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  “频繁的”译为未确定词的双语例句
    Thefrequent volcanic - intrusive activities implied the crust - mantle differentiation, multiple pouring of the mantle material and mutiple circulation of the crustal material, especially the tensionalstress environment reflected by 3 bimodal volcanic activities since Carboniferous(C1, J1, K1 ) created a multi - element and highly abundant geochemical field.
    频繁的火山一侵入活动揭示了壳幔分离、地幔物质多次注入、地壳物质多次循环,特别是石炭纪以来(C1、J1、K1)三次双峰式火山活动所反映的位张环境,造就了本区成矿元素多、丰度高的地球化学场和构造应力环境;
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    In this area, four north-dipping synsedimentary faults have occurred which strike northeast-east and descend in a series of steps from the south to the north.
    区内主要发育了四条北东东走向由南向北呈阶梯状节节下掉的北倾同沉积断层,控制了下第三系的沉积,并将整个斜块带切割成五个条带状断块,每个断块内具有东高西低的特征,受基底形态的控制,第三系地层由西向东由南向北逐步抬高,厚度逐渐变薄,特别是在下第三系伴随频繁的超覆现象;
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    As the most frequency post-earthquake disaster, the reason of the post-earthquake fire is sophisticate and its harm is huge.
    地震次生火灾作为地震次生灾害中发生最频繁的灾种,起火原因复杂其危害性也十分巨大。
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    This method has the merits of both compressed mass plane method and the polynornial method.
    本方法兼顾了压缩质面法和多项式法两者的长处,无论对平缓的界面还是起伏频繁的界面反演,都显示了一定的优越性。
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    The classification of karst landform is related closely to the development degree of karst and the concentration of karst water.
    由于受频繁的构造运动的影响,使岩溶发育具有多期性。 岩溶地貌类型的划分与岩溶发育程度,岩溶水的富集有密切联系。
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In South China, there are several small to medium sized basins which are characterized by the abundance of such features as multi-layering, lateral heterogeneity, thick sedimentary covers, variable rock facies, repeated erosions and varieties of faul-ting, etc .. These adverse geological conditions entail corresponding complications in. the application of seismic methods. Examples are disturbances from multiple reflec-tions and lateral waves, variable wave velocities, distortions from deep seated structures...

In South China, there are several small to medium sized basins which are characterized by the abundance of such features as multi-layering, lateral heterogeneity, thick sedimentary covers, variable rock facies, repeated erosions and varieties of faul-ting, etc .. These adverse geological conditions entail corresponding complications in. the application of seismic methods. Examples are disturbances from multiple reflec-tions and lateral waves, variable wave velocities, distortions from deep seated structures and others. All these give rise to difficulties in extracting informations concerning palaeozoic strata. The present paper discusses some of the views and methods to counter these difficulties.

在中国南方有一类中小型盆地,它们的特点是垂直方向的多层结构和水平方向的多级分割,形成复杂的构造格局。复杂性就在于沉积深厚,岩相多变;数度侵蚀,火成常见;断层不少,构造陡倾;起伏频繁,上下不符。因此产生了复杂的地震地质条件和探测的技术问题,诸如各类多次波,侧面波的干扰,复杂断层,各种不整合,尖灭带,速度多变,深层畸变等,造成取得古生代地层内部波组的困难。文中提出了解决这些问题的观点和措施。

The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system. In general, this...

The Hunhe fault zone is a western extension of the Shenyang-Dunhua Mishan fault and there can be found an evidence of Pre-Sinian movement. It is suggested that the faulting of Hunhe fault zone was significant in Mesozoic time and more intensive and frequent in Tertiary and Quaternary.Basing upon the data on geology, morphology and seismicity. this paper illustrates the trace of the neotectonic movement since Tertiary.Actually this fault acts as one of main faults of Cathaysian tectonic system. In general, this paper deals with only the Shenyan-Qingyuan section.

浑河断裂带在前震旦纪就开始活动,中生代时期活动剧烈,至第三纪和第四纪初、浑河断裂带的构造活动更为频繁强烈。本文主要讨论浑河断裂带自沈阳至清原县草市地段从第三纪以来的新构造活动的一些形迹。

Starting from the viewpoint of thermodynamics, the distribution characteristics of the hot springs and earthquakes in Yunnan province have been studied in this paper. Furthermore, a discussion is held on the crustal movement of this region and problems concerning seismic zoning.The area to the west of the Lanchang River belongs to the island arc geo-thermal anomalous region of the Burma-Andaman plate reduction zone. Gas wells, boiling springs and numerous ordinary hot springs are common occurrences in this region....

Starting from the viewpoint of thermodynamics, the distribution characteristics of the hot springs and earthquakes in Yunnan province have been studied in this paper. Furthermore, a discussion is held on the crustal movement of this region and problems concerning seismic zoning.The area to the west of the Lanchang River belongs to the island arc geo-thermal anomalous region of the Burma-Andaman plate reduction zone. Gas wells, boiling springs and numerous ordinary hot springs are common occurrences in this region. Therefore, it is one of the high intensity regions of Yunnan province because of its high level of scismicity. The two great shift fault zones surrounding the Red River and the Xiaujiang faults comprise two geothermal anomalous areas with frequent activities of earthquakes. They are also two of the high intensity regions. Those regions situated between the abovementioned 3 gcothermal anomalous regions are ones having relatively stable crust with fewer occurrences of earthquakes

本文从热力学的观点出发,探讨云南地区的温泉和地震分布特征,进而讨论了这里的地壳运动和地震区划问题。澜沧江以西的云南地区属于缅甸—安达曼板块消减带岛弧型地热异常区,这里分布着汽泉、沸泉和大量的普通温泉,地震活动频繁,是全省的高烈度区之一。环绕着红河断裂和小江断裂的两大平移断层带是两大地热异常区,而且地震活动频繁,是省内另外两大高烈度区。与上述三大地热异常区相间排列的地区为地壳相对稳定区,地震较少。

 
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