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湛江组
相关语句
  zhanjiang formation
    Sedimentary facies of the Zhanjiang Formation .
    湛江组沉积相特征
短句来源
    the initial occurrence of the South China tektite in strata is in the middle horizon within Beihai Formation, which is the erosion surface on the top of the lower part of Beihai Formation, but not on the top of Zhanjiang Formation.
    玻璃陨石从产状来看可分为埋藏的原生撒落型、暴露的原生撒落型和次生搬运型等几类 ,赋存的原生层位是北海组中 -下部的组内剥蚀面 ,而不是北海组与湛江组的界面 ;
短句来源
    Based on the age dating,geochemical and geophysical analyses,as well as field investigation along the coast of South China Sea,the authors expatiated the characteristics of sedimentary facies,chemical components and susceptibility of the Zhanjiang Formation(Early Pleistocene) and the Beihai Formation(Middle Pleistocene),and showed the pictures of deformation,folds,faults,and volcanism in the area.
    文章根据一系列野外调查和年代测定以及地球化学与地球物理测试分析,阐述了南海北部早更新世湛江组和中更新世北海组的沉积相、化学组分、磁化率等特征,并描述了该区构造变形、褶皱、断裂和火山活动特点。
短句来源
  zhanjiang formation
    Sedimentary facies of the Zhanjiang Formation .
    湛江组沉积相特征
短句来源
    the initial occurrence of the South China tektite in strata is in the middle horizon within Beihai Formation, which is the erosion surface on the top of the lower part of Beihai Formation, but not on the top of Zhanjiang Formation.
    玻璃陨石从产状来看可分为埋藏的原生撒落型、暴露的原生撒落型和次生搬运型等几类 ,赋存的原生层位是北海组中 -下部的组内剥蚀面 ,而不是北海组与湛江组的界面 ;
短句来源
    Based on the age dating,geochemical and geophysical analyses,as well as field investigation along the coast of South China Sea,the authors expatiated the characteristics of sedimentary facies,chemical components and susceptibility of the Zhanjiang Formation(Early Pleistocene) and the Beihai Formation(Middle Pleistocene),and showed the pictures of deformation,folds,faults,and volcanism in the area.
    文章根据一系列野外调查和年代测定以及地球化学与地球物理测试分析,阐述了南海北部早更新世湛江组和中更新世北海组的沉积相、化学组分、磁化率等特征,并描述了该区构造变形、褶皱、断裂和火山活动特点。
短句来源
  “湛江组”译为未确定词的双语例句
    The Engineering Geology of Gray Clay of Zhangjiang Group of Quaternary System in Haikou District
    海口地区第四系湛江组灰色粘土的工程地质特性
短句来源
    A layer of gray clay of Pleistocene series of Quatemary system commonly exists in Haikou District and it has been belonged to Zhanjiang Group.
    海口地区普遍存在一层第四系下更新统灰色粘土地层 ,地质界一般将其归为湛江组
短句来源
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On the basis of the predecessors' information, this paper has preliminarily summarized the geological background, geological characteristics, genesis, present utilization situation and exploitaion prospect of the clay deposit in Beihai city. This paper has presented that the clay deposit occurs in the Quaternary Zhanjiang Formation, the thickness of ore-bearing strata is great and stable, the ore bodies appear in thick-stratified forms, locally lens, the types of clay minerals can be divided into two: the hydromica-kaolin...

On the basis of the predecessors' information, this paper has preliminarily summarized the geological background, geological characteristics, genesis, present utilization situation and exploitaion prospect of the clay deposit in Beihai city. This paper has presented that the clay deposit occurs in the Quaternary Zhanjiang Formation, the thickness of ore-bearing strata is great and stable, the ore bodies appear in thick-stratified forms, locally lens, the types of clay minerals can be divided into two: the hydromica-kaolin clay and the illite-kaolin clay, the ores are good in quality. This paper has also believed that the deposit is locustrine-fluvial facies sedimentary deposit. The clay ore can be acted as the raw material in ceramic industry, paper-making industry and ceramsite, besides brick and tile.

本文根据前人资料基础上,初步总结了北海市粘土矿的地质背景、矿床地质特征、矿床成因和利用现状及开发前景。文中指出粘土矿产于第四系湛江组中,含矿层厚度大、较稳定;矿体呈厚层状,局部为透镜;矿石类型可划分为水云母—高岭石粘土和伊利石—高岭石粘土两类,质量较好,认为属湖泊—河流相沉积型矿床。据应用开发研究成果,除生产砖瓦外,还可作为陶瓷工业,造纸工业和陶粒原料。

The dolomite of Paipu, Hainan Island, is a recent dolomite firstly discovered in China.It developed in the fine sand-silt beds of coastal factes of Zhangjiang Formation,early Pleistocene.Through alteration,the rhombohedral crystalline dolomite was formed with a fogged center and clear margin structure, and belongs to a Fe-containing,Ca-excess dolomite.The formational process of the dolomite can be subdivided into two steps:(1) meta-homogenerous dolomitization caused by permeation and return flow;(2) early diagenessis...

The dolomite of Paipu, Hainan Island, is a recent dolomite firstly discovered in China.It developed in the fine sand-silt beds of coastal factes of Zhangjiang Formation,early Pleistocene.Through alteration,the rhombohedral crystalline dolomite was formed with a fogged center and clear margin structure, and belongs to a Fe-containing,Ca-excess dolomite.The formational process of the dolomite can be subdivided into two steps:(1) meta-homogenerous dolomitization caused by permeation and return flow;(2) early diagenessis dolomitization caused by mixing water which might go on to present time.

对我国首次发现的海南排浦现代白云岩的研究认为,该岩发育于早更新世湛江组滨海相细—粉砂层之中,通过交代作用形成具雾心亮边结构的菱面体自形晶,矿物上属钙过剩的含铁白云岩,其形成过程可分为二个阶段:准同生渗透回流白云岩化作用阶段;成岩混合水白云岩化作用阶段,而后一阶段可能延续至今。

A layer of gray clay of Pleistocene series of Quatemary system commonly exists in Haikou District and it has been belonged to Zhanjiang Group. This layer of clay posses a certain thickness and strength, commonly being as the main bearing layer of general industrial and civil architecture. The preliminary analysis on the engineering geology was made in the paper from the angle of geotechnic test and field test.

海口地区普遍存在一层第四系下更新统灰色粘土地层 ,地质界一般将其归为湛江组。此层粘土具有一定厚度和强度 ,常作为一般工业与民用建筑的主要持力层 ,从土工试验和现场试验角度 ,对其工程地质特性作初步分析

 
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