paleo-tethys

基本解釋

Based on above data and previous study KSTB is regarded as a right-hand shove transform tectonic belt which divides the paleo-Asian tectonic domain and the Tethys domain.
綜合以上資料及前人的研究成果認(rèn)為，康西瓦構(gòu)造帶是分隔古亞洲和特提斯兩大構(gòu)造域的右行走滑轉(zhuǎn)換構(gòu)造帶。
If the hypothesis that the Yangtze plate was separated from the Tarim plate and migrated eastward in the Permian can hold, it can serve as evidence for the first opening of Paleo-Tethys in China.
揚(yáng)子板塊在二疊紀(jì)與塔里木板塊離散并向東漂移的論斷若能成立，則為古特提斯在中國境內(nèi)首先打開提供依據(jù)；
This discovery has great significance for the understanding the process of the ocean-land transformation of the Paleo-Tethys.
這一發(fā)現(xiàn)對(duì)認(rèn)識(shí)古特提斯洋-陸轉(zhuǎn)化過程具有重要意義。

古特提斯
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.
本文主要研究了金沙江帶的蛇綠混雜巖、島弧火山巖和裂谷火山巖的地質(zhì)、地層和地球化學(xué)特征并對(duì)金沙江古特提斯演化模式提出了多次裂開、多次俯沖的多島洋體系模式。