隆起型 的英文怎麼說
中文拼音 [lōngqǐxíng]
隆起型
英文
ridgy form-
2. tazhong ancient uplift originated from normal fault in paleozoic, hydrocarbon formed in ordovician period, structure reverse made tazhong uplift form from the middle ordovician period to the late ordovician period, and it provided geologic background for the deposit of silurian - devonian stratum. tazhong uplift formed at the end devonian, ancient reservoir was destroyed and asphaltum sandstone formed, structure deformation more destroyed ancient reservoir in early permian, after then the major of structure deformation is regulation
塔中隆起源於早古生代拉張背景下的正斷層，寒武-奧陶紀為其烴源巖形成的重要時期；早奧陶世末-晚奧陶世末的構造反轉是塔中隆起的主要形成期，同時也為志留系形成地層及復合圈閉提供了古地理背景；志留?泥盆紀塔里木盆地南北緣均轉為活動大陸邊緣，形成了大量的斷裂和不整合；泥盆紀末塔中鼻狀隆起基本定型，古油藏遭受破壞，形成了瀝青砂巖；早二疊世晚期的構造變形使古油藏遭受進一步的破壞；二疊紀后構造變動主要以調節為主。Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin
通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。There are 5 depositional systems in the region. they are panne and jishan delta systems coming from chengning heave near the northwest border of the region, shuangfeng delta located in southwest part of the region coming from luxi dome, qudi fan - delta located in the southeast of the studying area and the sub - fan near fault or fan - delta of the southern part of the region. based on the study of sedimentary facies and depositional systems, 11 lithological traps are predicted
在等時地層格架內對沙三段各中期基準面旋迴內的沉積相和沉積體系進行了詳細研究，確定了沙三段沉積時期發育的五種沉積體系類型，即來自凹陷西北邊界埕寧凸起的盤河三角洲體系和基山三角洲體系、來自魯西隆起、分佈在凹陷西南部的雙豐三角洲體系、東南部的曲堤（扇）三角洲體系，南部的近岸水下扇/扇三角洲體系。Using the theory of soil rheology, the relationship among settlement, plumpy and excavation the nonlinear rheological fem program pertinent to excavation is also established used and its availability is proven
運用巖土流變學的理論分析了沉降、隆起和開挖關系，並建立了與之相適應的軟土非線性流變模型。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 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，巴楚前緣斷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撓曲變形。隨著擠壓應力場的增大，巴楚隆起在撓曲基礎上不斷抬升，形成幾條大型斷裂帶。Immanent factors forming subtle trap is many times spread of lake water body. many large land - carriage clastic system provide large deposit space. ancient heave slope band controls distributing of subtle trap
湖盆水體多次擴展是隱蔽油氣藏形成的內在因素；多處大型陸源碎屑體系為隱蔽油氣藏的形成提供了廣闊的儲集空間；古隆起斜坡帶控制隱蔽油氣藏的分佈。With an area of 5300 km2, dongpu depression is located in the southwest of lin - qing depression, bohaiwan basin, bounded with lu - xi uplift by lan - liao fault in the east, with nei - huang uplift by chang - yuan fault in the west, with lan - kao heave by the north feng - qiu fault in the south, with xin country depression by ma - ling fault in the north, while spreading along nne defection, taking on the forms of being wide in the south, and narrow in the north. it is a rift fault depression basin with the characteristics of striking, with the basement being the paleozoic and mesozoic, and the capping beds being the cenozoic
東濮凹陷位於渤海灣盆地臨清坳陷西南端，東側以蘭聊斷裂為界與魯西隆起為鄰，西側以長垣斷裂為界與內黃隆起相接，南以封丘北斷層為界與與蘭考凸起相鄰，北以馬陵斷層為界與與莘縣凹陷相望，是以古?中生界為基底，以新生界為蓋層，古近紀形成的拉分走滑?裂谷型箕狀斷陷盆地。To display the protruding breast of a woman, the designers make the waist girth appear as thin as possible to represent the high breast indirectly ; by means of the flat back of chipau they highlight the wavy shape of the breast
旗袍在交代婦女隆起的胸部時採用了避實就虛的設計手法，把整個女性身體視為一個聯系性很強的整體，通過腰肢纖細的設計而突現胸部的豐腴；通過背的平展而誇前胸的波型。This paper studies the status of this region by theories of regional sustainable development, mathematic models and gis methods in 10 years. this article analyzes general development level, harmony status and special changes of harmony status about every period of time, discusses the influence of each sustainable development subsystem to regional sustainable development, and brings foreword development stratagems to realize sustainable development of the studied region
