背斜的 的英文怎麼說
中文拼音 [bēixiéde]
背斜的
英文
anticlinal-
A full backpack was not enough, i needed to hung a tent, a dampproof mat, a matting outside my backpack, and a most professional alpenstock and a spider inserted outside my backpack agley, and hung a aluminium water bottle made in spain at backpack belt at my front chest
背包塞滿了是遠遠不夠的，我仍需須要外掛上帳篷防潮墊地席涼鞋和快掛數個，當然最顯專業風范的行走杖和三腳架也得斜斜的插在背包外面，再在前胸的背包帶上掛上個西班牙產鋁制水壺。In view of the variation in the dip, here could be a local anticlinal fold.
鑒于傾斜方向的變化，此地可能存在一個局部的背斜褶皺。The core of the anticlinal fold, which is squeezed between faults, underwent intense crushing.
背斜褶皺的核部在斷層間受到擠壓，遭受到很強的破壞。Spacings between anticlinal crests and synclinal troughs in the member tend to be equal in some series of folds.
巖層中的背斜峰和向斜谷之間的距離趨于相等。It appears to be a sharp anticline with a strong suggestion of faulting on one side.
它看來象是在一邊有著明顯的斷層跡象的陡峭的背斜。Research on construction technique for mawangcao tunnel 1 to cut across anticline and coal seam
馬王槽1號隧道穿越倒轉背斜和煤層的施工技術Analysis on the minerogenetic geological condition of the gold ore in the lianhuashan anticline, western guizhou
貴州蓮花山背斜金的成礦地質條件分析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
摘要濟陽坳陷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沉積背斜構造，然而由於坳陷在斷陷期基底滾動式沉降，造成撓曲頂部的塌陷，形成復雜的塊斷結構，使本區同沉積構造發生強烈改造，往往與各次級斷層或沉積地層相復合，表現出獨特的構造景觀。The author suggests that the three lithosphere - scale faults, lancangjiang fault, jinshanjiang - ailaoshan fault and axis fault in the middle of the basin, are the main geological structures that control the formation of basin, magmatism and metallogenic congregate district. the anticline structure with an axis of triassic strata and the related fault system within the basin, and gonglang arch - shaped folding structure in the south of the basin are the geological structure controlling the formation of ore fields. junctions of two or more faults with different orientation, interlayer cataclastic structural zone and oxidation - reduction ( redox ) boundary were the favorable position for the formation of ore bodies
認為瀾滄江斷裂、金沙江-哀牢山斷裂及盆地中軸斷裂這三條巖石圈斷裂是主要的控盆-控巖（巖漿巖）構造及礦集區尺度的控礦構造；盆地中以三疊系為軸的背斜構造及相關的斷裂系統、盆地西南緣公郎弧形構造等是礦田尺度的控礦構造；多組斷裂的交叉、層間破碎帶及地層柱中的氧化還原界面是形成礦體的有利部位。Hydrocarbons may be trapped in anticlines draped over deeply-buried horsts in the pre-deltaic basement.
油氣可以被捕集在背斜中，這類背斜蓋在前三角洲基底中深埋了的土壘上。By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.
