次生褶皺 的英文怎麼說
中文拼音 [cìshēngxízhòu]
次生褶皺
英文
secondary fold-
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，其盆地基底為古生代時期華北板塊、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褶皺帶，具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶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、造山帶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。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。其基底為古生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位的陸緣或島弧褶皺帶，具有古生代造山帶的性質。They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill. we mark off five kinds of buried hill belts. they include three different kinds of trap on the basis of the cause of trap formation
本次研究在重新認識濟陽坳陷區域構造背景的基礎上，將濟陽坳陷古生界潛山的形成過程分為四個階段，即古生代早中生代?穩定沉降?隆升?輕微褶皺變形及逆斷層發育階段、中生代?初步斷陷階段?塊斷期、新生代早期?斷拗階段?塊斷潛山形成期以及新生代晚期?坳陷階段?潛山定型期。During the vicomtes story she sat upright, looking from time to time at her beautiful, plump arm, which lay with its line changed by pressure on the table, then at her still lovelier bosom, on which she set straight her diamond necklace. several times she settled the folds of her gown and when the narrative made a sensation upon the audience, she glanced at anna pavlovna and at once assumed the expression she saw on the maid - of - honours face, then she relapsed again into her unvarying smile. after ellen the little princess too moved away from the tea - table
在講故事的當兒，她腰板挺直地坐著，時而瞧瞧輕松地擱在茶幾上的肥胖而美麗的手臂，時而瞧瞧更加美麗的胸脯，弄平掛在胸前的鉆石項鏈，她一連幾次弄平連衣裙的皺褶，當故事講到令人產生深刻印象的時候，她回過頭來看看安娜帕夫洛夫娜，立時現出和宮廷女官同樣的面部表情，隨后便安靜下來，臉上浮現出愉快的微笑。The tectonic motion is very intense in front belt of north tianshan mountain, drape fault and so on very develop, and there occurred many times destruct earthquakes
摘要北天山山前地帶是構造運動十分強烈的地區，褶皺斷裂等構造現象十分發育，這里曾發生過多次中強破壞性地震。分享友人