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ground fissures
相关语句
  地裂缝
     The feature and researching significance of the ground fissures formed by Zhangbei 6.2 earthquake
     张北6.2级地震地裂缝特征及其研究意义
短句来源
     Wholly 785 geologic hazards have been ascertained through investigation,in which there have 372 landslides,246 collapses,77 ground fissures,47 mudflows,11 karst collapses and 32 flooding washes.
     调查发现地质灾害共有785处,其中滑坡372处,崩塌246处,地裂缝77处,泥石流47处,岩溶塌陷11处,洪涝洼地32处。
短句来源
     Study on the Ground Fissures in Hebei Plain
     河北平原地裂缝研究
短句来源
     The application of the finite element method in the study of tectonic stress-field and the ground fissures in Hebei plain
     有限元在河北平原区构造应力场与地裂缝分布研究中的应用
短句来源
     The characteristics of anomalies of H2 in soils of the ground fissures in Xian are studied, and the mechanism of anomalies in H2 is discussed in this paper.
     本文研究了西安地裂缝的土壤H2异常特征,并讨论了H2异常机理。
短句来源
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  地裂
     Disasters of Xi'an Ground Fissures and Controlling Measures
     西安地裂灾害及其防治措施
短句来源
     PERIODICITY OF GROUND FISSURES AND EARTHQUAKES IN THE EARTHQUAKE BELT OF THE WEIHE RIVER
     渭河地震带地裂与地震活动的周期性
短句来源
     Then the middle yard can be used when the intervals of two paralle ground fissures and two leftlateral sense are bigger than 60 m and 80 m respectively.
     平行地裂段间距大于60m、左行雁列次级地裂段间距大于80m时,可考虑中间场地的使用;
短句来源
     The further study of ground fissures can be a useable way to prevent geological disaster.
     并提出了研究地裂的目的是为预防地质灾害服务,在预防方面尽量采取避让的措施。
短句来源
     Through actual data study, pointed out the ground fissure in the area belongs to gaping and cascading down type, also explained five inductive factors of ground fissures in the area through studying full and accurate data, there by provided ground fissure harnessing methods and orientation with abundant geologic data.
     通过对实际资料的分析,指出本区地裂缝类型为张跌型,并以较多的资料翔实地说明了诱发本区地裂地质灾害不可分割的五个因素,从而为治理地裂缝地质灾害提供了丰富的地质资料和治理方向。
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  “ground fissures”译为未确定词的双语例句
     Analysis of Features and Developmental Range of Ground Fissures Influenced by Faults
     断层影响下地表裂缝发育范围及特征分析
短句来源
     Collecting seism datum(Ms 3.0)which amounts to about 3000,and analyzing the relativity between ground fissures and earthquakes;
     收集≥3.0级以上地震资料3000多例,分析了地震与地裂缝间的相关性;
短句来源
     In this paper, the author discuss the relation between active tectonics and the origin, geomitric form and spatial distribution of ground fissures.
     本文重点论述了构造地裂隙的成因,形态特征,空间分布规律及其与活动构造的关系。
短句来源
     Formation Mechanism of the ground fissures formed by earthquake in Jiaochang platform of Minjiang River and its affect to slope stability
     岷江较场台地地震裂缝形成机制及其边坡稳定影响
短句来源
     In this paper the relationship between the fracture processes of strong earthquakes and the seismic activity was investigated toy studying the source mechanism, the distribution of afterslloks and the migration of strong earthquakes occurring on this belt and combining with the configuration of macroisoseismic lines and the distribution of ground fissures.
     本文通过研究发生在断裂带上强震的震源机制、震源过程、余震分布、地震迁移并结合宏观等震线、地震裂缝分布等资料,研究强震破裂过程与地震活动的关系。
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  ground fissures
Widespread liquefaction and associated sand boils, ground fissures and ground deformations due to lateral spreading occurred during this earthquake.
      
Although, there isno clear surface breaks associated with this earthquake, the localisation ofgeological disorders, such as ground fissures, during the Beni-Ourtilaneearthquake, which are remarkably located near the fault, may have atectonic meaning.
      
Liquefaction associated ground deformations such as lateral spreading, flow failures, ground fissures and subsidence, sand boils, and slope failures were observed.
      
This explains the correlation between ground fissures and active Quaternary normal faults.
      
Ground fissures and subsidence have caused extensive damage in structures and the utility networks (roads, railroad line, Larisa NATO airport, telecommunication network) in the plain of Thessaly, central Greece, in the last 20?years.
      
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The Haicheng earthquake (Feb. 4, 1975, M=7.3) has caused the extensive liquefaction of sand in the Lower Liaohe River region, which expressed itself as ejected water and sandflows, sundken lands and sandy holes on ground surface, ground drumlings, landslides and ground fissures.According to the degree of ejection and ground failure the liquefied region may be classified into three areas different in hazard, i. e. intensive( I ), moderate(Ⅱ) and weak (IE). The liquefied region in the Lower Liaohe...

