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   tectonic fissures 的翻译结果: 查询用时:0.008秒
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tectonic fissures
相关语句
  构造裂缝
     Reservoir spaces are mainly remaining of intergranular hole, induced porosity and cracks, or in more detail, remaining intergranular hole of the oolitic dolomite, intergranular enlarged solution hole, gypsum dissoved hole of gypseous dolomite, inter-crystalline hole of dolomite and tectonic fissures.
     储层的主要储集空间是残余粒间孔、次生孔隙和裂缝即:鲕粒白云岩的残余粒间孔、粒间扩溶孔、膏质白云岩中的膏溶孔、白云石晶间孔和构造裂缝;
短句来源
  构造裂隙
     New blasting practice and methods in non tectonic fissures
     非构造裂隙的新爆破方法与实践
短句来源
     Pb and Zn may be derived from the underlying strata,host rock and overlying strata,and sulfur from sulfate in the strata. Ore-forming dynamic was provided by Caledonian and Yenshanian movements. Tectonic fissures and pore in the carbonate rock played the part of ore fluid channel and host space.
     铅锌元素主要可能来自下伏地层、赋矿地层本身,硫可能来自地层硫酸盐,加里东、燕山运动可提供成矿动力,各种构造裂隙和高孔隙度的碳酸盐岩可成为导矿、配矿构造或容矿空间,化探显示有明显的铅锌异常带,本区的几个矿点与黔东—湘西成矿带内铅锌矿的各种特征很相似。
短句来源
     The natural mineral springs are obviously controlled by fault, fold and structural alteration zone and the water circulates along deep fracture zone and moves along interlayer faults or tectonic fissures, finally, wells out under an artesian condition.
     矿泉水受构造断裂、活动断裂构造蚀变带及褶皱控制明显,或沿深大断裂深部循环,或沿褶皱层间裂隙、构造裂隙向倾伏方向富集、运移、承压出露。
短句来源
     Evaluating Method of Effect of Tectonic Fissures on Roadway Stability
     构造裂隙对巷道稳定性影响的评价方法
短句来源
     Other controlling factors are geologic background, palaeokarst diagenesis, tectonic fissures, fault distribution,etc. In addition, palaeogeomorphology, effective thickness of reservoir and development of non-reservior are also effective.
     其他主要控制因素还有地质背景、古岩溶成岩作用、构造裂隙及断层分布等,古地貌、储层有效厚度以及非储层发育程度等对储层非均质性也具一定影响。
短句来源
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  “tectonic fissures”译为未确定词的双语例句
     Hydro-geochemistry and transportation of the fluid inclusion in karst seam hole and tectonic fissures are studied with applications of isotope techniques.
     应用同位素技术方法,研究溶蚀缝洞和构造断裂带的流体地球化学与运移行为。
短句来源
     The major accumulation spaces of dolomite in the study area are intercrystal pores, intercrystal solution openings and tectonic fissures. Fine-coarse crystallized dolomite has good accumulation petrophysical properties, and is a kind of good-well reservoir.
     本区白云岩主要储集空间为晶间孔、晶间溶孔和构造缝 ,细 -粗晶白云岩储集物性好 ,为好 -较好的储层。
短句来源
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  tectonic fissures
The influence of tectonic fissures on a stress state has been estimated.
      


It is considered that the mineralization process is a form of energy exchange of ore component inore fluid system, and is in accordane with the principle of geochemical potential conservation. Thishas been testified through the experimental study based on Duobaoshan porpbyry copper deposit, itsgeological characteristics and its ore-controlling conditions. these results well illustrate the principleof geochemical potential conservation. Duobaoshan porphyry copper deposit was formed under specificstructural environment...

It is considered that the mineralization process is a form of energy exchange of ore component inore fluid system, and is in accordane with the principle of geochemical potential conservation. Thishas been testified through the experimental study based on Duobaoshan porpbyry copper deposit, itsgeological characteristics and its ore-controlling conditions. these results well illustrate the principleof geochemical potential conservation. Duobaoshan porphyry copper deposit was formed under specificstructural environment of crossed tectonic fissures which create open spaces for the mineralization.Suppose the geochemical potential μU induced by potential energy of ore fluid remains unchanged,the geochemical potential μK induced by kinetic energy of ore fluid decreases and the geochemical potential μP induced by pressure energy of ore fluid increases. Such effects became the origin of the concentration of copper sulphides in Duobaoshan porphyry copper deposit.

