斷裂撓曲 的英文怎麼說

中文拼音 [duànliènáo]
斷裂撓曲 英文
faulted flexure
  • : 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...
  • : 裂動詞[方言] (東西的兩部分向兩旁分開) open
  • : 動詞1. (輕輕地抓) scratch 2. (擾亂;阻止) hinder 3. (彎曲,比喻屈服)yield;flinch:不屈不撓indomitable; unyielding
  • : 曲名詞1 (一種韻文形式) qu a type of verse for singing which emerged in the southern song and ji...
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  1. Zijingguan fault zone is characterized with cataclasite series of tectonic rocks and joints alongside the deformational zone, and sometimes with uniclinal flexure or folds. the intensity of deformation increases from the sides to the center of the fault in the section, which appears from joints to cataclastic rocks

    紫荊關帶兩主變形帶以碎巖系列構造巖和節理帶組合為特徵,局部出現和褶皺,由兩盤至中心變形強度增大,一般由節理帶過渡為碎巖帶。
  2. The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep. under the background of indian plate subducting under asia - europe plate, bachu forebulge was greatly affected by the development of southwest depression and awati depression. almost all of its structure reversed, and as a result of it, both of its south and north boundary migrated. according to its evolution history and its feature, the authors tentatively use both - side migration model to interpret the evolution of compound forebulge. since triassic, almost all the spheres above lithosphere synchronously became flexure. because transpressional stress field became increasingly strong, bachu forebulge continued uplifting and big faults formed. then, bachu uplift, as a whole, slipped upward along those big faults and showed migrating toward thrust zone in plane. in tectonic tranquility, the lithosphere bounded back and in consequence of it, bachu uplift slipped down and showed migration toward craton, at that moment negative inversion structures developed. while the forebulge migrated toward its south and north foredeep, it was very possible that locally extensional stress appeared in the forebulge

    在印度板塊向歐亞板塊俯沖的大背景下,巴楚前緣隆受西南坳陷和阿瓦提凹陷的影響,新生代時構造體制發生反轉,邊界向南北遷移。根據其發育過程特徵,作者用復合前緣隆起兩端遷移模式對復合前緣隆起獨特的構造發育史進行了解釋:即三疊紀以來巖石圈各圈層同步變形。隨著擠壓應力場的增大,巴楚隆起在基礎上不抬升,形成幾條大型帶。
  3. 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

    盆地規模的沉積旋迴多是盆地幕式陷、多幕擠壓沉降、多期構造反轉、塊差異沉降等構造作用的沉積回應;高頻層序單元的發育則主要與湖平面和沉積物供給量的變化有關。
  4. Test method for modulus of rupture in bending of electrode graphite

    石墨電極芯模數的試驗方法
  5. The author argues that the model can be used to calculate the longitudinal force caused by the temperature or the load acting on one of the double railway tracks, as well as the braking force and the breakage force

    此模型可計算溫度的影響,探究雙線橋樑上的單線荷載作用下的力、制動力和單軌時的軌力。
  6. Meanwhile, the paper has analyzed the influences of fatigue, damnification, bend and liquid collision to sucker rod breaking as well, and suggested some positive measures to avoid sucker rod breaking according to the characteristics of sucker rod breakin in guangbei area of bamianhe oilfield

    同時,對于因抽油桿疲勞、損傷、、液擊對抽油桿的影響也進行了分析,並針對八面河油田廣北區抽油桿的特點提出了積極防治對策。
  7. These phenomena show that the fault has strongly activities at the same time. at that time tan - lu fault zone occurred a large - scale left - lateral displacement. the strike - slip movement on the tan - lu fault zone cau sed the zhangbaling uplifting which became source region and the hefei basin appeared strike - slip flexure at the west side of the fault

    說明了控盆?郯廬帶在該時期具有強烈活動,且以大規模走滑運動為主,郯廬帶的走滑使得東側張八嶺進一步快速隆升,仍構成沉積物源系統;在西側,合肥盆地因走滑而,形成沉積可容空間。
  8. Ophthalmic optics - contact lenses - determination of rigid lens flexure and breakage

    眼科光學.隱形眼鏡.硬質鏡片度和性的測定
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