隆起带的英文

• mole track

• "隆起"英文翻译    rise; tuberositas; bulge; pr ...
• "带"英文翻译    belt; girdle; ribbon; band; ...
• "赤道隆起带。" 英文翻译 :    equatorial bulge
• "可能隆起带" 英文翻译 :    zone of potential heave
• "中央隆起带" 英文翻译 :    central uplift belt
• "地质条状隆起带" 英文翻译 :    welt
• "起带器" 英文翻译 :    belt lifter
• "隆起" 英文翻译 :    [地质学] rise; tuberositas; bulge; protuberate; eminentia; hump; uplift; upheaval; heave; intumescentia; lifting; cripling; swelling; scabrosity; welt; symon fault; hoove-up (指底板); raise; tenting; eminence;◇隆起带 upwarping zone; uplifted zone; 隆起区 bulge region; rise region; 隆起翼 rise flank
• "起带头作用" 英文翻译 :    play the role of an initiator; take the lead
• "一起带走" 英文翻译 :    carry along; carryalong
• "扶垛状凸起带" 英文翻译 :    buttress zone
• "背隆起" 英文翻译 :    dorsal hump
• "底隆起" 英文翻译 :    bottom heave=basal heave
• "额隆起" 英文翻译 :    frontal eminence
• "腹隆起" 英文翻译 :    ventral tubercle
• "古隆起" 英文翻译 :    palaeohigh
• "后隆起" 英文翻译 :    after wale; after-wale
• "眶隆起" 英文翻译 :    orbital tubercle
• "隆起, 隆凸" 英文翻译 :    eminelntia
• "隆起,隆凸" 英文翻译 :    eminentia
• "隆起；平错" 英文翻译 :    heave
• "隆起；上升" 英文翻译 :    upheaval
• "隆起部" 英文翻译 :    crown
• "隆起处" 英文翻译 :    bumcontact; bumpad
• "隆起的" 英文翻译 :    bulbous; embossed; intumescent; protuberant; ridgy

