs is restricted; the model reflects slow adjustment of these linked to the state of recovery. As a case study,
the model reviews the large Niigata-Chuetsu earthquake of 2004. Considering the damage to the transportation infrastructure,
the model indicates the extent of the economic losses arising from the earthquake distributed over regions as a consequence
of the intra- and interregional trade in a regional economy. The results show that 20% of the indirect losses occur in the
Niigata region directly affected by the earthquake, whereas 40% of the total losses are experienced in the Kanto region and
non-negligible losses reach rather remote zones of the country such as Okinawa. 相似文献
215.
We have detected the rotational lines of HCOOCH3 toward a Class 0 low-mass protostar, NGC1333 IRAS4B, which is reported to be extremely young according to the dynamical age
of the molecular outflow (a few 100 yr). This suggests that the complex organic molecules appear from the very early stage
of protostellar evolution. On the other hand, the complex organic molecules are not detected in a more evolved protostar,
L1527. We have also found a similar trend in a massive star forming region, NGC2264. The HCOOCH3 emission is almost absent toward IRS1, whereas it is concentrated near MMS3, which is younger than IRS1. In addition, the
HCOOCH3 intensity peak is slightly shifted from the dust emission peak, as is seen in the Orion KL Compact Ridge, giving an important
clue to solve its origin. 相似文献
216.
Geoelectric and hydrologic surveys during spring tides revealed the spatiotemporal distribution of groundwater quality produced by tidal forcing in Fongafale Islet, Funafuti Atoll, Tuvalu. The observed low resistivity showed that saline water largely immersed the surficial Holocene aquifer, indicating that there is no thick freshwater lens in Fongafale Islet, unlike in other atoll islands of comparable size. Half of the islet was constructed by reclaiming the original swamp with porous, highly permeable coral blocks; this reclaimed area should not be considered as part of the islet width for calculation of the expected thickness of the freshwater lens. The degree of aquifer salinization depends on the topographic characteristics and the hydrologic controls on the inland propagation of the tidal forcing. Large changes in bulk resistivity and the electrical conductivity of groundwater from wells indicate that periodic salinization in phase with the semidiurnal tides was occurring widely, especially in areas at lower elevation than the high-tide level and in reclaimed areas with high permeability. Thin sheets of nearly fresh and brackish water were observed in the surficial aquifer in areas above the high-tide level and in taro swamps, respectively. The thinness of the brackish and freshwater sheets suggests that the taro swamps and the fresh groundwater resources of the islet are highly vulnerable to salinization from anticipated sea-level rise. An understanding of the inherent geologic and topographic features of an atoll is necessary to evaluate the groundwater resources of the atoll and assess the vulnerability of its water resources to climate change. 相似文献
217.
Yasuyuki Muramatsu Yukari Takada Hiroyuki Matsuzaki Satoshi Yoshida 《Quaternary Geochronology》2008,3(3):291-297
Analytical procedures in the determination of iodine-129 (half-life: 1.6×107 y) have been studied using accelerator mass spectrometry (AMS), with special references to the separation procedures of iodine from soil samples for the AMS measurement. Iodine was successfully volatilized from soil samples by pyrohydrolysis at 1000 °C and collected in a trap solution. Iodine was purified from the matrix by solvent extraction. Finally, it was precipitated as silver iodide to make a target for AMS. In order to obtain information on the 129I/127I ratio in a chemical blank (or iodine carrier), we have determined the ratios in several iodine reagents and found that the ratios fell in a narrow range around 1.7×10−13. The detection limit for soil sample (1 g material) by the present method was about 0.01 mBq/kg or 4×10−11 as the ratio of stable iodine (129I/127I ratio), i.e. these values were much better than that by neutron activation analysis (NAA) used in our previous studies. We have applied this method in the analysis of soil samples collected from different places in Japan. We could successfully determine 129I in soil samples with low 129I concentrations, which could not be detected by NAA. Sample size necessary for the soil analysis by AMS was only about 0.5 g or less, whereas about 100 g of the sample were required for NAA [Muramatsu, Y., Ohmomo, Y., 1986. Iodine-129 and iodine-127 in environmental samples collected from Tokaimura/ Ibaraki, Japan. Sci. Total Environ. 48, 33-43]. Using this method, new data were obtained for the 129I levels in 20 soil samples collected from background areas far from nuclear facilities, and the ranges were 1.4×10−5−4.5×10−3 Bq/kg as 129I concentrations and 3.9×10−11−2.2×10−8 as 129I/127I ratios. These values are useful in understanding the 129I levels in Japanese environments. Higher 129I concentrations were observed in forest soils than those in field and rice paddy soils should be related to the interception effect of atmospheric 129I due to tree canopies. Relatively high 129I/127I ratios found in rice paddy soils could be explained by their low stable iodine concentrations which were caused by the desorption of stable iodine from the rice paddies during the cultivation. 相似文献
218.
