斷塊地帶 的英文怎麼說
中文拼音 [duànkuāidedài]
斷塊地帶
英文
fault block terrain-
Hefei basin that is located on the southern fringe of the north china plate and by the side of tan - lu fault zone is a mesozoic cenozoic continental basin
合肥盆地為一中、新生代陸相盆地,位於華北板塊南緣、郯廬斷裂帶西側近旁側。( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin
( 6 )論文探討了賽什騰? ?錫鐵山斜向逆沖推覆構造的地質意義,認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的結果,該認識對于研究柴北緣區域構造格局、盆山關系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義,對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。Having analyzed preliminarily formation mechanism of these common characteristics of anomaly, it concludes that : these are results, controlled by basically united tectonic stress field of large - range, caused by stress - strain accumulation and certain phase strong earthquakes, according to deformation difference brought about in tectonic position along the boundary zone and within second - order faults of active blocks resulted from unstable and inharmonious features for movement of block system at different levels and deformation of boundary
分析這些異常共性特徵的形成機制,初步認為:是在基本統一的大區域構造應力場控制下,不同層次塊體系統運動及其邊界帶變形的非平穩、非協調性,在活動地塊邊界地帶和地塊內部次級斷裂構造部位產生變形差異而導致應力-應變積累、孕育強震到一定階段的結果。The research result shows that this physical model is useful to determine the locked area along plate boundary faults and further to make the long term and middle term earthquake prediction
研究結果表明,運用該模型方法可利用大地測量數據確定沿板塊邊界斷層帶的相對閉鎖區,從而進行中長期地震預報。The frontal structure of longmenshan in the west of sichuan is very complex, showing intense structure deformation in overthrust belt, high structure amplitude, steep stratigraphic dip, developed fault blocks, complex seismic wave field, frequent change of lateral velocity, and poor image of post - stack time migration processing
摘要川西龍門山前緣構造非常復雜,逆掩推覆構造帶構造形變強烈,構造幅度大,地層傾角陡,斷塊發育,地震波場復雜,速度橫向變化大,常規疊后時間偏移處理成像效果較差。Sinistral strike - slip faults along the southern alashan margin and eastwards extending of the altun fault
阿拉善地塊南緣的左旋走滑斷裂與阿爾金斷裂帶的東延The species, heights, diameter breast heights, canopy widths and plant numbers in 38 quadrats of 6 belt transects, which were located in yingsu cross - section and kaerdayi cross - section lying in the lower reaches of tarim river where populus euphratica concentrated, were investigated to study the distribution patterns, aggregation intensities and distribution pattern scales of p. euphratica populations at different distances away from the river
摘要在塔里木河下游胡楊分佈集中的英蘇、喀爾達依斷面,設置了6條樣帶38塊樣地進行植被種類、高度、胸徑、冠幅、株數等因子調查,研究了不同離河距離胡楊格局分佈類型、聚集強度及其格局規模。Jiangda tectonic belt lies in the north of the three - rivers ( nujiang, lancangjiang, and jinshajiang ) tectonic belt, sw china ; the east of changdu massif ; the west of jinshajiang faults zone
江達構造帶地處西南三江構造帶北段,昌都地塊東緣,金沙江斷裂帶西側。Due to the west north direction subduction, fast collapse ( delamination ) may take place and the mantle plume emerged in ludong, in addition, owing to the subduction of pacific plate under eurasian, there appeared left - lateral advection and extension for tan - lu faults ( named as yishu fault in shandong ), and together with the collapse of yanshanian orogenic belts, all induced the crustal extension in shandong
由於太平洋板塊對歐亞板塊的俯沖( nw向) ,魯東地區巖石圈發生了快速拆沉減薄作用,同時魯東地區也可能會出現地幔柱的活動;另外,在太平洋板塊俯沖作用影響下,郯廬斷裂(山東稱沂沭斷裂)帶發生了大型左行走滑剪切和拉張活動。In accordance with this rule, it may safely be assumed that the forefathers of boston had built the first prison - house somewhere in the vicinity of cornhill, almost as seasonably as they marked out the first burial - ground, on isaac johnson s lot, and round about his grave, which subsequently became the nucleus of all the congregated sepulchres in the old churchyard of king s chapel
