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内潮汐
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  internal-tide
     INTERNAL-TIDE DEPOSITS OF THE MIDDLE AND UPPER ORDOVICIAN IN WELL TZ 32, TARIM BASIN
     塔里木盆地塔中32井中上奥陶统内潮汐沉积
短句来源
     Ordovician Internal-tide Deposits in TZ30 Well, Tarim Basin
     塔里木盆地TZ30井中上奥陶统内潮汐沉积
短句来源
     By comprehensive study of cores and various data, internal-tide deposits are recognized in the middle-upper Ordovician of TZ30 well in the Tarim basin, which is the second example found in China after finding in the Tonglu area, Zhejiangprovince.
     通过岩心观察和其他资料的综合研究,在塔里木盆地TZ30井中上奥陶统中鉴别出了内潮汐沉积。
短句来源
     The Ordovician internal-tide and internal-wave deposits in West Zhejiang and Tarim Basin are typical cases in this field.
     我国浙西和塔里木盆地奥陶系的内潮汐、内波沉积已成为该领域的典型研究实例。
短句来源
     A Review on Research of Internal-wave and Internal-tide Deposition in Waters
     水体内部的沉积作用——内波、内潮汐沉积研究综述
短句来源
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  internal tide
     Current Situation and Advance of Internal Wave and Internal Tide Deposit Study
     内波、内潮汐沉积研究现状与进展
短句来源
     From 1990s, as a newly generated field of tract-current in deep water, internal wave and internal tide theory is rising up. Now, lots of internal wave and internal tide deposits have been found or demonstrated in modern water system and paleo-sediments. The sediment characters and deposit models have been investigated and studied widely.
     自20世纪90年代,内波、内潮汐沉积作为深水牵引流沉积研究中一个新的研究方向开始兴起,此后在国内外现代水体和古代地质记录中陆续发现或论证了大量的内波、内潮汐沉积,并对其沉积特征、沉积模式等进行了广泛的探讨和研究,然而对于内波、内潮汐沉积作用方式的研究还比较匮乏,这是内波、内潮汐理论发展的一大障碍。
短句来源
     FORMS OF INTERNAL WAVE AND INTERNAL TIDE SEDIMENTATION
     内波与内潮汐沉积作用的方式
短句来源
     RESEARCH STATUS AND PERSPECTIVE OF INTERNAL TIDE AND INTERNAL WAVE DEPOSITS
     内潮汐和内波沉积研究现状与展望
短句来源
     7.contorted bed facies:slumping deposit; 8.bidirectional cross-laminated sandstonefacies:internal-tide deposit; 9.unidirectional cross-bedded and cross-laminated sandstonefacies:deposit of internal tide with superposing internal wave.
     与其伴生的相有:(6)暗色泥质岩相:悬浮沉积,(7)扭曲层相:滑塌沉积,(8)双向交错纹理砂岩相:内潮汐沉积,(9)单向交错层-交错纹理砂岩相:叠加有内波作用的内潮汐沉积。
短句来源
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  “内潮汐”译为未确定词的双语例句
     The net transport trending of the sediments in the tidal channel within the channel mouth is towards the lagoon.
     口门内潮汐通道深槽泥沙净搬运趋势指向湖。
短句来源
     Patterns of the ratio variation with time of the earthquake sequence at Lijiang area before the M 7.0 shock are obtained. The result indicates that the value of the ratio was higher than 1 during the time of more than two years before the M 7.0 shock,and began to go up severely at the time six months before the big shock,and reached the maximum just before the shock.
     结果表明 ,在 7.0级丽江大震前的 2a多时间内 ,潮汐体应力压张地震比一直高于 1,距大震前半年开始剧烈升高 ,临震时达到最大 .
短句来源
     Deep-water carbonate sediments include allochthonous carbonate sediments released from shallow water by gravity flow and carbonate contourite and static autochthonous deep sea carbonate sediments.
     深水碳酸盐沉积包括深水重力流作用形成的异地沉积和非重力流沉积 ,在非重力流沉积中又有深水牵引流 (等深流、内波、内潮汐等 )沉积和静态原地碳酸盐沉积。
短句来源
     Four basic sedimentary microfacies and five vertical successions of internal-wave/in- ternal-tide deposits have been recognized and summarized.
     通过对塔中地区中—上奥陶统碎屑岩段岩心观察和地震剖面的系统分析,发现了该岩段内由内波和内潮汐作用形成的各种牵引流沉积构造单元。
短句来源
     The geologic entity formed by large-scale sediment-waves is most valuable in mineral resources.
     内波、内潮汐沉积方面,最有矿产意义的当属由大型沉积物波构建的地质体。
短句来源
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  internal-tide
All these features ensure a more rapid sink for the internal-tide energy.
      