Dredged spoil (DS) was used as a silt and clay additive in the construction of artificial tidal flats from mountain sand (MS). As the ratio of DS in the sediment media increased, the number of emerging macrobenthos increased. The composition of the macrobenthic community was also affected by the addition of DS, and the changes might be dependent on the ratio of DS to MS. In addition, the macrobenthos in the artificial tidal flats was more abundant than that in the control tidal flat, which was constructed with natural tidal flat sediment. With a silt and clay content of 25%, polychaetes Ceratonereis erythraeensis and Capitella sp. and the gastropod Batillaria cumingii were dominant, whereas no bivalves were present. With less silt and clay (5% and 10%), the bivalves Ruditapes philippinarum and Musculista senhousia were observed in the artificial flats, while their numbers in the control tidal flat were lower. 相似文献
219.
Satoru Kojima Kazuhiro Tsukada Shigeru Otoh Satoshi Yamakita Masayuki Ehiro Cheikhna Dia Galina Leontievna Kirillova Vladimir Akimovich Dymovich Lyudmila Petrovna Eichwald 《Island Arc》2008,17(4):502-516
The Anyui Metamorphic Complex (AMC) of Cretaceous age is composed of metachert, schist, gneiss, migmatite and ultramafic rocks, and forms a dome structure within the northernmost part of the Jurassic accretionary complex of the Samarka terrane. The two adjacent geological units are bounded by a fault, but the gradual changes of grain size and crystallinity index of quartz in chert and metachert of the Samarka terrane and the AMC, together with the gradual lithological change, indicate that at least parts of the AMC are metamorphic equivalents of the Samarka rocks. Radiolarian fossils from siliceous mudstone of the Samarka terrane indicates Tithonian age (uppermost Jurassic), and hence, form a slightly later accretion. This signifies that the accretionary complex in the study area is one of the youngest tectonostratigraphic units of the Samarka terrane. The relationship between the Samarka terrane and AMC, as well as their ages and lithologies, are similar to those of the Tamba–Mino–Ashio terrane and Ryoke Metamorphic Complex in southwest Japan. In both areas the lower (younger) part of the Jurassic accretionary complexes were intruded and metamorphosed by Late Cretaceous granitic magma. Crustal development of the Pacific‐type orogen has been achieved by the cycle of: (i) accretion of oceanic materials and turbidites derived from the continent; and (ii) granitic intrusion by the next subduction and accretion events, accompanied by formation of high T/P metamorphic complexes. 相似文献
220.
Color-change processes of a plinian pumice and experimental constraints of color-change kinetics in air of an obsidian 总被引:1,自引:0,他引:1
Mihoko Moriizumi Satoru Nakashima Satoshi Okumura Yuta Yamanoi 《Bulletin of Volcanology》2009,71(1):1-13
Colors of plinian pumices were measured by spectrocolorimetry, and their quantitative color parameters in the L*a*b* color
space were determined. A series of heating experiments of obsidian was conducted to simulate the color-change processes of
rhyolitic glasses. In these experiments, following three stages of color-change processes were observed. Stage I showed a
rapid b* (yellowishness) increase associated with fast dehydration controlled by water diffusivity (D
water). In stage II, a* (reddishness) increase was accompanied by Fe2+ decrease. Both a* increase and Fe2+ decrease can be simulated by a diffusion model. Obtained diffusivity D
oxidation were about two orders of magnitude smaller than D
water
. The a*-value increase after the oxidation in stage III appeared to be quasi-linear with time, indicating the zeroth order
reaction corresponding to the formation of hematite-like structures in rhyolitic glasses. The diffusion-limited a* increase
model in stage II was applied to a natural plinian pumice fall unit to evaluate time periods of color-change processes through
oxidation by air of fragmented rhyolitic materials. 相似文献