矿床的矿化作用过程,实质上是一种能量转换过程。它表现为成矿体系中各组分的地球化学位的转换,同时遵守地球化学位守恒。据此,笔者根据多宝山斑岩铜矿床地质特征及控矿条件分析,对其铜矿化的能量守恒进行实验研究与分析。实验结果表明,在多宝山特定的构造地球化学环境下,当成矿流体进入相对开放的构造裂隔中时,使成矿流体因动能而引起的地球化学位μ_K降低,因压力能而引起的地球化学位μ_p增大,这是建立地球化学还原障,产生硫化物矿化作用过程的原因所在。

Xintan landslide, lying in the north bank of the middle reaches of the yangtze River, is a slide colony in the manner of ancillary,inheritance,falling and reactivity;and consists of the soil and the stone and presents the shear of middle sector and the traction of upper sector.Tt is compounded serially by a series of the slide masses that has a genetic connection each other.The energy of sliding is attenuated considerably because the stress are released mainly in the way of despersion.The sliding deformation...

Xintan landslide, lying in the north bank of the middle reaches of the yangtze River, is a slide colony in the manner of ancillary,inheritance,falling and reactivity;and consists of the soil and the stone and presents the shear of middle sector and the traction of upper sector.Tt is compounded serially by a series of the slide masses that has a genetic connection each other.The energy of sliding is attenuated considerably because the stress are released mainly in the way of despersion.The sliding deformation is caused basically because the group of tectonic fissures in the upper bedrock are developmental and the long-period rockfall materials lead t he upper sector of sliding mass to produce the loading and creeping action and the fore fringes of each sector to concentrate the stress and to cause the deformation, unstability and sliding,which pull the fore sector and draw the rear fringes to fall.In addition, this paper deals with the relationship between deformed slide mass and structure condition in the neighbour region.

位于长江中游北岸的新滩滑坡是一个中段剪出、上段牵引垮落式继承性古老复活型土石质复式滑坡体群。它由一系列具有成生联系的滑坡体(或崩滑体)串联组合而成。由于应力以分散释放为主,故滑动能量大大衰减。本文认为导致滑坡变形的主因是上部基岩中多组构造裂隙发育,长期岩崩物质使滑体上段产生加载、蠕滑作用,使各段前缓应力集中,产生变形失稳座滑,推动前段、牵动后缘垮落的结果。本文还探讨了滑坡体变形与周缘地质构造条件的关系问题。

There are many tectonic fissures in Q22-Q32 loess at Zhuya, Shandong Province. The tensional fissures are filled with Ca-veins, the rapidly cracked fissures with mixed sand, .gravel and clay, the slowly constantly cracked fissures with fine sand and clay, and the compressional slip fissures with nothing. The latter two fissures are later than the former two in active period. The directions of the fissures are coinsident with the directions of regional tectonic...

There are many tectonic fissures in Q22-Q32 loess at Zhuya, Shandong Province. The tensional fissures are filled with Ca-veins, the rapidly cracked fissures with mixed sand, .gravel and clay, the slowly constantly cracked fissures with fine sand and clay, and the compressional slip fissures with nothing. The latter two fissures are later than the former two in active period. The directions of the fissures are coinsident with the directions of regional tectonic lines, and their occurrences and mechanical characteristics are in agreement with regional contemporary tectonic stress field.The formation of these fissures in loess deposits is related to the position where the Zhuya scarp is located. Zhuya scarp lies in Wudi-Qingzhou active fault zone in the NW direction. Six moderate and strong earthquakes occurred at the intersection of NW- and NE-trending faults. Zhuya scarp is just located at the intersection of NE-trending Zihe and NW-trending Zibo-Zhuya active faults, where the stress can be easily accumulated. This area is more sensitive to tectonic movement.

山东朱崖一带Q_2~2—Q_3~2黄土中发育了许多构造裂缝。有封闭的张性裂缝、快速张裂的裂缝、缓慢持续张裂的裂缝及有摩擦面的压扭性裂缝,后两种裂缝形成时间晚。裂缝的的产状、力学特征与现代区域构造应力场有较好的相关性。 朱崖黄土裂缝的形成与其所处的构造部位有关。朱崖位于NW向的无棣—青州(益都)活动构造带内,历史上NW向断裂与NE向断裂的交叉点上发生了六次中、强地震,朱崖位于NE向淄河断裂与活动的NW向淄博—朱崖断裂交叉点上,是应力易于集中、构造活动明显的部位。

 
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