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41.
We have studied a set of equations with nonlinear and nonadiabatic terms which describes a simple oscillator. The equations have only one fixed point located at the origin. It is found that the oscillator shows the sequence of the period-doubling for the change of a parameter and results in chaotic oscillation. We illustrated the behaviour of the oscillator for several set of parameters and showed that the equations of the oscillator can be reduced to the one-zone model of stellar pulsation with simple nonlinear terms. It is suggested that the stellar irregular variability is resulted from the chaotic motion due to the nonlinear effect. 相似文献
42.
The third order theory of coupling is discussed regarding the radial pulsation of stellar models. 相似文献
43.
陕西双王含金角砾岩体为水压角砾岩体,是深源富碱含金流体使泥盆系一套热水沉积的富钠质岩系发生水力压裂作用形成的。早期共轴递进挤压使能干性富钠质岩系与非能干性富泥质岩系发生变形分离,分别形成近等距分布的透镜状弱变形域与线性强变形带,其中,弱变形域中央是一个相对低温,低压,高渗透率的透镜状天然泵吸中心;晚期的右旋高角度斜冲非共轴递进剪切使弱变形域中央最发育的一组节理和裂隙由压性转变为张性,并沟通溶 部的裂隙系统,泵吸中心巨大的压力降使深部的承压流体在富钠质岩系中产生周期性的构造泵吸一水力压裂-沉淀愈合作用,根据分解变形构造型式预测的隐伏含金水压角砾岩体已获钻探初步验证。 相似文献
44.
邵东保和堂矿区龙潭组1,2煤形成地下三角洲平原废弃期,3煤形成于三角洲建设期,前者聚煤条件较好。在三角洲废弃破坏期,潮汐水流对形成于三角洲平原的煤层有较强的发行作用。本文提出了潮汐对煤厚,煤质及煤岩组成的作用机制。 相似文献
45.
新化古台山金锑矿床蚀变特征及其找矿方向 总被引:3,自引:0,他引:3
本文结合古台山金锑矿床地质特征,着重分析了围岩蚀变类型及其分带,分布规律与矿化的关系,阐述了围岩蚀变特征及其找矿意义。 相似文献
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48.
The 2013 European Seismic Hazard Model: key components and results 总被引:11,自引:5,他引:6
Jochen Woessner Danciu Laurentiu Domenico Giardini Helen Crowley Fabrice Cotton Gottfried Grünthal Gianluca Valensise Ronald Arvidsson Roberto Basili Mine Betül Demircioglu Stefan Hiemer Carlo Meletti Roger W. Musson Andrea N. Rovida Karin Sesetyan Massimiliano Stucchi The SHARE Consortium 《Bulletin of Earthquake Engineering》2015,13(12):3553-3596
49.
Mine Betül Demircioğlu Karin Şeşetyan Tamer Y. Duman Tolga Çan Senem Tekin Semih Ergintav 《Bulletin of Earthquake Engineering》2018,16(8):3399-3438
Over the years, several local and regional seismic hazard studies have been conducted for the estimation of the seismic hazard in Turkey using different statistical processing tools for instrumental and historical earthquake data and modeling the geologic and tectonic characteristics of the region. Recently developed techniques, increased knowledge and improved databases brought the necessity to review the national active fault database and the compiled earthquake catalogue for the development of a national earthquake hazard map. A national earthquake strategy and action plan were conceived and accordingly with the collaboration of the several institutions and expert researchers, the Revision of Turkish Seismic Hazard Map Project (UDAP-Ç-13-06) was initiated, and finalized at the end of 2014. The scope of the project was confined to the revision of current national seismic hazard map, using the state of the art technologies and knowledge of the active fault, earthquake database, and ground motion prediction equations. The following two seismic source zonation models are developed for the probabilistic earthquake hazard analysis: (1) Area source model, (2) Fault and spatial smoothing seismic source model (FSBCK). In this study, we focus on the development and the characterization of the Fault Source model, the background spatially smoothed seismicity model and intrinsic uncertainty on the earthquake occurrence-rates-estimation. Finally, PSHA results obtained from the fault and spatial smoothed seismic source model are presented for 43, 72, 475 and 2475 years return periods (corresponding to 69, 50, 10, and 2% probability of exceedance in 50 years) for PGA and 5% damped spectral accelerations at 0.2 and 1.0 s. 相似文献
50.
Domenico Giardini Laurentiu Danciu Mustafa Erdik Karin Şeşetyan Mine B. Demircioğlu Tümsa Sinan Akkar Levent Gülen Mehdi Zare 《Bulletin of Earthquake Engineering》2018,16(8):3567-3570
The collaborative project Earthquake Model of the Middle East (EMME, 2010–2015) brought together scientists and engineers from the leading research institutions in the region and delivered state-of-the-art seismic hazard assessment covering Afghanistan, Armenia, Azerbaijan, Cyprus, Georgia, Iran, Iraq, Jordan, Lebanon, Palestine, Pakistan, Syria and Turkey. Their efforts have been materialized in the first homogenized seismic hazard model comprising earthquake catalogues, mapped active faults, strong motions databank, ground motion models and the estimated ground motion values for various intensity measure types and relevant return periods (e.g. 475–5000 years). The reference seismic hazard map of the Middle East, depicts the mean values of peak ground acceleration with a 10% chance of exceedance in 50 years, corresponding to a mean return period of 475 years. A full resolution poster is provided with this contribution. 相似文献