根據這一慣例,我們可以有把握地推斷:波士頓的先民們在谷山一帶的某處地方修建第一座監獄,同在艾薩克約朝遜地段標出頭一塊壟地幾乎是在同一時期。后來便以他的墳塋為核心,擴展成王家教堂的那一片累累墓群的古老墓地。He led her through the wall of prickly trees, that were difficult to come through, to a place where was a little space and a pile of dead boughs. he threw one or two dry ones down, put his coat and waistcoat over them, and she had to lie down there under the boughs of the tree, like an animal, while he waited, standing there in his shirt and breeches, watching her with haunted eyes. but still he was provident - he made her lie properly, properly
他引著她在不易穿過的刺人的樹叢中穿了進去,直到二塊稍為空曠而有著一叢拓死的樹枝的地方,他把些干拓的樹校鋪在地上,再把他的鈣套和上衣蓋在上面,她只好象一隻野獸似地,在樹下躺下去同時,只穿著襯衣和短褲的他,站在旁邊等待著,牢牢地望著她,但是他還有體貼閡到的,他使她舒舒服服地躺著,不過,他卻他她的內衣的帶子扯斷了,因為她只管懶慵地躺著,而不幫助他。Relationship between the wrench structure in the north - margin block - faulting belt in the qaidam basin and altun tectonic system
柴達木盆地北緣塊斷帶的扭動構造與阿爾金構造體系的關系The xiaoqinling area locates in the south margin of north china block which is bounded on the north by the taiyao fault and on the south by the luonan fault
小秦嶺位於華北地塊南緣構造帶,夾持在太要-武家山斷裂和洛南-欒川斷裂之間。According to luonan fault and shandan fault extending roughly from east to west, the qinling erogenic belt is divided into three parts : the south margin of north china block, the northern qinling and the southern qinling
秦嶺造山帶內部以洛南-欒川斷裂和商丹斷裂帶為界將其劃分為華北地塊南緣構造帶、北秦嶺構造帶和南秦嶺構造帶。The slope zone in northern biyang sag is characterized by complex structure, developed minor fault blocks, varied seismic vertical and horizontal velocities and difficult to get imaging, which result in that conventional imaging approaches are hard to meet the needs for exploration and development of this area
摘要泌陽凹陷北部斜坡帶構造復雜,小斷塊發育,地震縱、橫向速度變化劇烈,成像困難,常規的地震成像方法成果難以滿足勘探開發的需要。The seasons brought no change, and continually the clouds hung heavily above her.
季候的轉換不曾帶來什麼變化,沉重的雲塊總是繼續不斷地懸掛在她頭上。In himalayan, the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation. in eastern ore belt, ore - controlling is mainly strike - slip fault and fold ; but in western ore belt, it is block
喜馬拉雅運動第一期45ma盆地掀斜;第二期23ma以差異隆升剝蝕為主;第三期4ma為脆性變形期,東礦帶近盆邊以走向斷裂及褶皺控礦為主,西礦帶為斷塊控礦。It brings forward that the basic - superbasic cluster ( band ) related ni is variscan magmatic rock. it lies in the jin ping superficial fault unit ( also named " golden band " ) of subsidiary fracture unfold and wheel position of hong he " s profound fault and the marginal overgrowth band of yang zi platform
通過上述研究,認為該與鎳有關的基性-超基性巖群(帶)為華力西期巖漿巖,位於紅河深大斷裂舒展轉彎部位的次級斷裂上、揚子地臺邊緣增生帶的金平蓋層斷塊單元中(也稱「金鑲邊」帶中) 。2. the tectonic framework in the basin presents the lozenge patterns which are consist of the w - e structural belts and nw - se structural belts. the w - e structural belts are primary, and that the nw - se structural belts are the transfer belts related to the former
認為盆地內構造變形具有南北分帶、東西分塊的菱形格局特徵,盆地以東西向的擠壓沖斷構造帶為主,北西向構造帶是一個與東西向擠壓構造帶伴生的構造變換帶,主要在變形過程中起調節作用。The study covers regional stratigraphy, regional geological structures and their evolution ; deep - large fracture system and building - moutain straps in the basin ; distributing of mineralization concentration area and mineralazition characteristics of different metal fields ; volcanic magmatic activity and magmatic distributing ; the petrology, element geochemistry features of the magmatic rock series ; the relationship between magmatic distributing and mineralization ; the relationship between magmatic forming - age and mineralization ; the relationship between magmatic form and mineralization ; source of mineral materials, source of hydrothermal solution and source of mineralizing agent ; transport forms of metal in the solution ; the ore - forming geochemical mechanism, etc. it turns out as follows : ( 1 ) lanping basin formed in the linkup of the plates and it was propitious to form deep - large fracture
研究內容包括:區域地層及區域構造演化;盆地深大斷裂系統及造山帶;區域地球物理場;礦集區礦床的時空分佈、礦化特徵;巖漿巖活動與巖漿巖分佈;巖漿巖巖石學特徵;巖漿巖元素地球化學特徵;巖漿巖分佈與成礦的關系;巖漿巖成巖時代與成礦的關系;巖漿巖組成與成礦的關系;成礦物質的來源,成礦流體的來源;成礦物質搬運、富集的地球化學機理等。研究結果表明:蘭坪盆地發育于板塊的拼接地帶,有利於發育深大斷裂系統。分享友人