依據地貌形態分為三類：正向穹窿型、負向塌陷型、邊隆核陷型：依據巖漿-熱力作用影響的深淺程度或深度分為五類： （古）地熱異常群集區、表淺層火山噴發-熱液活動與淺成侵入型、熱力背斜（熱穹窿） 、中深層侵入型、深部地幔（地殼）熱柱型；提出了熱力構造作用空間分佈的理想模式，將洋陸系統、盆山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用（拆沉）等納入一個整體統一的熱力作用系統中，為盆地動力學研究打開了一個新窗口；研討了熱力構造研究方法。59 sot : jai wanigesinghe ( german ) we have a cinema, this is the art gallery, over there is the daimler - stadium, where all the matches are, here is the pedestrian district, this is the schloss - platz with the column, in the background you can see the sloping hills covered with houses, for me that ' s what stuttgart expresses … at least at first glance
我們有一個電影院，這邊是藝術館，那裡是戴姆勒體育場，在那裡會舉行很多的比賽，這里是步行街，而這邊是宮殿廣場背景則是傾斜的山脈，點綴有零星的房屋，這就是我心目中的斯圖加特的景象…至少，這是給人的第一印象。Based on the studies of microthermometry, gas composition, liquid composition, rare earth elements, ore - forming elements and 13c, d, 18o of fluid inclusions from the mineralization district and the representative deposits, such as zacun gold deposit, shuixie copper - cobalt deposit, shiyancun stibium deposit and bijiashan stibium deposit, two metallogenic fluid systems have been distinguished, i. e., zijinshan metallogenic fluid system and gonglang metallogenic fluid system in weishan - yongping mineralization district
礦化集中區及扎村金礦、水泄銅鈷礦、石巖村銻礦、筆架山銻礦等典型礦床流體包裹體的顯微測溫、氣相成分、液相成分、稀土元素、重金屬元素及~ （ 13 ） c ， d ， ~ （ 18 ） o穩定同位素的研究表明，雲南巍山-永平地區銅金多金屬礦化集中區存在兩個成礦流體系統：紫金山背斜成礦流體系統與公郎弧成礦流體系統。Through the study we know the valley of syncline and the peak of anticline are all good storing places of ore - forming element. to form large industrial ore deposit, the condition of magma channels and the metallogenic fluid must be up to the mustard synchronously
研究結果表明，礦體的形成過程中，向斜構造的凹部和背斜構造的軸部虛托部位都是成礦的有利位置，但僅此還不夠，還應該有較好的通道條件和豐富的含礦流體來源。The study results on hydrocarbon preserving conditions have suggest ed that influenced by latter tectonic movements, especially by the yanshan ~ himalayan tectonic movement, obviously different hydrocarbon preserving conditions occur between the eastern and the western parts bounded by the qiyue mountain. the whole lower paleozoic hydrocarbon enclosing and preserving conditions for the shizhu synclinorium - fangdoushan antici inorium to the west of qiyueshan mountain have the advantage over those of the qiyueshan antici inorium - lichuan synclinorium to the east of qiyue mountain
通過油氣保存條件的研究認為：受後期構造運動的影響，尤其是燕山期?喜山期構造運動的影響，造成區內以齊岳山為界東西油氣保存條件存在明顯差異，齊岳山以西的石柱復向斜?方斗山復背斜下古生界油氣整體封存條件明顯優于齊岳山以東的齊岳山復背斜?利川復向斜。The limited hydrothermal karst and mixed zone beneath the anticline axis controls the porosity distribution of ordovician system and it is anticipated that surroundings of the axis of fold formed by compressional reverse orverthrusting during indo - chinese epoch and the coordinated area of morphology of anticline in the screen of buried hill and that of top surface morphology is the best position for development of the reservoir
局限的熱液巖溶和裸露的背斜軸部之下的混合帶對千米橋潛山奧陶系孔隙分佈具有重要控製作用，預期在印支期擠壓逆沖作用形成的背斜軸部，特別是潛山內幕背斜形態與潛山頂面形態相互協調的區域，應是儲層發育最好的部位。By means of stress - strain feature of upper and lower strata of fold neutral plane in the course of longitudinal fold formation, the differences between the upper coal bed and lower coal bed of fold neutral plane are analyzed from the coal thickness, coal structure, coal body structure, coalbed gas occurrence and diversities etc., revealing the cause of these appearances
摘要利用縱彎褶皺變形中中和面上下巖層的不同應力與應變特點，分析了處于褶皺中和面上下各煤層在背斜與向斜部位煤層厚度、煤層構造、煤體結構及煤層瓦斯的賦存規律與差異性，揭示了這些現象產生的原因。It is shown that deep abnormal high pressure confined area ( abnormal prressure fluid compartment ) at footwall in southern margin of the basin and uplift sector closely related to faulting should be as a domain or direction for exploration ， and structural traps ( like faulting barrier ， anticline ， etc. ) along with original oil / gas reservoirs at major faulting footwall as the main exploratary targets
盆地南緣斷裂下盤深層的異常高壓封閉區（流體封存箱） 、與斷裂密切相關的隆起段是今後主要勘探方向與領域，斷裂遮擋、背斜等構造型圈閉? ?主斷裂下盤原生油氣藏是主要的勘探對象。The ore - hosted strata of xitieshan lead - zinc ore deposit is located in a limb of a anticline and suffered from deformation partition
摘要錫鐵山大型鉛鋅礦床含礦巖系的構造格架位於背斜的一翼，普遍遭受變形分解作用。Formation time and formation mechanism of the weiyuan anticlin e in sichuan basin
四川盆地威遠背斜的形成時代及形成機制分享友人