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海侵层序
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  transgressive sequence
     THE CHARACTERS OF TRANSGRESSIVE SEQUENCE OF TERRIGENOUS BASIN: CORRELATION BETWEEN THE TRIASSIC IN CENTRALEUROPEN BASIN AND THE CRETACEOUS IN SONGLIAO BASIN OF CHINA
     陆相盆地中的海侵层序特征:中欧盆地三叠系与松辽盆地白垩系对比研究
短句来源
     The maximum flooding surface lying in estuarine - shallow marine muddy unit demarcates the underlying transgressive sequence and overlying regressive sequence.
     位于河口湾—浅海相中的最大海侵面将冰后期海侵沉积旋回分为其下的海侵层序和其上的海退层序.
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  “海侵层序”译为未确定词的双语例句
     TERTIARY TRANSGRESSIVE SEQUENCES ANDSTRATIGRAPHIC CORRELATION INCHINA OFFSHORE AREA
     中国近海早第三纪海侵层序及地层对比
短句来源
     A systematic planktonic foraminiferal biostratigraphic succession and sequence of marine transgression and regession in well BY7-1-1 located somewhere at the mostsouthern end of Zhujiang River Mouth Basin are introduced in this paper.
     本文系统介绍了珠江口盆地最南的一个探井——BY7—1—1井浮游有孔虫生物地层和海侵层序。 通过对该井有孔虫全面系统采样分析,发现了渐新世浮游有孔虫组合。
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  相似匹配句对
     Transgressive-Regressive Sequences of the Upper Paleozoic at the Wudang Section in Guiyang
     贵阳乌当上古生界的海侵—海退层序
短句来源
     TERTIARY TRANSGRESSIVE SEQUENCES ANDSTRATIGRAPHIC CORRELATION INCHINA OFFSHORE AREA
     中国近海早第三纪海侵层序及地层对比
短句来源
     (3) sequence stratigraphy;
     层序地层学;
短句来源
     SEQUENCE BIOSTRATIGRAPHY
     层序生物地层学
短句来源
     THE TRANSGRESSION OF CARBONIFEROUS IN LIAONING
     辽宁石炭纪海侵
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  transgressive sequence
The detailed classification resulted in a more accurate portrayal of the marsh transgressive sequence than was obtainable with TM data alone.
      
Distribution of chloride in a transgressive sequence of fine-grained sediments
      
The West Pontides tectonic belt of northern Turkey comprises a Lower Ordovician-Lower Carboniferous transgressive sequence.
      
If so, the transgressive sequence coincides with the last appearance of Grammatodon in the early Temaikan of the Catlins district.
      
Other members of the persculptus Zone fauna persist above the sandstone marker bed into the next transgressive sequence.
      
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The Zhujiang River delta is located in subtropical zone of the South China, Its reception basin is a submerged-valley-typed estuary, with small tidal ranges and weak wave energy, scattered with many small islands. The input runoffs are large water-flowed and low silt-discharged rivers, mainly composed of the Xijiang, Dongjiang and Beijiang Rivers, among which the Xijiang River is the main source of water and silt for the delta (making up 73.5% of the total runoff and 87% of the total silt dischargs).

珠江三角洲是在晚更新世玉木亚间冰期和全新世大西洋期,由多条河流的泥、沙输入溺谷型河口湾内,形成具不同沉积特征的叠覆、镶嵌复合体,经历了由河口湾沉积向河控三角洲沉积的演变.其沉积相序分两类:一类是玉木亚间冰期和大西洋海侵阶段,形成以潮汐作用为主的溺谷型河口湾沉积相序,属海侵层序;另一类为大西洋期海平面相对稳定以来,以迳流作用为主的进积型河控三角洲沉积相序.

A systematic planktonic foraminiferal biostratigraphic succession and sequence of marine transgression and regession in well BY7-1-1 located somewhere at the mostsouthern end of Zhujiang River Mouth Basin are introduced in this paper. For comparison with European stratotype, five Late Cenozoic formations in Zhujiang River Mouth Basin were studied chronostratigraphically.

本文系统介绍了珠江口盆地最南的一个探井——BY7—1—1井浮游有孔虫生物地层和海侵层序。通过对该井有孔虫全面系统采样分析,发现了渐新世浮游有孔虫组合。这一重大发现给重新认识该区上、下第三系界线,以及对整个南海北部地层对比提供了新资料。并对有关的一些地质问题进行了讨论。

The barrier - lagoon systems (BLS) are widely distributed in the southwesten Inner Mongolia Autonomous Region during Carboniferous Period. The lagoon deposits of different singes in the systems are superimposed mutually,forming various sequences, with a great thickness. This is hard to be formed and preserved in the Holocene. According to sedimentological characteristics and depositional sequence, the transgressive, regressive, stationary and locally transgressive barrier lagoon systems in the carboniferous...

The barrier - lagoon systems (BLS) are widely distributed in the southwesten Inner Mongolia Autonomous Region during Carboniferous Period. The lagoon deposits of different singes in the systems are superimposed mutually,forming various sequences, with a great thickness. This is hard to be formed and preserved in the Holocene. According to sedimentological characteristics and depositional sequence, the transgressive, regressive, stationary and locally transgressive barrier lagoon systems in the carboniferous deposits of the studied area have been recognized, which are similar to the types in Holocene. It confirms that the stratigraphic models of barrier-lagoon systems summarized in the study of Holocene are helpful for recognition and study of the analogies in the geological time. However, the barrier-lagoon systems of the Carboniferous Period in the studied area have been formed in broad space for a long time, they are usually compound, such as transgressive - locally transgressive, stationary - locally transgressive BLS. In addition, the stationary BLS is characterized by both underlying and overlying strain to be terrestrial in Holocene , but the counterparts in the carboniferous deposits of the studied area are characterized by superimposition of more than ten barrier-lagoon sequences almost in the same area for a long time under conditions of continuous tectonic subsidence and stabilization of coastline.The transgressive barrier - lagoon systems occur in transgressive sequence and have lagoon deposits exceeding the coincident barrier sands in thickness. The formation model for BLS has been established.

石炭纪内蒙古西南部广泛发育砂坝─泻湖沉积体系,该体系不同时期形成的泻湖沉积物相互叠置、沉积厚度大、沉积层序多样,这在全新世泻湖中难以形成和观察到。依据沉积特征、沉积层序,识别出与现代同类沉积体系相似的四种基本类型:海侵型、海退型、稳定型和局部海侵型。这表明研究全新世砂坝─泻湖体系得出的地层模式有助于识别地质时期的同类沉积体系。由于研究地区石炭纪砂坝─泻湖体系发育于广阔的空间和较长的时间内,它们常成复合类型,如海侵型─局部海侵型、稳定型─局部海侵型。此外,全新世稳定型砂坝─泻湖体系的上覆和下优层皆为陆相,但是石炭系同类沉积体系在同一地区连续叠置,这是长时期构造持续下陷和岸线相对稳定的反映。海侵型砂坝─泻湖体系形成于海侵层序中,泻湖沉积物的厚度大于砂坝沉积物的厚度,据此,建立了不同于现代同类沉积体系的地层模式。

 
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