片语

hypergene environment表生环境

hypergene condition表生条件

hypergene process[地质]

hypergene minerals表生矿物

hypergene zoning表生分带性

Hypergene water表生水

hypergene leaching表生淋滤

hypergene structure表生构造

hypergene geochemistry表生地球化学

英汉例句

• in shallow hypergene zone, the shift of elements is of long-term and complicated feature and is influenced by a lot of factors, which plays an important role in destabilization of slope.

  在浅表生带中，元素迁移是斜坡失稳孕育过程中显着的伴生作用，直观、细致地反映出斜坡失稳演化过程的长期、复杂、受多种因素控制的特征。

• karst cave minerals are products of hypergene chemical deposition under the action of groundwater.

  洞穴矿物是在洞穴环境下由冷的地下水活动所产生的表生化学沉积作用产物。

• it is very important to carry out the kinetic study of the oxidation and reactive transference of tl in hypergene condition.

  因此对表生条件下，含铊矿物的氧化溶解动力学以及反应性迁移的实验研究具有重要的现实意义。

• in addition, dissolution of grain dolostone also occurs and shows the characteristics of hypergene dissolution in some places, which may contribute to the development of reservoir space.

  另外，局部可见颗粒白云巖发生溶蚀，有些地方具有表生溶蚀作用的特点，对白云巖储集空间的发育有一定贡献。

• the quartz veins in the studied region are hypergene and crystallized in the condition rich in water.

  研究区石英脉均为超浅成富水条件下结晶形成的。

• furtherly, lithology is considered to be the material base of hypergene karst which is on the ground of palaeostructure and mainly controlled by the palaeogeomorphology.

  认为巖性是表生巖溶形成的物质基础，古构造为表生巖溶发育提供了背景，而古地貌是控制表生巖溶发育的关键。

• based on the analysis of core and thin slice, it is concluded that the forming of ma 51 dolomite reservoir is dominated by hypergene karstification, burial dissolution and mineral filling.

  巖心与薄片分析表明，该研究区的表生巖溶作用、埋藏溶解作用和矿物充填作用对马五1亚段白云巖储集层形成的影响较大。

• rare earth elements (rees) play an important role on understanding and studying hypergene processes.

  ree是了解和研究地球表生过程的一个重要手段。