The Haicheng earthquake (Feb. 4, 1975, M=7.3) has caused the extensive liquefaction of sand in the Lower Liaohe River region, which expressed itself as ejected water and sandflows, sundken lands and sandy holes on ground surface, ground drumlings, landslides and ground fissures.According to the degree of ejection and ground failure the liquefied region may be classified into three areas different in hazard, i. e. intensive( I ), moderate(Ⅱ) and weak (IE). The liquefied region in the Lower Liaohe River has been a regression area in Holocene period, covered by a layer of clayey soil with a thickness of 2-5m. This layer is thinner in the intensive hazard area with a higher aquifer head, but thicker in the weak hazard area with a lower head.The monograin structure of ejected sands shows the loosening nature of liquefied sandy layer. In the intensive hazard area the sand grains ejected are found to be coarser. According to the present analysis of sand grains it is concluded that the roundness of grains is of less importance in determining whether a sandy soil can be readily liquefied or not.

海城地震引起下辽河平原大面积砂土液化,液化震害有喷水冒砂、陷落砂坑、地滑移等等。液化区是全新世海退之地,震害严重区地表粘性土层薄,承压水头高;震害轻微区地表粘性土层厚,承压水头低。喷砂颗粒的单粒结构表明液化砂层具有松散的特点,砂颗粒的滚圆度在液化难易上不起主要作用。

Our neotectonic investgations in the Yongsheng region,western Yunnan,where the magnitude 8 earthquake of 1515 took place,have revealed intense activities of the N-S trending tectonic belt and the E-W trending one intersecting the former,Ahd the faults along the two belts were multicyclically activated at different ways of movement showing the changes of stress field in the neotectonic period.The Yongsheng earthquake occurred in the intersection of the a above-mentioned two tectonic belts and produced two ground...

Our neotectonic investgations in the Yongsheng region,western Yunnan,where the magnitude 8 earthquake of 1515 took place,have revealed intense activities of the N-S trending tectonic belt and the E-W trending one intersecting the former,Ahd the faults along the two belts were multicyclically activated at different ways of movement showing the changes of stress field in the neotectonic period.The Yongsheng earthquake occurred in the intersection of the a above-mentioned two tectonic belts and produced two ground fissure zones on the mountain ridge which extend in coincidence with the E-W tectonic belt. The single fissure has a maximum width of 8 m and more. The ground fissures were tensile and generated by the principal compressional stress of the same direction as the E-W seismic tectonic belt.The Chenghai thrust fault of the N-S trending tectonic belt,being monitored now,is less active and the tectonic stress has little influence on it. East and west qf the chenghai thrust,the other N-S trending faults,however,arc intensely active and need to be monitored

本文研究了永胜1515年8级大震震区的新构造活动,发现控制该区的南北向构造带与之交汇的东西向构造新活动十分强烈。断裂活动是多期的,各期的活动方式也不同,反映的应力场在輓近时期发生过多次变化,而永胜地震则发生在上述两组构造的交汇处。永胜地震在基岩上形成两条东西向裂缝带。它们以力学性质特殊(是主压应力方向与东西向发震构造平行情况下形成的典型张破裂型裂缝)和单条裂缝宽度最大(最宽处在8米以上)而在国内外罕见。作为本区控震构造的南北向金河——永胜——宾川断裂中常被文献提到并被监测的程海压扭性逆断层是一条新活动很弱、感受构造应力作用很轻的断层,而改为加强监测其东西两侧其它几条新活动强烈的断层为宜。

The second paper discusses anomalous non-seismic ground fissures,analyzes their cau- ses based on actual informations at hand.This is of great importance for stabilizing human minds so as to help promoting production and construction.The paper includes the follow- ing subheads such as,introduction,discrimination between seismic ground fissures and non- seismic ground fissures,the principal factors causing non-seismic ground fissures and some field observation examples,and concluding remarks....

The second paper discusses anomalous non-seismic ground fissures,analyzes their cau- ses based on actual informations at hand.This is of great importance for stabilizing human minds so as to help promoting production and construction.The paper includes the follow- ing subheads such as,introduction,discrimination between seismic ground fissures and non- seismic ground fissures,the principal factors causing non-seismic ground fissures and some field observation examples,and concluding remarks.

文章是关于非地震地裂缝异常问题,结合实际资料,分析非地震地裂缝成因,对安定人心以有利于生产建设具有积极意义,内容包括引言、地震地裂缝与非地震地裂缝的区分、非地震地裂缝异常的主要因素及其实例和结语。

 
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