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施洞口
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  shidongkou
     Placer Abnormal of Volcanic lithoclast at Longjingjie in Kaili of Guizhou locates in regional Shidongkou deep and major fault nearby, abnormal materials that are obsidian lithoclast and volcanic glass.
     贵州凯里龙井街火山岩屑重砂异常位于区域性施洞口深大断裂近旁 ,异常物质为黑曜岩屑及火山玻璃。
短句来源
     Its existing shows that neighborhood of Shidongkou fault zone once arises acid volcanic eruption in neoid period and provides new important information with basic geological study of Guizhou. [
     它的存在 ,显示了施洞口断裂带附近 ,挽近地质时期曾有酸性火山喷发活动 ,为贵州基础地质研究提供了新的重要信息
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  “施洞口”译为未确定词的双语例句
     The Reversed Thrust Nappes in Shidongkou, Guizhou and Their Basic Features
     施洞口地区的逆冲推覆体及其基本特征
短句来源
     Based on the new data collected in the 1 : 5000 regional geological survey, this paper introduces four different types of reversed thrust nappes like outside flying peaks, structure windows, thrusts and double thrust structures which have been marked in Shidongk-ou in recent years.
     本文以1:5万区域地质调查新资料为基础,重点介绍了施洞口地区近年来首次圈定的具有飞来峰、构造窗、冲断体和双冲构造4种不同样式的逆冲推覆体。
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  相似匹配句对
     3 Effects of different nitrogen applied level on nitrogen
     氮?
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     The Reversed Thrust Nappes in Shidongkou, Guizhou and Their Basic Features
     洞口地区的逆冲推覆体及其基本特征
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     维舒胶囊
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     Overview to landscape design on tunnel opening
     隧道洞口景观设计
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     The Green Method Study of Portal Part of Tunnel
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Based on the new data collected in the 1 : 5000 regional geological survey, this paper introduces four different types of reversed thrust nappes like outside flying peaks, structure windows, thrusts and double thrust structures which have been marked in Shidongk-ou in recent years. The paper makes detailed analysis and approaches to their formation effect or formation mechanism, tentatively thinking that they were all formed in Yanshan period. Besides, the paper also makes a detailed introduction and preliminary...

Based on the new data collected in the 1 : 5000 regional geological survey, this paper introduces four different types of reversed thrust nappes like outside flying peaks, structure windows, thrusts and double thrust structures which have been marked in Shidongk-ou in recent years. The paper makes detailed analysis and approaches to their formation effect or formation mechanism, tentatively thinking that they were all formed in Yanshan period. Besides, the paper also makes a detailed introduction and preliminary estimation of Shidongkou rifts which have special structural positions, their main occurrances, occur-rance change features, and the SE -NW reversed nappe actions and displacement amount.

本文以1:5万区域地质调查新资料为基础,重点介绍了施洞口地区近年来首次圈定的具有飞来峰、构造窗、冲断体和双冲构造4种不同样式的逆冲推覆体。对它们的形成作用或形成机制进行了较详细的分析和探讨。初步认为,它们均形成于燕山期。此外,本文对具有特殊构造位置的施洞口断裂,其主要的产出状态、产状变化特征及由南东向北西的1—4次逆冲推覆作用及位移量亦进行了较详细的介绍和初步的估算。

The Jiumenchong limestones formation,Lower Cambrian,eastern Guizhou is Characterized by its crystalline-granular texture,showing that lime mud sediment has been recrystallized.Because sedimentation,diagenesis and str- ucture action of the limestone are different in different area and layer,it is different in their path and stage of the limestone reerystallization evolu- tion. Usually,it is obvious that there are two main evolutional paths and 2-3 evolutional period.The evolutional path is mainly decided by sedimentary...

The Jiumenchong limestones formation,Lower Cambrian,eastern Guizhou is Characterized by its crystalline-granular texture,showing that lime mud sediment has been recrystallized.Because sedimentation,diagenesis and str- ucture action of the limestone are different in different area and layer,it is different in their path and stage of the limestone reerystallization evolu- tion. Usually,it is obvious that there are two main evolutional paths and 2-3 evolutional period.The evolutional path is mainly decided by sedimentary features.The sedimentary features have a predominant influence in the first evolutional period.Compaction,pressolution and maturation of organic com- ponents have major influences in second evolutional period,and they are decisive factors in the secondary evolution.Structural stress has a decisive function in the third cvolutional period.Correspondingly,two main evolu- tional paths,two-three evolutional periods and three possible reservoir rocks types are abserved,with the fissure types as the most possible case,and the prosity-fissure type is the best reservoir rocks.For example,Zhenyuan, Shidongkou,Nangao,near to the eastern large fault nearly all reservoir rocks are of the fissure type.There is fissure type reservoir formation in the lower part in western part too.There is fissure type or nonreservoir rock near the area with lower curvature or unfaulted area in the middle part.

黔东下寒武统九门冲组灰岩是由灰泥沉积物经重结晶作用而成的晶粒结构灰岩。由于不同地区、层段的沉积、成岩和构造作用的差异,导致了灰岩重结晶演化途径、阶段上的不同。一般可见两大演化途径和2~3个演化阶段。沉积特征主要决定了演化途径,并对第一演化阶段发生显著的影响;压实、压溶作用和有机质演化对第二阶段影响最甚,并决定着次一级演化分枝;构造应力对第三阶段演化起决定性作用。与上述演化相对应的储集性也县有两大演化途径和2~3个演化阶段及三种可能储集类型,最大可能是缝隙型,最佳储集类型是孔隙-缝隙型。东部大断裂带附近,如镇远、施洞口、南皋一带多为缝隙型,西部下段亦为缝隙型,而中段在曲率低值区或无断裂一带是孔隙型或致密的非储集岩。

Shidongkon thrust in southern Guizhou is an important fault zone. As a result of its thrusting, two terrains of different tectonic units and levels were conjoined. During its thrusting, the structure deformations with different styles anddegrees formed. For the lower plate of the main-slide plane. the brittle deformation domimated. the vertical zonation of its rock resulting in defference in deformations of the structure sub-levels. However, the upper plate of the main-slide plane is characterized by the ductile...

Shidongkon thrust in southern Guizhou is an important fault zone. As a result of its thrusting, two terrains of different tectonic units and levels were conjoined. During its thrusting, the structure deformations with different styles anddegrees formed. For the lower plate of the main-slide plane. the brittle deformation domimated. the vertical zonation of its rock resulting in defference in deformations of the structure sub-levels. However, the upper plate of the main-slide plane is characterized by the ductile deformation, but in various parts of the thrust, the stress distribution and structure deformation being defferent.

施洞口断裂是贵州东南部一条重要的断裂带,在它的逆冲推覆作用过程中,逆冲推覆构造的不同地段,其应力分布、构造变形特点都有一定差异。而逆冲推覆构造所产生的巨大水平挤压力在地台盖层中亦可产生构造变形。由于盖层结构中物质具垂直分带,各构造亚层变形特征也各具特点。

 
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