地震自相似现象初探   总被引：2，自引：1，他引：2  

李海华  张勇利 《内陆地震》1990,4(4):292-300

依据破裂过程和震源物理参数相似性,给出了自相似震源椭球体三轴之比约为a:b:c=1:0.2:0.2。基于分维理论和方法,讨论了自相似的地震时空分布的分维和强震前的降维现象。由前兆展布范围,大震前区域地震活动特征以及地震空区等可导出近源前兆(红肿)区线性尺度约为震源区的5倍。  相似文献   

新疆阿尔泰花岗岩类源区物质的定量模拟   总被引：6，自引：1，他引：6  

刘伟 《大地构造与成矿学》1991,15(3):199-207

对产出于阿尔泰、额尔齐斯、乌化古三条构造-岩浆带上的六个典型岩体进行了源区岩石化学组成和初始熔体部分熔融程度的定量模拟。模拟结果表明:六个岩体的ε_(Sr)~t值多介于0-120之间,源区岩石多为地幔物质与陆壳物质的混合源,地壳柱中成熟陆壳所占比例较少,反映了中亚型地洼区在地壳化学结构上的一个重要特征.从北往南,ε_(Sr)~t值与壳源锶所占百分率逐渐减小,反映了从地槽造山带核心部位往边缘部位往边缘部位,地壳柱中成熟陆壳所占比例逐渐减小。初始熔浆部分熔融程度温度、压力呈正消长关系。  相似文献   

STUDY ON CORRELATIVE EARTHQUAKES AND SEISMIC WINDOW NETWORK IN TIANSHAN REGION     

Wang Gulling Ao Xueming 《内陆地震》1991,(4)

In this paper , by using the seismic data of strong earthquake (M≥7) which have occurred since 1900,correlative features of strong earthquake activity in Tianshan region which crosses China and USSR have been studied . Meanwhile , we selected 15 seismic windows (11 in China , 4 in USSR) by censusing , systematically researching and statistically examing seismic data of regional seismic network which are in Chian and USSR.The anomalous features of seismic window and seismic window network , prediction index and prediction plan have been studied . In the same time ,its prediction efficency have been evaluated . Several examples of successful earthquake prediction are given out in this paper .Finally ,the possible physical mechanism of the results are discussed.  相似文献   

环境遥感的未来十年——祝贺中国地理学会环境遥感分会成立10周年     

陈述彭 《遥感学报》1991,(3)

过去十年,随着卫星航空信息日渐丰富,作为国家重点攻关项目的遥感技术不断开拓了应用的新领域,初步形成了一个新的高科技信息服务行业。“八五”期间,遥感又列为重点项目,预期气象卫星信息的开发与应用,将会再次出现高潮。在资源卫星群星灿烂,航空遥感持续发展的形势下,需要充分利用现有设备潜力和所取得的技术进步,集中力量,研制大容量存储,实时传输和快速处理功能的智能化技术系统。这样才能适应防灾,估产为主要目标,并兼顾开放城市及全球研究的需求。  相似文献   

东秦岭灰池子花岗岩基岩石地球化学特征及其成因     

张正伟 《岩石学报》1991,7(3)

灰池子花岗岩基主要由黑云斜长混合花岗岩和二长混合花岗岩组成。前者是加里东期的交代花岗岩;后者是在海西晚期钾交代作用再次改造先期岩石形成的。因此是一个由多次交代作用形成的混合花岗岩岩基。本文从构造地球化学的某些观点讨论这种岩石形成过程中钾元素迁移机制。  相似文献   

Geochemistry of the Baishitouquan Amazonite—and Topaz—bearing Granite in the Mid—Tianshan Belt,Xinjiang,China     

Gu Lianxing  Yang Hao  Gou Xiaoqin  Guo Jichun  Wang Jinzhu 《中国地球化学学报》1994,13(4):289-304