本文利用區域可持續發展理論，應用數學模型以及gis方法對該區域的可持續發展狀況進行了研究，分析了該區域10年來的綜合發展水平、協調性狀況以及分時段的協調狀況的空間演變，探討了該區域內各可持續發展子系統對區域可持續發展的影響，並在此基礎上提出了中原城市群經濟隆起帶實現可持續發展的發展戰略。The special aerial magnetism, gravity and mt at chasang segment in the western uplifting district show that it is superposed by two or three large - scale south dipping structural block with east - west strike. the closure of bangong lake - dingqing limited ocean and the further gathering of neighboring blocks later form it
西部隆起區查桑段特殊的航磁、重力和mt顯示其由2 - 3個近東西向大型南傾構造塊體疊覆而成，受班公湖-丁青有限洋關閉和相鄰地塊進一步匯聚形成。The results showed that the expressions of il - 1 receptor type 6 tt i in normal adult rat brain were very widely, and there were intense immuno - positive cells of il - 1 receptor type i in septal area, medial preoptic area, neocortex, hippocampus, paraventricular nucleus of the hypothalamus, supraoptic nucleus, hypothalamic ventromedial nucleus, arcuate nucleus and median eminence
結果顯示：型il - 1受體在正常成年大鼠腦內有廣泛的表達，隔區、視前內側區、新皮質、海馬、下丘腦室旁核、視上核、下丘腦腹內側核、弓狀核和正中隆起等部位有較多型il - 1受體陽性的細胞。Because mount jade was built by euro - asia plate and philippine plate, it has an elevation of 3952 meters, and a cross shape
玉山山塊因歐亞板塊和菲律賓板塊相擠撞而隆起，主脈略呈十字型，海拔3952公尺。There are 5 depositional systems in the region. they are : panhe and jishan delta systems coming from chengning heave near the northwest border of the region, shuangfen delta located in southwest part of the region coming from luxi dome, qudi fan - delta located in the southeast of the studying area and the sub - fan near fault or fan - delta of the southern part of the region
確定了沙三段沉積時期發育的五種沉積體系類型，即來自凹陷西北邊界埕寧凸起的盤河三角洲體系和基山三角洲體系、來自魯西隆起、分佈在凹陷西南部的雙豐三角洲體系、東南部的曲堤（扇）三角洲體系，南部的近岸水下扇/扇三角洲體系。The evaluation has been made for normally used four envelope functions of earthquake ground motion. being as evaluation standard of the envelope function this paper pointed out that the controlling capability of the parameters involved in functions of the peak position of the envelope with single peak and the shape of the envelope are essential besides simplicity of the formula of envelope function
本文對已經提出的四種經常使用的包線函數模型進行了評價，認為對于評價單峰點包線函數，除了要求形式簡單以外，其優劣可以用函數對峰點位置和高峰隆起程度的控制能力作為標準。My guess was that the rising mountains to the west shifted the drainage pattern, sending water east toward the atlantic
我當時推測，向西隆起的山脈改變了水系型態，使得河水向東流往大西洋。Bachu arch is a large back - thrust uplift. tectonic evolution of its large boundary fault fracture have relation with oil / gas distribution involuntarily. its large boundary fault fracture is basement rift formed in late hercynian period and strongly actived in late himalayan period. oil / gas distribution of bachu - markit have relation with fault interspace distribution. so, this paper also discussed interspace distribution and movement stage of fault
巴楚隆起是一個大型背沖斷隆，其邊界大斷裂的形成演化自然關繫到本區的油氣分佈，隆起的邊界大斷裂多是海西晚期形成的基底斷裂，后在喜山期強烈活動，兼具壓扭走滑性質。There are two kinds of model for forming gas pools both in the abnormally pressured compartment and out the compartment in the system. after the breakage of overpressured fluid compartments in silurian system, hydrocarbons generated in the compartments flowed to carboniferous in a phase of mixed fluids
下伏志留系高壓封存箱生成的油氣隨箱體頂部破裂呈混相涌流進入石炭系，油氣在石炭系中向繼承性發育的古隆起運移聚集，形成大型古油氣藏，后逐漸演化成古氣藏。Bachu arch is a common forland uplift of southwest of tarim forland basin northeast of tarim forland basin. this arch previously is a low submerged paleohigh which rised integrality above water from late hercynian to terminal hercynian, was exposed to denudation mostly because of uplifting integrality in mesozoic, ulteriorly uplifted and strongly reformed in late himalayan. markit slope is a slope north dipping in early paleozoic, tilted in south - north orientation in hercynian
巴楚隆起作為塔西南前陸盆地和塔東北前陸盆地的共用前陸隆起，是一個早古生代潛伏於水下的低隆，海西晚期至末期呈整體性隆升，露出水面，中生代整體隆升，大面積遭受剝蝕；喜馬拉雅晚期進一步隆升和強烈被改造，才定型成現今的構造格局。This paper also summarized factors of controlling distribution of oil / gas distribution. ( 1 ) control role of palaeohigh ( 2 ) control role of fault ( 3 ) control role of unconformity surface ( 4 ) control role of fracture system
本論文還從對該區現有典型油氣藏分析著手，總結出控制該區油氣藏分佈的因素：古隆起控油；斷裂控油；不整合面控油；裂縫系統控油。分享友人