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earthquake相关的网络例句

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与 earthquake 相关的网络例句 [注:此内容来源于网络,仅供参考]

Fujian region exhibits a consistent southeastward movement: the average velocity before the earthquake was 32.1 mm/a; the velocity during the earthquake and in the two years after the earthquake t...

福建地区存在一致的南东向运动地震前(第1时段)运动速度平均为32.1mm/a;震时和震后两年时间内(第2时段)运动速度大幅度增加到38.7mm/a;震后第2个两年(第3时段)运动速度相对于第2时段大幅度减小为30.0mm/a;震后第3个两年(第4时段),运动速率相对第3时段有较大增加并超过了第1时段。

The main study areas of SEIZE include:(1)physical nature of asperity;(2)temporal relationships among stress, strain, and pore fluid pressure throughout the earthquake cycle;(3)controls on the updip and downdip limits of the seismogenic zone of subduction thrusts;(4)nature of tsunamigenic earthquake zones;(5)role of large thrust earthquake in mass flux.

SEIZE的主要研究内容包括:①凸凹体的物理性质;②在地震周期里,应力、应变和孔隙流体成分随时间的变化;③在俯冲逆冲断层上,发震带上界和下界的确定;④引起海啸的发震带的特征;⑤大型逆冲带地震在物质转换过程中所起的作用。

Let's cite some events for illustration: in 29 BC of the Han Dynasty:"On syzygy solar eclipse occurred in the daytime and then an earthquake struck at night"; in 120 of the Eastern Han Dynasty:"On syzygy solar eclipse occurred in the daytime; soon afterwards earthquake hit 8 regions"; in1068 of the Song Dynasty:"Earthquake struck again and at night lunar eclipse occurred"( the History of the Song Dynasty ) and etc.

比如汉朝公元前29年——朔,日有食之。

Based on the whole year datum of 251 examination items recorded by 102 digital stations of earthquake underground fluid in 2003, systemically summarizing the distribution of digital stations, quality of the datum , the joint between the digital datum and simulative datum , and so on in china, there is a comparison analysis on the actuality of digital observation of earthquake underground fluid and part of means between homeland and fremdness, preminarily discussing the questions of digital monitoring for earthquake underground fluid in china.

以2003年全国地震地下流体数字化的102个台站的251个测项的全年资料为基础,系统总结了全国数字化台站的分布、资料的质量、数字化资料和模拟资料的衔接情况等,并就目前我国地震地下流体数字化监测的现状和国内外的部分手段进行了对比分析,初步探讨了我国地震地下流体数字化监测中存在的问题。

Study of seismic standard shows that one 〓 magnitude earthquake may cause some extent surface rupture, but the characters of earthquake have proved this fact, if earthquake centre distribute along a fault, or congregate, we cannot rule out to occur a possibility of macroseism (M≥4) in the future.

地震学标志的研究认为,历史地震资料表明,在我国一个〓级地震即可产生某种程度的地表破裂,但是,如果震中沿着断层线分布或集中,那就不能排除今后发生大震(M≥4级)并产生地面破裂的可能性。

Compared with PSHA's result, it is similar to an actual earthquake, presenting directly the earthquake hazard and making the results of earthquake risk assessment more reliable.

也可以用设定地震进行震害预测,与单纯提供地震危险性概率分析结果相比,设定地震类似于将要发生的地震,从而使震害预测的结果建立在一个比较现实的物理背景上。

The rupture process of 2009 August 10 Andaman earthquake was obtained by inverting the broadband seismic data of Global Seismographic Network based oil the fast inversion method of earthquake rupture process about 4 hours after the earthquake occurrence.

运用地震破裂过程快速反演方法,在2009年8月10日安达曼地震发生后,采用全球地震台网的宽频带地震资料,快速反演了这次地震的破裂过程,在地震发生约4小时后得出了这次地震的破裂过程反演结果。

The rupture process of 2009 October 7 Vanuatu earthquake was obtained by inverting the broadband seismic data of Global Seismographic Network based on the fast inversion method of earthquake rupture process within 3 hours after the earthquake occurrence.

运用地震破裂过程快速反演方法,在2009年10月7日瓦努阿图地震发生后,采用全球地震台网的宽频带地震资料,快速反演了这次地震的破裂过程,在震后3小时内得出了这次地震破裂过程的反演结果。

The rupture process of 2009 July 15 off west coast of South Island of New Zealand earthquake was obtained by inverting the broadband seismic data of Global Seismographic Network based on the fast inversion method of earthquake rupture process within 4 hours after the earthquake occurrence.

运用地震破裂过程快速反演方法,在2009年7月15日新西兰南岛西海岸近海地震发生后,采用全球地震台网的宽频带地震资料,快速反演了这次地震的破裂过程,并于震后4小时内得出了这次地震破裂过程的反演结果。

The rupture process of 2009 September 29 Samoa Islands region earthquake was obtained by inverting the broadband seismic data of Global Seismographic Network based on the fast inversion method of earthquake rupture process within 3.5 hours after the earthquake occurrence.

运用地震破裂过程快速反演方法,在2009年9月29日萨摩亚群岛地区地震发生后,采用全球地震台网的宽频带地震资料,快速反演了这次地震的破裂过程,并于震后3.5小时内得出了这次地震破裂过程的反演结果。

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