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Laurasia相关的网络例句

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与 Laurasia 相关的网络例句 [注:此内容来源于网络,仅供参考]

Later, the first occurrence of a large-scale orogeny, the campaign it is now called the Yanshan movement, the essence of it is the beginning of the ancient Pacific plate subduction to Laurasia.

于是中国东部的陆地在古太平洋的挤压下隆起成为高山和高原,于是这段时期中国的河流基本上都是从东部发源,向西注入古忒提斯洋。

The freshwater ichthyofaunas mainly from northern China are characterized by primitive actinopterygians,and they are closest to those from Siberia and Middle Asia,and also contain some forms similar to the fishes from other regions of Laurasia and the Gondwanan continents.

与当时"南海北陆"的古地理格局一致,淡水鱼类主要分布于北方大陆的河湖相盆地,但也见于扬子板块与北方大陆碰撞后的四川盆地;海生鱼类则主要分布于华南和喜马拉雅地区。

Except for HIMU-type OIB with negativeΔ7/4 ratios in the Wandashan massif, all other rocks have positiveΔ7/4 andΔ8/4 values, a feature of the Laurasia continent in the Northern Hemisphere.

除完达山外来拼贴地体的HIMU型OIB具有负的△7/4值,东北地区中生代火成岩都为正的△7/4和△8/4值,显示出亲北方劳亚大陆的岩石圈属性。

2It is presumed according to the distribution patterns of Aletris L. and itsgenetically close genera that Aletris L. probably originated in Laurasia not later than the early tertiary.

2根据粉条儿菜属及其近缘属的分布格局推测,该属可能在不晚于第三纪早期,起源于古北大陆。

The Changning-Menglian belt located in western Yunnan of the Sanjiang fold belt in the Himalayan tectonic region of the Tethys is one of the important areas of studing and resolving many significant geological problems, like the nature、scale、 geological evolution、and ore-forming process of the paleo-Tethys and the boundary between Gondwana and Laurasia、etc., It has been always drawn close attention of geologists.

昌宁-孟连带位于特提斯喜玛拉雅构造域三江褶皱带,是研究和解决古特提斯性质、规模及地质演化、成矿作用及冈瓦纳与劳亚古陆分界等重大地质问题的重要地区之一,历来为地质学家所关注和研究。故滇西古特提斯昌宁-孟连带沉积地质研究对解决上述问题有着十分重要的意义。

Kazakhstan is located in the north of Central Asia, belonging to the southern margin of Laurasia, i.e., the southern margin of Craton and Kazakhstan plates in East Europe. Late Paleozoic continental margin basins, such as the Pre-Caspian Basin, are formed in the region.

哈萨克斯坦位于中亚地区北部,大地构造上属于劳亚大陆南缘,即东欧克拉通和哈萨克板块南部边缘,形成晚古生代大陆边缘盆地,如滨里海盆地。

Except for HIMU-type OIB with negativeΔ7/4 ratios in the Wandashan massif, all other rocks have positiveΔ7/4 andΔ8/4 values, a feature of the Laurasia continent in the Northern Hemisphere.2 In the southern Hinggan Mountains distributes a Cretaceous felsic igneous rock belt characterized by highly positive-ε_ T_(DM = 0.42~0.64Ga,ε_ =+4.0~+5.9 and radiogenic Pb ~(206Pb/~(204)Pb = 18.36 ~ 18.56 isotope compositions.

除完达山外来拼贴地体的HIMU型OIB具有负的△7/4值,东北地区中生代火成岩都为正的△7/4和△8/4值,显示出亲北方劳亚大陆的岩石圈属性。2在大兴安岭南区林西-霍林河地区存在一条近似平行索伦-贺根山-小兴安岭古缝合带的高ε_早白垩世中酸性火山岩组合。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1:25万地质填图进一步揭开了青藏高原地区大地构造的奥秘:阿尔金山是昆仑,祁连-秦岭造山系的一部分;阿尔金断裂确是一条大型转换断层;木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带;松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地;冈底斯带曾经历了重要的印支造山运动;不存在从古生代延续到三叠纪的大洋盆地,即不存在所谓古特提斯或永久特提斯;古生代时期,在青藏高原地区亦不存在具古生物,古地理分隔意义的大洋盆地,当时,包括中朝,扬子,塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南,属冈瓦纳大陆结构复杂的北部边缘;雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹,它们均是从三叠纪起就发展成大洋裂谷带的;以雅鲁藏布江带为主洋盆带的特提斯洋,从三叠纪晚期开始消减,经历了印支,燕山,喜马拉雅3个阶段脉动式板块汇聚造山过程。

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