Characteristics of internal-wave and internal-tide deposits and their hydrocarbon potential
      
The study of internal-wave and internal-tide deposits is a new research field on sedimentology during the last ten years.
      
The relationship between internal-wave and internal-tide deposits and petroleum is discussed, and finally internal-wave and internal-tide deposits are shown to be a new potential field for petroleum exploration.
      
Thus, reduced internal-tide amplitude is associated with increased soliton amplitude.
      
  internal tide
It is hypothesized that internal tide-induced variations of the sound velocity field on the shelf affect the degree of energy interaction between the first mode and the bottom.
      
Simulation of the internal tide in the Strait of Bab el Mandeb (the Red Sea)
      
Results related to simulations of the barotropic tide in the Red Sea and to the internal tide in the Strait of Bab el Mandeb are presented.
      
The geographic properties of low-frequency internal waves in the region are discussed primarily on the basis of the mechanism of internal tide generation on the continental shelfbreak, and the mechanisms of local generation and global generation.
      
Progress of studies on the internal tide generated by the passage of barotropic tide over continental shelf/slope
      
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Current- meter data collected over the past 20 years has revealed the existence of currents flowing alternatively up and down most submarine canyons and other submarine valleys. These currents are attributed to internal weaves that are subsurface waves between layers of different density or within layers where vertical density gradients are present. An important kind of internal wave is that which has a period equal to the semidiurnal or diurnal tide and referred to as an internal tied. Velocities of bidirectional...

Current- meter data collected over the past 20 years has revealed the existence of currents flowing alternatively up and down most submarine canyons and other submarine valleys. These currents are attributed to internal weaves that are subsurface waves between layers of different density or within layers where vertical density gradients are present. An important kind of internal wave is that which has a period equal to the semidiurnal or diurnal tide and referred to as an internal tied. Velocities of bidirectional deep-water currents range from 20-50 cm / sec. Such currents can move sediment up to fine sand and form a lot of ripples at depths of several thousand meters. Nevertheless, internal-tied deposits have not been recognized in the ancient rock record.

本文论述了在世界范围内首次鉴别出的新的沉积类型——内潮汐沉积,发现于美国弗吉尼亚州芬卡苏地区奥陶纪深水海底水道充填沉积中。已识别出两种相:①双向交错纹理极细砂岩相,以发育分别向古水道上方和下方倾斜的双向交错纹理为特征,被归因于内潮汐作用沉积的产物。②单向交错层和交错纹理中至细砂岩相,发育向古水道上方倾斜的低角度板状交错层和交错纹理,被解释为叠加有内波的内潮汐沉积物。据沉积相层序分析,内潮汐沉积形成于海平面上升、粗屑重力流受到抑制的时期。

Acorrding to the strain flower theory,the method and formulas which determined plane strain state and extracted tidal plane strain, volumetric strain and shear strain by combinatory observation of three tidal strain components are given. Especially, based on the tidal strain theory and the actural observation of tidal line strain, a tidal shear strain on the earth' s surface is simulated by using the character of subtractive combination of tidal line strain. We have raised a new method and formulas which determined...

