orogenic phase中文是什么意思

• 造山期
• 造山相

• "phase"中文翻译    n. 1.形势，局面，状态；阶级。 2.方面，侧面。 3 ...
• "late orogenic phase" 中文翻译 :    晚造山相
• "late-orogenic phase" 中文翻译 :    晚期造山幕
• "paroxysmal orogenic phase" 中文翻译 :    突变性造山期
• "orogenic" 中文翻译 :    造山的; 造山运动的
• "kata-orogenic" 中文翻译 :    鼎盛造山期的
• "late orogenic" 中文翻译 :    造山运动晚期
• "late-orogenic" 中文翻译 :    晚造山期的; 造山运动晚期
• "orogenic activity" 中文翻译 :    造山运动
• "orogenic batholith" 中文翻译 :    造山成因的岩基
• "orogenic belt" 中文翻译 :    造山带
• "orogenic crumpling" 中文翻译 :    造山挤压作用
• "orogenic cycle" 中文翻译 :    造山旋回; 造山循环
• "orogenic episode" 中文翻译 :    造山幕
• "orogenic epoch" 中文翻译 :    造山期
• "orogenic event" 中文翻译 :    造山事件
• "orogenic facies" 中文翻译 :    造山相
• "orogenic movement" 中文翻译 :    造山运动
• "orogenic province" 中文翻译 :    造山省
• "orogenic sediment" 中文翻译 :    造山运动沉积物; 造山运动沈积物
• "orogenic sequence" 中文翻译 :    山地土系列
• "orogenic soil" 中文翻译 :    山地土壤
• "orogenic unconformity" 中文翻译 :    造山不整合; 造山运动不整合
• "orogenic welt" 中文翻译 :    造山接缝
• "orogenic zone" 中文翻译 :    造山带

• The qiongzhong granite should have been formed at orogenic relaxing stage after the peak of indosinian orogeny , and the danxian granite were formed at the latest orogenic phase
  琼中岩基可能形成于“印支期”碰撞造山运动峰期后的松弛阶段，而儋县岩基则可能形成于造山运动的结束阶段。
• 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。