• In prophase there existed thermal and magma activity , and before the
  其下为一火成岩体隆起带，之下有更深部的热力作用区。
• The development of zhongyuan urban agglomeration , as a key construction project of building a comfortably off society an all - round way in henan province , is being paid attention widely
  中原城市群经济隆起带作为河南省全面建设小康计划的重点建设项目，其发展受到广泛注视。
• The research result has suggested that in the southern and northern sides of the kangmar - hajinsangre dome zone , the east - west direction lineral structure forms outstanding arc - shaped of south , throughout all the region from west to east
  研究表明，在康马?哈金桑惹隆起带南北两侧，近东西向线形构造呈向南突出的弧形，自西向东贯穿全区。
• In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric , karst region controlled by folded structures near depressed belts and blinded karst region in fault basins
  目前开展的可有效利用的地下水资源调查评价将该区划分为隆起带裸露岩溶分布区、沉降带边缘褶皱构造控制岩溶分布区和断陷盆地隐伏岩溶分布区。
• The control of the deep - seated structural - magmatic process over the metallogenic system around the middle - lower yangtze river reaches is shown as : ( 1 ) the mantle uplift belt is closely related to the general geological background of the metallogenic system ; ( 2 ) the primitive magma originated from different parts of the mantle uplift belt ( mantle ridge or mantle slope ) shows differences in style of formation and composition and results in different magmatic series and metallogenic subzones , respectively ; ( 3 ) the varying depths of structural - magmatic chambers may form a " three - layered structure " ( central type , network - like and ring - like ) and this is the primary factor that controls the different magmatic series and the concerned cluster of ore deposits ; ( 4 ) the alkaline basaltic magma derived from the mantle ridge forms high - potassium and calcium alkaline magma and shoshonitic magma due to its altering intensity of afc process with the lower crustal material , which has something to do with the copper - gold and iron - sulphur metallogenic subsystems , respectively
  深部构造岩浆作用对长江中下游成矿带安徽沿江地区成矿系统的控制表现为： ( 1 )地幔隆起带与成矿系统的总体地质背景的演变密切相关； ( 2 )源于地幔隆起带不同部位(幔脊与幔坡)的原始岩浆，其生成方式和物质组成不尽相同，它们分别产生相应的不同岩浆岩系列和成矿亚带； ( 3 )不同深度的构造岩浆房组成中心式网格式环带式“三层结构” ，是控制区内不同岩浆岩系列及有关矿床集中分布的主要因素； ( 4 )源于地幔隆起带脊部的碱性玄武岩浆，由于与下地壳物质发生的afc作用强度不同，形成了高钾钙碱性岩浆和橄榄安粗岩浆，分别与铜、金成矿亚系统和铁、硫成矿亚系统有关。
• 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
  本文利用区域可持续发展理论，应用数学模型以及gis方法对该区域的可持续发展状况进行了研究，分析了该区域10年来的综合发展水平、协调性状况以及分时段的协调状况的空间演变，探讨了该区域内各可持续发展子系统对区域可持续发展的影响，并在此基础上提出了中原城市群经济隆起带实现可持续发展的发展战略。
• During late mesozoic and cenozoic , extensions were widespread in eastern china and adjacent areas . the induced compressions and extensions , uplifting and subsidence as well as large - scale magamatism , increased the pre - existing ne - nne trending faults , uplifts and subsidence belts . this is how ; the giant transform structure led to the formation of xihu depression
  在晚中生代与新生代，拉张作用广泛分布于中国东部及邻区，导致了挤压与拉张、隆起与沉降以及大规模的岩浆作用，于是使早先存在的北东北北东向断层、隆起带与沉降带增强，这也是大的转换断层形成西湖凹陷地层的机理。
• In that , it introduces detailedly the zhongyuan urban agglomeration at first , which is about how to form zhongyuan urban agglomeration and why this region forms and its development . in succession , it researches the sustainable development of this region with above - mentioned theories and societal , economic and environmental data of the studied region . it mainly analyses the level of general development and harmony status of economic , societal and environmental subsystem of the studied region in 10 years
  第五部分是本文的主体部分，该部分首先对中原城市群经济隆起带进行了较为详细的论述，论述了该区域的由来、历史演化及其形成原因，之后应用上述的理论及数据对该区域的可持续发展状况进行了分析，主要分析了该区域系统10年来的综合发展水平状况、经济、社会和环境子系统间的协调状况以及不同时段该区域系统协调状况的空间分布状况，并对其进行了评价分析，提出了该区域今后的发展战略。
• The authors hold that the joint actions of numerous factors such as the upper mantle uplifted zone ( the mantle thinned zone of lithosphere ) , the upper mantle anomalous area ( relatively low - velocity area ) , the uplifted zone of intracrustal high - conductivity layer , the deep fault ( shear zone of lithosphere ) , the margin of the crust - upper mantle uneven masses , the basement uplifted area reflected by gravity high , the magmatic belt and tectonic intersection reflected by skipped magnetic field , control the distribution of auriferous skarn deposits and copper ( associated with gold ) skarn deposits
  作者认为，上地幔隆起带（岩石圈地幔减薄带） 、上地幔异常区（相对低速区） 、壳内高导层隆起带、深断裂（岩石圈剪切带） 、地壳上地幔不均匀性块体的边缘、重力高反映的基底隆起区、跳跃磁场反映的岩浆岩带和构造交汇处等诸多因素的共同作用控制著含金夕卡岩矿床和铜伴生金夕卡岩矿床的分布。
• In this case during paleozoic , nearly east west trending arc structures resulted from the interaction between china plate and siberian plate . in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault , diaoyudao fault , okinawa fault , uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate
  本文所涉及近东西向展布的弧形构造形成于古生代时期中国板块与西伯利亚板块的碰撞带，而在中生代，中国板块下的kula - pacific板块向西俯冲导致了北北东向和北东向构造（如duimadao断层、 diaoyudao断层、 okinawa断层、隆起带和沉降带）以及位于中国板块东部的火山岩浆带。