额济纳旗的英文

发音:

"额济纳旗"怎么读用"额济纳旗"造句

英文翻译手机版

ejin qi

"额"英文翻译 forehead
"济"英文翻译 cross a river
"纳"英文翻译 receive; admit
"旗"英文翻译 flag; banner; standard
"额济纳河" 英文翻译 : ejin river
"额济纳的胡杨" 英文翻译 : eos 300d
"济纳" 英文翻译 : zina
"贝专纳旗" 英文翻译 : bechuanaland flag
"布济纳" 英文翻译 : bouzina
"济纳特" 英文翻译 : zinat
"卡济纳" 英文翻译 : kazyna
"科济纳" 英文翻译 : kozina
"雷济纳" 英文翻译 : rydzyna
"列济纳" 英文翻译 : rezina
"穆济纳" 英文翻译 : muzina
"纳济纳" 英文翻译 : nazina
"锡济纳" 英文翻译 : sidzina
"阿济纳诺" 英文翻译 : arzignano
"波罗济纳" 英文翻译 : porozina
"卜赖济纳" 英文翻译 : brezina
"济纳伊姆" 英文翻译 : dhi na'im
"克拉济纳芬" 英文翻译 : klazienaveen
"曼济纳斯" 英文翻译 : manzinus
"托马济纳" 英文翻译 : thomazina; tomasina; tomazina
"古尔德济纳泉" 英文翻译 : hassi rhourde ez zina; rhourde ez zina hassi

例句与用法

Measuring the total economic value of restoring ejina banner ' s ecosystem services
额济纳旗生态系统恢复的总经济价值评估
Comparison and application of different contingent valuation methods in measuring total economic value of restoring ejina banner ' s ecosystem services
额济纳旗生态系统服务恢复价值评估方法的比较与应用
However , the reservoir porosity and permeability of lower cretaceous in erlian basin is better than that of yingen - ejinaqi basin
但二连盆地下白垩统储层的孔隙度和渗透率比银根额济纳旗盆地要好得多。
Based on aeromagnetic data , this paper has analysed and studied regional tectonic characteristics and evolution of yingen - ejin banner basin , affirmed the existence of ne - trending fault in this area , and probed into the role of the formation and development of this set of faults in regional tectonics
摘要根据航磁资料，分析和研究银根额济纳旗盆地的区域构造特徵及其演化，同时确定了该区北东向断裂的存在，并探讨该组断裂的发生发展对区域构造的作用。
It points out the targets for next exploration in yingen - ejinaqi basin are the lithologic and stratigraphic as well as buried hill reservoirs ( volcanic rock and granite ) in the east , the jurassic and lower cretaceous as well as buried bill ( pre mesozoic granite ) reservoirs in the west
提出了银根额济纳旗盆地的下一步勘探方向：在东部，以岩性、地层、古潜山（火山岩或花岗岩）油藏为主：在西部，以侏罗系、下白垩统及古潜山（前中生界花岗岩）油藏为主。
Abstract : based on aeromagnetic data , this paper has analysed and studied regional tectonic characteristics and evolution of yingen - ejin banner basin , affirmed the existence of ne - trending fault in this area , and probed into the role of the formation and development of this set of faults in regional tectonics
文摘:根据航磁资料，分析和研究银根额济纳旗盆地的区域构造特征及其演化，同时确定了该区北东向断裂的存在，并探讨该组断裂的发生发展对区域构造的作用。
We can draw some conclusions below by analyzing the salt capacity in the soil in the ejnqi oasis in the direction from east to west and from south to north , which is that in the horizonal direction , the total salt capacity in the soil become more and more higher with the longer distance far from the center of the oasis and in the vertical direction the salt capacity differs evidently with depth
额济纳旗绿洲东西、南北两个方向的取样点的盐份含量具有以下特点：以绿洲中心为基点，离绿洲越远，总含盐量越高；在垂向上，远离绿洲的土壤中各种盐类的浓度随深度的变化也很大。
Chagan sag is a secondary tectonic unit in chagandelesu depression , northeastern yingen - eji ' naqi basin , and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate , with the character of erogenic belt . in working area and its adjacent area , the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly , intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase
查干凹陷属于银根?额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元，其盆地基底为古生代时期华北板块、哈萨克斯坦板块和塔里木板块交接部位形成的陆缘或岛弧褶皱带，具有古生代造山带的性质。研究区及邻区印支期侵入岩形成于造山带强烈挤压陆内俯冲的构造环境；燕山早期侵入岩形成于由挤压转向拉伸、造山带的增厚陆壳开始发生伸展垮塌的构造环境；早白垩世火山岩形成于造山期后进一步发生伸展垮塌的区域构造环境。
Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin , northeastern yingen - ejinaqi basin , and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate , tarim plate and kazakstan plate
查干德勒苏凹陷属于银根?额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元。其基底为古生代时期华北板块、塔里木板块和哈萨克斯坦板块交接部位的陆缘或岛弧褶皱带，具有古生代造山带的性质。
Based on the comparative study of yingen - ejinaqi basin and erlian basin from the aspects of mesozoic strata , regional structures , magmatic activity , source rocks , reservoir , oil and gas reservoir formation characteristics , oil and gas distribution , and deep crustal structure , it shows that these two basins are similar to each other in regional geology amid petroleum geological features
摘要通过对银根额济纳旗盆地与二连盆地的中生代地层、区域地质构造、岩浆活动、烃源岩、储层、油气成藏特征、油气分布规律及深部地壳构造等的研究，表明两盆地的区域地质及石油地质特征具有相似性。