The Baishitouquan amazonite and topaz-bearing granite is one of the typical high-rubidium and high-fluorine granites in the eastern part of the Mid-Tianshan belt. This intrusion is in sharp contact with Mid-Proterozoic schists, gneisses and marbles, and is composed of four zones transitional from the bottom upwards: leucogranite, amazonite granite, topaz-bearing amazonite granite and topaz quartz albitite. The Baishitouquan granite contains highly ordered K-feldspar, Li-rich mica, Mn-rich garnet, α-quartz and low temperature zircon and is chemically high in Si, K, Na, Al, Li, Rb, Cs and F, and low in Ti, Fe, Ca, Mg, P, Co, Ni, Cr, V, Sr and Ba, with Na₂O<K₂O. Amazonite from the amazonite granite zone contains 1867 ppm Rb. The F contents of bulk rocks are 3040 and 4597 for the amazonite granite and topaz-bearing amazonite granite zones, respectively. These two zones have δ¹⁸O values of 8.97–9.85‰ (SMOW) and show flat REE distribution patterns with strong Eu depletion. K-Ar and Rb-Sr ages of this intrusion are 226. 6 Ma and 209. 6 Ma respectively, with an initial⁸⁷Sr/⁸⁶Sr ratio of 0.987±0.213. The Baishitouquan granite is the product of crystallization of a low temperature, and water, rubidium and fluorine-rich magma, which may have been derived from partial melting of muscovite-rich crustal rocks. Consolidation of this granite involved two contrasting and successive stages: melt crystallization and hydrothermal metasomatism and precipitation. Various geological features of this granite were formed during the transition from the magmatic to the hydrothermal stage.  相似文献   

震源系统不稳定度指标和强震短临预报   总被引：1，自引：0，他引：1       下载免费PDF全文

秦保燕  王裕仓  温增平  李亚荣 《地震工程学报》1994,16(4):1-9

在探讨震源系统不稳定产生的物理基础前提下，应用调制模式提出了利用小震日频次起伏加剧与外因的相关性进行强震的短临时间预报的设想，具体提出了调制小震频次起伏加剧的两个判别震源系统不稳定度的指标λ＿１和λ＿２。前者为单因子调制指标，后者为多因子调制或多因子调制强化指标。关于大震的地点预报，应用立交模式短临阶段出现调制小震通过未来大震的共轭小震活动条带进行预报。  相似文献   

矿物热释氡找矿方法中氡的来源探讨     

苏守田 《铀矿地质》1985,(2)

本文探讨了矿物热释氡找矿中氡的来源问题。我们对七五二花岗岩中铀矿床的无矿及含矿花岗岩用闪烁射气法进行了各种温度间的矿物热释氡量的测定;用包裹体爆裂法进行了爆裂温度及相对爆裂次数的测定。通过实验发现,加热样品在包裹体爆裂以前,能释放出大部分氡,在包裹体大量爆裂的温度区间热释氧量反而很少。磨破包裹体放出氡后,再加热仍然有氡气释放出来。用包裹体中的铀含量计算出的氡量低于测定方法的灵敏度,无法测出,说明矿物热释氡量与包裹体无关。样品又做了化学铀分析和放射化学镭分析。明显看出热释氡量与铀、氡含量成正相关关系。各种实验均证明氧气不是来自包裹体,而是来源于整个矿物。  相似文献   

Surface runoff and sediment yield in the Ardèche rangelands     

J. M. Roels 《地球表面变化过程与地形》1984,9(4):371-381

This paper presents a case study of runoff and sediment generation under Submediterranean rangeland conditions (Ardèche drainage basin, France). Measurements indicate that on a rough hillslope interrill runoff and sediment are not produced uniformly over the slope surface. It is observed that runoff concentrates immediately in non-permanent interrill flow paths, which under average storm conditions vary in length from 1.0 to 12.5 m. Long interrill flow paths may eventually become permanent. These permanent flow paths, called pre-rills, are introduced as a new source area, and are considered to be the initial stage in the development of rills. Along pre-rills considerable quantities of runoff and sediment are carried away. This study also shows that calculations based on interrill, pre-rill, and rill runoff will only have significance if storm and soil conditions are specified in detail. It is concluded from a correlation analysis between the runoff volume and the amount of soil loss on a storm-by-storm basis that the runoff volume alone cannot explain the amount of sediment that is generated in each source area; soil availability is an additional factor that must be taken into account.  相似文献   

东亚大陆地震的地球自转动力观测资料分析          下载免费PDF全文

安欧 《地震地质》1987,9(4):71

东亚大陆大地震的活动带走向、活动方式、震源主压应力方向、总迁移方向,沿纬度的分布和发震频度随时间的变化,均与地球自转速率变化有成因联系。本文从地球自转加速、减速、匀速的变化趋势进行这方面的观测资料分析,证明地球速率变化是东亚大陆地震的基本动力来源  相似文献