陡倾的英文

• heavy pitching
• steep dip
• steep pitch

• "陡"英文翻译    steep; precipitous
• "倾"英文翻译    incline; lean; bend
• "陡倾角" 英文翻译 :    high dip angle; steep dip
• "陡倾斜" 英文翻译 :    steep pitch
• "陡倾锥" 英文翻译 :    steep-sided cone; stesided cone
• "陡倾长翼" 英文翻译 :    steep long limb
• "陡倾伏褶皱" 英文翻译 :    steeply plunging fold
• "陡倾角偏移" 英文翻译 :    stedimigration
• "陡倾矿层" 英文翻译 :    pitching seam
• "陡倾逆断层" 英文翻译 :    steeply inclined reversed fault
• "陡倾斜的" 英文翻译 :    high dipping
• "陡倾斜地层" 英文翻译 :    half-edge layer
• "陡倾斜反射" 英文翻译 :    steeangled reflection
• "陡倾斜矿体" 英文翻译 :    steeply dipping ore body
• "陡倾斜煤层" 英文翻译 :    half-edge seam
• "陡倾斜岩层" 英文翻译 :    steep-dipping bed
• "陡倾斜组" 英文翻译 :    group of steep dipping
• "陡倾斜褶皱" 英文翻译 :    steeply inclined fold
• "陡倾岩层" 英文翻译 :    pitching bed
• "陡倾正断层" 英文翻译 :    steep normal fault
• "急陡倾斜" 英文翻译 :    a steslope
• "冲断层陡倾区" 英文翻译 :    ramp region
• "陡倾斜地层；倾角为45" 英文翻译 :    half-edge layer
• "极大的陡倾伏褶皱" 英文翻译 :    exceptionally large steeply plunging fold
• "易产生顺层滑坡的陡倾高角斜坡面" 英文翻译 :    daylighting

• At a surface exposure the host rock dips steeply to the east .
  在一个露头处，含矿主岩向东陡倾。
• Southeast of the ccsd main hole , there are quite a few such reflectors , implying that eclogite bodies exist in the extension direction of the surface eclogite body
  在ccsd主孔东南方深部重力高部位有多个这样的拱形反射，预示在地表陡倾榴辉岩的延伸方向还有多个一定规模的隐伏榴辉岩体。
• The fractures in the right bank of some dam are composed of the tension fractures dipping toward to the inner slope and perpendicular to the slope strike
  摘要西南某水电站坝区右岸不但发育陡倾坡内并与坡面走向大致平行的张裂隙和断层也有一系列倾角近于直立与坡面走向近于垂直的张裂隙。
• Through opencut mining of cihai hidden iron ore deposit in recent years , it is found that there are multiperiodic diabase walls penetrated the steeply north - inclining iron ore bodies in different directions in early postmineral period so as to destroy the integrity of the iron ore bodies and divide them into many small south - inclining bodies
  通过对该隐伏矿床的露天挖掘开采，发现铁矿床在成矿后，早期有多期次辉绿岩墙以不同方向穿插于向北陡倾之铁矿体中，从而使铁矿体的完整性受到破坏，肢解成众多向南倾小矿体。
• Through imitated to experiment to the physics of the typical model slopes , it can be found that the k23 + 850 ' s dip slope is belong to creep - sliding and fracturing , that the k47 + 750 ' s scarp slope is belong to bending and fracturing , ( 3 ) it is a effective method by establishing the reasonable geology model , and proceed to study with evaluation of determine the nature and fix quantifying
  通过对典型边坡的物理模拟试验，研究发现k23 + 850处中倾顺向岩质边坡变形破坏形式为滑移?拉裂型，而k47 + 750处的陡倾内反向岩质边坡的变形破坏形式为弯曲?拉裂型。其次是建立合理的地质模型，对边坡进行定性及定量评价。
• And we pointed out the evolution of the first group which is the biggest level from north to south basically is limited by shaanbei syncline structure , the evolution of second group which is the mid - level form east to west or from west to east basically is limited by the bedrock joints , the evolution of the last one , which belongs to small level is limited by loess joints
  经过分析和研究，认为黄土圾区是以厚层黄上体为载体的特殊地貌景观，其自身沟道发展演化具有特殊性，以鱼鳞状黄土崩塌为主的高角度陡倾河谷的加宽发展方式为特点，构成洛） 11式河谷发展演化模式。