古褶皺帶 的英文怎麼說

中文拼音 [zhòudài]
古褶皺帶 英文
palaeides
  • : Ⅰ名詞1 (古代) antiquity; ancientry 2 (先哲的遺典、道統) books or orthodoxies of ancient sages...
  • : 名詞(褶子) pleat; crease; fold; wrinkle
  • : Ⅰ名詞(皺文) crease; wrinkle; crinkle Ⅱ動詞(起皺紋) wrinkle up; crumple; crinkle; crease
  • 古褶皺 : paleofold
  1. 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

    查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元,其盆地基底為生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成的陸緣或島弧,具有生代造山的性質。研究區及鄰區印支期侵入巖形成於造山強烈擠壓陸內俯沖的構造環境;燕山早期侵入巖形成於由擠壓轉向拉伸、造山的增厚陸殼開始發生伸展垮塌的構造環境;早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。
  2. 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

    查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元。其基底為生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位的陸緣或島弧,具有生代造山的性質。
  3. Geotectonically, the youjiang sedimentary basin was referred as youjiang yindosinian folded belt. triassic turbidites accumulated in the basin were derived from surrounding ancient lands including yuebei, jiangnan, and yunkai. tectonic setting of the sedimentary basin was in between an active continental margin and a continental island arc

    賦礦濁積巖系的主要物源區為盆地周圍的「越北陸」 、 「江南陸」和東邊地區包括欽防海西在內的「雲開陸」 ,沉積構造背景介於大陸島弧和活動大陸邊緣之間的過渡構造環境。
  4. According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin

    依據理論分析及勘探實踐,優選出4個有利的勘探區,它們是:庫車前陸沖斷近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉;準南前陸沖斷第二、第三排構造;川西北部及南部燕山運動期隆起、川中平緩構造以及深坳陷內部的非常規天然氣;柴北緣冷湖南八仙構造
  5. Several important tectonic events took place in the chinese continent during the early paleozoic, such as the amalgamation of xiyu plate, forming a unified crystalline basement with the cathaysian plate, development of widespread intraplate deformations in southern yangtze plate, and the occurrence of altay - ergun collision zone

    它們與蘇格蘭阿帕拉契亞的加里東事件完全不同,在中國大陸出現了西域板塊完成拼合,華夏板塊構成統結晶基底,南揚子板塊廣泛發育板內,此時還形成了阿爾泰額爾納碰撞等重要構造事件,而以中朝和北揚子板塊為代表的其他板塊則主要表現為穩定沉積,地塊運移,並呈離散狀態。
  6. 3 ) according to the dayi conglomerate " s gravel composition and direction when water flowed during geological age, comeback the paleogeograph of the longmenshan foreland basin, speculates that the dayi conglomerate " material source is located in the songpan - ganzi fold belt to the east, the pengguan fault to the west of the western sichuan plateau region

    3 )根據大邑礫巖礫石成分及流向分析,推測大邑礫巖物源區為松潘-甘孜以東、彭灌斷裂以西的龍門山地區,並恢復大邑礫巖沉積時期巖相地理,認為大邑礫巖物源主要來自龍門山沖斷一側。
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