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   冰川漂砾 的翻译结果: 查询用时:0.013秒
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冰川漂砾
相关语句
  glacial boulder
     DISCOVERY AND SIGNIFICANCE OF A HUGE GLACIAL BOULDER IN GEXIANSHAN, PENGZHOU, SICHUAN
     四川彭州葛仙山巨型冰川漂砾的发现及意义
短句来源
     A huge glacial boulder has been found at Gexianshan, Pengzhou, Sichuan. It, about 6 km×2.5 km×0.3 km in area, is a rare huge glacial boulder discovered up to now in the world. This huge boulder is distributed about 3 4 km along the margin of the Sichuan basin.
     四川彭州市葛仙山巨型冰川漂砾距四川盆地边缘地带约3~4km,规模巨大(约6km×25km×03km),是目前世界上发现的罕见巨型冰川漂砾
短句来源
  “冰川漂砾”译为未确定词的双语例句
     GIANT GLACIAL BOULDERS IN PENGZHOU-SHIFANG SECTION OF THE LONGMEN MOUNTAINS
     龙门山彭州—什邡地区的巨型冰川漂砾
短句来源
     Reconstructing the History of Drift Boulders' Movement by Using the Autochthonous Cosmogenic Isotope ~(10)Be
     利用陆面岩石中生成的宇生同位素重建冰川漂砾运动历史的尝试
短句来源
     Discovery of Flat Revolving Ellipsoid Glacier Boulder in Sichuan,China
     四川九寨沟县甘海子发现“扁平椭球体状冰川漂砾
短句来源
     The ages of drift boulders are usually very difficult to be dated directly, and it is harder to know whether the boulders have been re-transported or rolled over since their formation.
     冰川漂砾的形成年代通常难以直接测定,并且漂砾形成以后是否被再次搬运或者移动过,更是无法知道。
短句来源
     Based on the measurement and analyses of the cosmogenic isotope 10Be of a drift boulder, which is located in the vicinity of Haizishan in the southeastern margin of the Qinghai-Tibet Plateau, we may conclude that the boulder was formed during the glacial stage before the last (186~128 ka BP) and was re-transported and rolled over during the last glacial stage.
     本文以石英中生成的宇生同位素~(10)Be,对青藏高原东南部海子山的冰川漂砾进行了探讨,结果表明该砾石形成于倒数第二次冰期(186~128 ka BP之间),在末次冰期中再次被冰川搬运,使之反转。
短句来源
  相似匹配句对
     Glacier of the Qilian Mountain
     祁连山冰川
短句来源
     Glacier Masterpieces
     冰川杰作
短句来源
     DISCOVERY AND SIGNIFICANCE OF A HUGE GLACIAL BOULDER IN GEXIANSHAN, PENGZHOU, SICHUAN
     四川彭州葛仙山巨型冰川漂砾的发现及意义
短句来源
     GIANT GLACIAL BOULDERS IN PENGZHOU-SHIFANG SECTION OF THE LONGMEN MOUNTAINS
     龙门山彭州—什邡地区的巨型冰川漂砾
短句来源
     DISCOVERY AND SIGNIFICANCE OF BOULDERS IN CARBONIFEROUS COAL SEAM IN CHAOYANG MINE AREA,LIAONING PROVINE
     朝阳石炭系煤层中的漂砾
短句来源
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  glacial boulder
Here the chalk disappears under a thick layer of glacial boulder clay deposited during the Anglian glaciation around 400,000 years ago.
      
The chalk is overlain in places by glacial boulder clay and in areas the chalk has been eroded to expose older non-calcareous Cretaceous rocks.
      


Carboniferous strata are widely distributed and well developed in western Yunnan,

云南西部石炭系特别发育,自上而下可分为上石炭统卧牛寺组、丁家寨组,下石炭统铺门前组和香山组,中石炭统缺失。丁家寨组下部为滨海相杂砾岩,其中一部分砾石为冰川漂砾,中部属正常冰川-海洋相沉积,含冷水动物群化石,冰川砾石面上具擦痕、压裂和凹坑等;上部含(竹蜒)科化石,气候已由寒冷变为温暖。

A huge glacial boulder has been found at Gexianshan, Pengzhou, Sichuan. It, about 6 km×2.5 km×0.3 km in area, is a rare huge glacial boulder discovered up to now in the world. This huge boulder is distributed about 3 4 km along the margin of the Sichuan basin. Study of available data indicates that it was formed by transportation of the ice flow of the early Pleistocene Qinghai Tibet great ice sheet. It is one of the convincible evidences for the existence of the Qinghai Tibet great ice sheet as well as an...

A huge glacial boulder has been found at Gexianshan, Pengzhou, Sichuan. It, about 6 km×2.5 km×0.3 km in area, is a rare huge glacial boulder discovered up to now in the world. This huge boulder is distributed about 3 4 km along the margin of the Sichuan basin. Study of available data indicates that it was formed by transportation of the ice flow of the early Pleistocene Qinghai Tibet great ice sheet. It is one of the convincible evidences for the existence of the Qinghai Tibet great ice sheet as well as an important historic witness for the formation of the global pan ice sheet. This huge glacial boulder provides a new idea, a new way and a new method for the study of fundamental theories of numerous related borderline disciplines.

四川彭州市葛仙山巨型冰川漂砾距四川盆地边缘地带约3~4km,规模巨大(约6km×25km×03km),是目前世界上发现的罕见巨型冰川漂砾。现有资料研究结果表明,葛仙山巨型漂砾是早更新世青藏大冰盖冰流的搬运作用所形成的。是青藏大冰盖存在的有力证据之一,也是全球泛大冰盖形成的重要历史见证。同时对众多相关边缘学科的重大基础理论问题的研究,提供了新的思路、途径和方法

After the discovery of a planty of glaciated pots in Chifeng City,Inner Mongolia,in Great Hinggan Mountains and its both side area geomorphological types formed by glacial erosion and moraine are studied based on the deciphering of remote sensing image.It is found that most of glacial pots,distributed on giant glacial boulder,sheepback rock or rock drumlin,resulted from that in Huanggangliang Mountai,Qilaotu Mountain,Damatushan Mountain southern end of the sheet was obstructed,rotated and dispersed when Mongolia...

After the discovery of a planty of glaciated pots in Chifeng City,Inner Mongolia,in Great Hinggan Mountains and its both side area geomorphological types formed by glacial erosion and moraine are studied based on the deciphering of remote sensing image.It is found that most of glacial pots,distributed on giant glacial boulder,sheepback rock or rock drumlin,resulted from that in Huanggangliang Mountai,Qilaotu Mountain,Damatushan Mountain southern end of the sheet was obstructed,rotated and dispersed when Mongolia giant glacial sheet of movement toward the south overpassed the Great Hinggan Mountains.

在赤峰境内发现大量冰臼和冰臼群后,利用遥感图像对大兴安岭及其两侧的冰蚀、冰碛地貌类型进行解译发现:它们中的绝大多数原本在巨型冰川漂砾、羊背石或基岩鼓丘上。它们是蒙古大冰盖之一部分在沿东南方向越过大兴安岭时其南端受到黄岗梁、七老图山、大马群山的分流、阻隔、旋转的必然结果

 
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