Acorrding to the strain flower theory,the method and formulas which determined plane strain state and extracted tidal plane strain, volumetric strain and shear strain by combinatory observation of three tidal strain components are given. Especially, based on the tidal strain theory and the actural observation of tidal line strain, a tidal shear strain on the earth' s surface is simulated by using the character of subtractive combination of tidal line strain. We have raised a new method and formulas which determined plane strain state and extracted tidal plane strain, volumetric strain and shear strain by combinatory observation of two tidal strain components. An universal formula for discribing the combinatory information is put forward by the principle of wave superposition,and also we have driven the relevant geodetic coefficients and additional phase of combinatory information. Finally we briefly discuss the precursory physical mechanism of combinatory information and obtain that the subtractive combination of tidal line strain and the tidal shear strain on the earth' s surface are complete equivalent with the precursory response of an earthquake.

根据应变花理论,给出了由任意三方向潮汐线应变组合观测确定平面应变状态及提取潮汐面应变、体应变、平面剪切应变信息的方法和公式;特别是,根据潮汐应变理论和实际潮汐线应变的观测事实,利用两潮汐线应变差组合的特征,对地表潮汐剪切应变进行模拟,提出了由地表任意两独立方向潮汐线应变的组合观测确定地表潮汐平面应变状态及提取潮汐面应变、体应变信息的方法和公式,根据波叠加原理,提出了描述组合信息的统一公式,并导出了与之对应的各组合信息的大地系数和附加相位表达式;最后,简要讨论了各组合信息的前兆性物理实质,并得出潮汐线应变差组合观测对地震前兆信息的响应特征完全等价于地表平面内的潮汐剪切应变观测对地震前兆信息的响应特征。

Fincastle Conglomerate which was considered as deposits in shallow water in the pastis mainly gravity flow deposits and associated sediments ia deep water submarine chan-nels.Five gravity flow facies have been recognized:1.pebbly mudstone facies;2.matrix-rich conglomerate facies;3.matrix-poor conglomerate facies;4.massive sandstone facies;5.graded sandstone facies.Among them 1 and 2 are debris flow deposits;3 and 4 belongto grain flow deposits;and 5 is turbidite including high density and low density currentdeposits.The...

Fincastle Conglomerate which was considered as deposits in shallow water in the pastis mainly gravity flow deposits and associated sediments ia deep water submarine chan-nels.Five gravity flow facies have been recognized:1.pebbly mudstone facies;2.matrix-rich conglomerate facies;3.matrix-poor conglomerate facies;4.massive sandstone facies;5.graded sandstone facies.Among them 1 and 2 are debris flow deposits;3 and 4 belongto grain flow deposits;and 5 is turbidite including high density and low density currentdeposits.The associated facies comprise:6.dark shale and mudrock facies:suspension de-posit;7.contorted bed facies:slumping deposit;8.bidirectional cross-laminated sandstonefacies:internal-tide deposit;9.unidirectional cross-bedded and cross-laminated sandstonefacies:deposit of internal tide with superposing internal wave.The nine facies mentionedabove constitute five facies assemblages that show regular patterns.To sum up,the Fin-castle Conglomerate shows a clear upward-fining sequence,reflecting a process of that thesea level continued to rise and the source area was farther and farther to the sedimentarysite.

过去视为浅水沉积的“芬卡苏砾岩”,实为深水海底水道中的重力流及其伴生沉积。识别出5种重力流沉积相:(1)含砾泥岩相,(2)富基质砾岩相,(3)贫基质砾岩相,(4)块状砂岩相,(5)递交砂岩相。其中(1)和(2)为碎屑流沉积,(3)和(4)属颗粒流沉积,(5)为浊积岩,包括高密度和低密度浊流沉积。与其伴生的相有:(6)暗色泥质岩相:悬浮沉积,(7)扭曲层相:滑塌沉积,(8)双向交错纹理砂岩相:内潮汐沉积,(9)单向交错层-交错纹理砂岩相:叠加有内波作用的内潮汐沉积。上述九种相构成了5个有规律的组合,反映海平面持续上升,物源区不断远离沉积区的过程。

 
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