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31.
本文研究了1920年以来,云南地区M_s≥4.7级地震的时间序列及空间分布的特征标度。结果表明,当区内M_s≥4.7级地震在时间序列上出现我们定义的平静段和活跃段后,分别于418天和312天内即可能发生6级以上地震,对应率分别为71%和87%,1920年以来云南11次M_s≥6.8级地震前,出现活跃和平静特征标度的各5次。在空间上绝大多数(80%)大震震中处于我们所定义的长时间大范围空白缺震背景区或相对少震区内,仅少数(20%)位于4.7级以上地震相对密集区内或附近。4.7级以上地震上述时间序列及空间分布特征标度,可以作为云南6级,特别是6.8级以上地震中期或短期预测的判据和指标。同时可以看出,云南6级以上地震前,4.7级以上地震在时空演变上,经历了从无序到有序的演化过程。 相似文献
32.
Land surface temperature is a key parameter in monitoring the status of crop water stress by remote sensing, and studying the water and energy balance in cropland ecosystem. The component temperatures of crop and soil are especially significant in remote … 相似文献
33.
为了促进现代化的实现,作者试图找出中国与发达国家之间的经济差距,并选取了世界银行公布数据的三个指标,代入自己设计的简便公式,测得中国与韩国、希腊的经济差距为26年(以2000年基准)。于是作者将发达国家分为一般发达国家和高度发达国家,把发展中国家分为一般发展中国家和发展中的发达国家。作者预计2020年中国将达到发展中的发达国家水平。并预测中国将在2007年经济总量超英国;中国与英国的人均水平差距约为34年。中国与美国经济总量的差距约为35年,中美之间的人均水平差距约为44年,动态差距将在50年以上。结论,中国在2030年将可达到一般发达国家水平,即可实现现代化。 相似文献
34.
There is general agreement that calc-alkaline volcanic rocks at convergent plate margins are genetically related to the process of subduction (Ringwood, 1974; Maaloe and Petersen, 1981; Hawkesworth et al., 1997). However, opinions on the mode and site of generation of primary magma for island arc volcanism differ substantially. The site of generation of calc-alkaline magma is thought to be either in the mantle wedge (Plank and Langmuir, 1988; McCulloch and Gamble, 1991) or in the subducting slab (White and Dupré, 1986; Defant and Drummond, 1990; Edwards et al., 1993; Ryan and Langmuir, 1993). We present seismological evidence in favour of the latter concept. A distinctive seismicity pattern around and under the Krakatau volcano was identified during systematic studies of the SE Asian convergent plate margins by means of global seismological data. A column-like cluster of events, probably associated with the dynamics of the volcano, is clearly separated from the events in the Wadati-Benioff zone. The accuracy of hypocentral determinations of the events of the cluster does not differ from the accuracy of the events belonging to the subducting slab. The depths of the cluster events vary from very shallow to about 100 km without any apparent discontinuity. On the other hand, there is a pronounced aseismic gap in the Wadati-Benioff zone directly beneath the volcano at depths between 100-150 km. The Krakatau cluster connects this aseismic gap to the volcano at the surface. The pervasive occurrence of earthquakes in the continental wedge between the subducting slab and the Earth surface bears witness to the brittle character of the continental lithosphere and casts doubt on the existence of large-scale melting of mantle material. The aseismic gap (Hanu and Vank, 1985), interpreted by us as a partially melted domain occurring in subducted slabs in practically all active subduction zones that reach depths greater than 100 km, is here used as evidence for the location of the primary source region of island arc volcanics in the subducting plate. 相似文献
35.
基于随机振动理论确定桥梁地震碰撞的临界间隙 总被引:2,自引:1,他引:2
确定梁桥邻跨间避免地震碰撞的最小间隙,对于梁桥地震碰撞危险性预测及防地震碰撞措施的设计有着显著意义。本文基于随机振动理论建立梁桥地震碰撞邻跨临界间隙的计算方法,分析模型采用跨径不等的两跨简支梁桥,且考虑隔震支座非线性恢复力的影响。文中首先建立了系统的非线性运动方程;随后运用随机等效线性化理论将其线性化;最后在复模态空间推导了临界碰撞间隙的均值与方差的计算方法。人工地震动的非线性时程分析结果验证了本文算法的正确性。参数分析表明,临界间隙随邻跨长度比增大而增大,随支座屈服力与上部结构重量比值减小而增大,随隔震支座屈服位移增大而增大,随桥墩振动周期增大而增大。隔震支座屈服前后刚度比值对临界间隙大小影响很小。 相似文献
36.
37.
