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缝合带的英文

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"缝合带"怎么读用"缝合带"造句

英文翻译手机手机版

  • suture zone
  • suturezone

例句与用法

  • The eqm can be subdivided into the northern and southern parts , which are separated by the shangnan - zhenping suture
    东秦岭以商南镇平缝合带分为东秦岭北部和东秦岭南部。
  • The bayan bold gold deposit is situated in the obduction zone of platform margin to the north of inner mongolian suture zone
    摘要白音宝力道金矿床位于内蒙古古缝合带北侧的陆缘逆冲带内。
  • There are two suture zones in beishan area : the hongliuhe - niujuanzi - xichangjing suture zone ( early paleozoic era ) and the hongshishan - pengboshan suture zone ( upper paleozoic era ) , and the latter is the final plate junction between the tarim plate and kazakhstan plate
    认?本区先后存在红柳河牛圈子洗肠井(早古生代)和红石山百合山蓬勃山(晚古生代)两条缝合带,后者是哈萨克斯坦与塔里木板块的最终缝合带。
  • According to the characteristics of strata , tectonization and magmatism within the research area in the southwest margin of north china paleocontinent , and under the ideological guidance of mobilism and systematology , the geotectonic framework of the area could be divided as follows : ( 1 ) the longshoushan mountains continental margin ; ( 2 ) the hexi corridor back - arc basin ; ( 3 ) the northern qilianshan mountains suture zone ; ( 4 ) the central qilianshan mountains dispersion type island arc terrane ; ( 5 ) the southern qilianshan mountains back - arc basin ; ( 6 ) the qaidam massif
    根据本区地层、构造、岩浆作用特点,在“系统论” 、 “活动论”思想指导下,厘定华北古大陆西南边缘的构造格局如下:龙首山陆缘带、河西走廊弧后盆地、北祁连缝合带、中祁连离散型岛弧地体、南祁连弧后盆地、柴达木地块。
  • The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone , and once extended northwards and southwards , respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous . ( 1 ) during the middle - late jurassic , the rift zone was occupied by deep - water turbidites , radiolarian siliceous rocks , shallow - water carbonate rocks , clastic rocks and basic - ultrabasic rocks , while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks
    摘要位于班公湖怒江缝合带与雅鲁藏布江缝合带之间的措勤盆地,在中侏罗世早白垩世期间具有以且坎古昌阿索裂谷带为沉积、沉降中心向南北两侧展开的古地理格局:中晚侏罗世时期,裂谷带内由深水浊积岩、放射虫硅质岩和浅水碳酸盐岩、碎屑岩岩片及基性超基性岩等组成;裂谷带两侧由滨浅海相碎屑岩和碳酸盐岩组成。
  • Based on the geological , stratigraphic and geochemical characteristics of the ophiolitic melange , island - arc and rift volcanic rocks from the jinshajiang zone , an archipelagic tectonic model with multi - rift and multi - subduction is proposed to explain the evolution of jinshajiang paleo - tethys . the ophiolitic melanges of the jinshajiang zone are mainly outcropped at baimangxueshan , tongduo , gongka , dongzhulin and jiyidu in the deqin county . the geochemistry of major and trace elements of the jinshajiang ophiolite shows its geochemical characteristics are similar to those of the more and island - arc volcanic rocks , but different from those of the typical n - mopjb
    金沙江蛇绿混杂岩主要分布在德钦县的白茫雪山、通多、共卡、东竹林和吉义独地区,主量和微量元素地球化学特征研究表明,金沙江蛇绿岩不具有典型n - morb的地球化学特征,而具有介于morb和岛弧之间的地球化学特征,暗示它并非形成于宽阔的大洋环境,不是古特提斯在滇西北地区的主缝合带,可能是古特提斯多岛洋体系中的一个弧后盆地。
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