巴颜喀拉的英文

• bayanhar

• "巴"英文翻译    hope earnestly; wait anxious ...
• "颜"英文翻译    face; countenance
• "喀"英文翻译    noise made in coughing or vo ...
• "拉"英文翻译    cut; slash; slit
• "巴颜喀拉山" 英文翻译 :    bayan har shan; bayan kara ula
• "巴颜喀拉山口" 英文翻译 :    bayan har shankou
• "巴颜喀拉山脉" 英文翻译 :    bayan kara ula
• "我爱你巴颜喀拉" 英文翻译 :    i love you,bayan kala; i love you--bayankala
• "巴颜喀喇山" 英文翻译 :    bayanhar mountains
• "巴颜" 英文翻译 :    bayan
• "喀拉" 英文翻译 :    chimaerasuchus paradoxus; chimera (mythology); lama kara
• "巴颜图" 英文翻译 :    buyantu
• "喀拉喀拉岛" 英文翻译 :    krakatau pulau; pulau krakatau
• "巴颜扎尕尔" 英文翻译 :    bayainchaggar
• "喀拉墩" 英文翻译 :    karadong
• "喀拉海" 英文翻译 :    kara sea; karskoye more
• "喀拉湖" 英文翻译 :    karakul, oz
• "喀拉科" 英文翻译 :    chimaerasuchidae
• "喀拉克" 英文翻译 :    el kerak; karak; kir moab
• "喀拉拉" 英文翻译 :    kerala
• "喀拉奇" 英文翻译 :    karachi
• "喀拉特" 英文翻译 :    kalat
• "喀拉蚩" 英文翻译 :    karachi; karanchi; karāchi; kurrachee; kurrachi
• "sea喀拉海" 英文翻译 :    kara
• "阿什喀拉" 英文翻译 :    al ashkharah

• Structural deformation and dynamic mechanisms of the bayan har foreland basin in the yinshishan region , qinghai
  青海银石山地区巴颜喀拉前陆盆地构造变形特征及动力学机制
• This area was controlled by four large - scale faults : south kunlun suture , jinsshajiang suture , bangonghu suture and yaluzangbu suture . this area has undergone polymetamorphism and deformation and at least three periods of magmatism . continuous activities of magmatism , metamorphism were mainly controlled by collision of the terranes
  _ 1 ： 240 - ( ) 220ma ，巴颜喀拉洋壳向昆仑地体俯冲，以昆仑岩带和阿尼玛卿岩带中cag型岩浆侵位为标志；阿尔金剪切作用发生。
• Combining the isotope geochronological results with the fieldwork observations , we could draw some conclusions as follows : the kunlun - bayan har terranes experienced the subduction of oceanic crust and collision somewhat earlier than the bayan har - qiangtang terranes , with only a very short interval in between and even the collisions overlapped partially in time
  _ 2 ： 227 - 218ma ，巴颜喀拉和羌塘之间洋壳俯冲，以金沙江岩带iag型岩浆侵位为标志。 _ 3 ： 217 - 212ma ，造山后期岩浆侵位。
• In the northern part , the oceanic crust occurring between the bayan har and kunlun terranes started subduction from south to north at about 243 ma , and did not stop until the development of post - orogenic pog - type granite in the bayan har terrane at 220 ma , thus illustrating the orogeny in the form of subduction and collision kept active for over 20 ma
  以pog型花岗岩在巴颜喀拉地体内大量生成、在阿尼玛卿岩带中较多出现、在昆仑岩带利金沙江岩带少量出现为标志。期： 160 - 140ma ，断裂系活动；金沙江、东昆仑剪切作用发生；部分岩体动力变质变形。
• Through the analysis of subsidence history in the north of western ordos basin , as a result of the terranes northward accretion and the successive collision of the baykala block in the middle triassic , the qiangtang block in the late triassic , the lhasa block in the middle jurassic , the gangdese block in the cretaceous and the subduction of izanagi plate in yanshanian period , the studied region became a intracontinental foreland basin from late triassic to cretaceous
  摘要通过对鄂尔多斯盆地西缘北段沉降史的分析可知，晚三叠世白垩纪，由于中三叠世巴颜喀拉地体、晚三叠世羌塘地体、中晚侏罗世拉萨地块、白垩纪冈底斯地体连续向北增生、碰撞以及燕山期伊佐奈岐板块的俯冲，盆地西缘北段的响应显示为陆内前陆盆地的特征。
• In the link party of qinling - qiliang - kunlun belt , the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin . the bayan har basin thought to be the preexistence of the songpan - garze belt , is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic . the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ) , then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic
  在秦祁昆仑结合部研究中，加强和突出了精细的岛弧盆分析和造山作用关系的研究，探讨了秦、祁、昆结合部多岛弧盆特征；通过巴颜喀拉地区沉积特征，沉积体的空间展布和形态，面式物源供给方式，矿物成分和地球化学背景分析，其沉积盆地属性总体上反映出一个从过渡地壳-洋壳基础上发育起来的周缘前陆盆地的发展和演化过程。