同源岩浆成因金矿成岩成矿时差的统计研究 总被引:2,自引:2,他引:2
同源岩浆成因金矿的成岩成矿时差是确定矿床与岩浆岩成因关系的重要基础。而中国同源岩浆成因金矿分布十分广泛,前人在成矿学和岩石学方面做了大量的研究,为此本文收集了国内一些典型金矿的成矿和相关同源岩浆岩的同位素测年数据,讨论并定量厘定了该类金矿床成岩成矿时差的分布特征及分布范围。数据统计分析及柯尔莫哥洛夫准则检验结果显示,成矿事件一般同步或略滞后于同源岩浆活动,成岩成矿时差在95%信度下服从正态分布,介于0~16.0Ma,均值约为7.0Ma。因此,若金矿成岩成矿存在着≤16.0Ma的时差,就应该重视二者之间的同源成因联系。同时,笔者也强调:准确的成岩成矿时差应加强对金矿成岩成矿地质背景的研究;重视时差研究与微量元素和同位素示踪相结合,从年代学和地球化学方面对矿床成因作出合理的解释。 相似文献
38.
A polymetallic zone dominated by U-W mineralization was found in Northeast Guangxi. Distributed along the east contact zone
of a complex granite mass, it extends for about 100 km in length, with more than fifty deposits and prospects embraced. The
deposits show a wide range of genetic types, related to the granite, from magmatic (including pegmatite and skarn deposits)
through hydrothermal mineralizations (hypo-, meso- and epithermal) all the way to tin placers, constituting a very intact
metallogenetic series of granites. The epithermal U-W deposits are considered as a new type for their unique geological and
geochemical characters, such as the paragenesis of U and W and the large time gap (> 40 Ma) between ore and granite.
This project was financially supported by the Open Lab. of Ore Deposit Geochemistry, Chinese Academy of Sciences. 相似文献
39.
N. F. Vojkhanskaja 《Astrophysics》2007,50(3):351-361
Cataclysmic variables (CV) and pre-cataclysmic binaries (PCB) are discussed. The main difference between them (accretion or
its absence) is shown to be a consequence of the evolutionary process and the properties of their progenitors. Both types
of system have a bimodal distribution of their periods, but the extrema are in counterphase. Luminosity-effective temperature
diagrams for the primary components are used to show that both systems have approximately the same age, which conflicts with
the notion of PCBs as precursors of CVs. Calculations of the maximum distance between components for which the system remains
stable show that CVs have passed this limit, while PCBs maintain their stability during this evolution. It is suggested that,
after ejecting a common shell, future CVs immediately become semi-detached systems. It this is so, then there must be cataclysmic
variables which are the central stars of planetary nebulae.
__________
Translated from Astrofizika, Vol. 50, No. 3, pp. 427–439 (August 2007). 相似文献
40.
Kesang WANGCHUK András DARABANT Prem Bahadur RAI Maria WURZINGER Werner ZOLLITSCH Georg GRATZER 《山地科学学报》2014,11(5):1182-1191
We investigated whether species richness, diversity and density of understory herbaceous plants differed along logging(gap) and grazing(primarily by cattle) disturbance gradients, and sought to identify drivers of richness, diversity and density of understory vegetation of logged sites. A factorial experiment was conducted in the mixed conifer forest of Gidakom in Western Bhutan. Levels of the logging treatment included small(0.15 – 0.24 ha), medium(0.25 – 0.35 ha) and large(0.36 – 1.31 ha) gaps. The grazing treatment included grazed(primarily by cattle) and ungrazed(where herbivores were excluded by a fence) plots nested within each gap. Data were collected from 12 gaps(4 replicates at each level of logging) using the point intercept method. Shannon Weaver Diversity and Margalef's indices were used to estimate species diversity and describe species richness, respectively. Soil samples were analyzed for pH and nutrients. The interaction effect of logging and grazing was significant(p≤0.001) only on species diversity. Relative to ungrazed areas, species diversity was significantly higher(0.01≤p≤0.05) in medium grazed gaps. Under grazed conditions, soil P was negatively correlated with gap size and species diversity. While species diversity was positivelycorrelated(0.01≤p≤0.05) with soil N in grazed plots species richness was positively correlated(0.001≤p≤0.01) with soil N in ungrazed plots. Relative density of Yushania microphylla and Carex nubigena were higher under ungrazed conditions. Our study suggests that the combined effect of cattle grazing and logging results in higher species diversity of understory vegetation in medium and grazed gaps in mixed conifer forests of Bhutan,whereas increase or decrease in relative density of major species is determined primarily by the independent effects of grazing and logging. From management perspective, forest managers must refrain from creating large gaps to avoid loss of nutrients(mainly P and N), which may eventually affect tree regeneration. Managers intending to maintain understory vegetation diversity must consider the combined effects of grazing and logging, ensuring low to moderate grazing pressure. 相似文献