1) Eastern Asian Paleocontinent
东亚古陆
2) Laurasia continent
劳亚古陆
1.
The numerical range of the Pb isotopic composition and the spatial distribution of the two types of samples can be correlated with those of Gondwana and Laurasia continents.
根据铅同位素组成，西南三江地区前中生代的碳酸盐岩可分成具高放射性和低放射性成因铅同位素特征的两种类型，其数值范围和样品的空间分布都可分别与已知的冈瓦纳和劳亚古陆群的铅同位素组成对比。
3) East Asian continent
东亚大陆
1.
Based on paleomagnetic, paleo-biogeographic and geotectonic analyses, the East Asian Continent moved in large extent to the south direction during the Middle and Late Mesozoic to Early Cenozoic, but it moved in large extent to the north since Middle and Late Cenozoic.
根据古地磁、古生物地理和地质构造分析，东亚大陆在中生代中晚期至新生代初期大幅度向南运动；新生代中晚期以来大幅度向北运动。
4) East Asia continental margin
东亚陆缘
5) East Asia continent
东亚大陆
1.
The Indian plate′s continuous motion to the north, the convective removal to the thickening lithosphere caused by small-scale mantle convection and the effect of denudation on the uplifted plateau are regarded as main driving forces that make the patterns of stress field of East Asia continent at present time.
将印度板块持续地向北推进、下伏地幔小尺度对流对增厚大陆岩石层的搬离作用以及剥蚀作用视为形成现今东亚大陆形变和应力场格局的主驱动力 。
2.
The East Asia continent was assembled by a lot of micro-continents during the Indosinian period (250-220 Ma), producing very thick lithosphere.
东亚大陆是在印支期(250～220Ma)由诸多微陆块拼接而成,曾形成巨型的岩石圈(根)。
6) Pal-Asia
古亚洲大陆
补充资料：古陆
craton
大陆的最古老部份，自从先寒武纪时期以来从没有再受过剧烈地壳变动的影响。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条