沉陷斷塊 的英文怎麼說

中文拼音 [chénxiànduànkuāi]
沉陷斷塊 英文
trough block
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : Ⅰ名詞1 (陷阱) pitfall; trap2 (缺點) defect; deficiency Ⅱ動詞1 (掉進) get stuck or bogged do...
  • : Ⅰ動詞1 (分成段) break; snap 2 (斷絕;隔斷) break off; cut off; stop 3 (戒除) give up; abstai...
  • : 名詞(古時佩帶的玉器) penannular jade ring (worn as an ornament in ancient china)
  • 沉陷 : 1. (下陷) sink; cave in 2. (沉降) sinkage; downpunching; depression; subsidence; [建築] settlement
  1. Due to the multi - period tectonic movement and evolution of mechanical mechanism, syndeposition structures occur extensively in jiyang sag, the base of the sag subsided alternatively during the fault depression, which resulted in sinking of top bending and complicated block structure accordingly, reconstructed the syndeposition intensively, and produced the special structural landscape in combination with all levels of faults and sedimentary formations within it

    摘要濟陽坳由於受到多期構造運動的影響,在前第三系古地形高點背景上廣泛發育同積背斜構造,然而由於坳期基底滾動式降,造成撓曲頂部的塌,形成復雜的結構,使本區同積構造發生強烈改造,往往與各次級層或積地層相復合,表現出獨特的構造景觀。
  2. 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區域構造背景的基礎上,將濟陽坳古生界潛山的形成過程分為四個階段,即古生代早中生代?穩定降?隆升?輕微褶皺變形及逆層發育階段、中生代?初步階段?期、新生代早期?拗階段?潛山形成期以及新生代晚期?坳階段?潛山定型期。
  3. The main conclusions are as follows ; firstly, under the influence of three phases of episodic activities, three two - order sequences is composed of three depositional cycles and three regional unconformities ; secondly, under the control of structure activities such as fault - block activities and the influence of three - order climate cycles and source recharge, lower cretaceous can be divided into six three - order sequence ; thirdly, because fault activities is weak and fault slope is gently, fan deltas exist in steep slopes in early and later stages and subaqueous fans exist and turbidite fans exist in troughs in middle stage

    主要的結論為:其一,受三期幕式活動影響,形成了3個大的積旋迴和3個區域不整合面,構成了下白堊統3個二級層序;其二,受內翹傾和等構造活動的控制,以及三級氣候旋迴和物源供給因素的影響,下白堊統劃分出6個三級層序;其三,在單湖盆中,湖泊階段的早、晚期由於凹邊界層活動較弱,面較緩,陡坡可以發育扇三角洲,在湖泊階段的中期主要為水下扇砂礫巖體,並在窪槽區發育濁積扇。
  4. Depositional cycles on basin scale have been interpreted as the result of depositional response to tectonism such as episodic rifting, polyphasic compressive flexural subsidence and reversion, and differential subsidence of fault blocks ; while the formation of high frequency sequences was attributed to variation in lake level and sediment supply

    盆地規模的積旋迴多是盆地幕式裂、多幕擠壓撓曲降、多期構造反轉、差異降等構造作用的積回應;高頻層序單元的發育則主要與湖平面和積物供給量的變化有關。
  5. Based on the theory of plate tectonics and the new knowledge of continental dynamics, this paper starts mostly with tectonic analysis and then makes a comprehensive view on the characteristic of stratum composition, gold mine mineralized, magmatic activity as well as ruptures activity to discuss the yanshanian tectonic evolution of the xiaoqinling area under the regional tectonic framework of qinling orogenic belt

    本文以板構造理論和大陸動力學研究的新認識為指導,採用以構造分析為主線,結合區內地層積、金礦成礦、巖漿活動以及南北兩側盆地形成演化等綜合分析,在秦嶺區域構造大框架下對小秦嶺燕山期的構造演化特徵進行探討。
  6. Results obtained in the research are : l. by the virtue of palaeostructure analysis and method of balanced cross sections, we have studied the formation and development history of qianmiqiao buried hills, and indicate that the formation of ordovician buried hills can be mainly divided into four periods, namely, stable uplift period, fold - thrust period, block - fault tilting period, and thermal subsidence and depression period

    論文取得以下成果: 1採用古構造分析和平衡剖面技術,研究了千米橋潛山的形成演化史,指出其下古生界奧陶系潛山的形成主要經歷了穩定抬升、褶皺沖翹傾和熱降坳四個時期。
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