在亚洲，新特提斯洋直至始新世才完全闭合，导致喜马拉雅造山带拼合到亚洲大陆南缘，后经强烈抬升形成现今宏伟的青藏高原。近年来有的学者认为印度大陆与欧亚大陆之间不存在广阔的新特提斯大洋。
新特提斯洋 Neo-Tethys
We argue that the Neo-Tethys began northward subduction in the Early Jurassic to Late Triassic time and closed in the Late Cretaceous time,thus causing ophiolite tectonic emplacement.
笔者认为新特提斯洋在晚三叠世至早侏罗世发生向北的俯冲消减,在晚白垩世闭合,蛇绿岩构造侵位。
参考来源 - 喜马拉雅东构造结地区雅鲁藏布江蛇绿岩地质年代学研究·2,447,543篇论文数据，部分数据来源于NoteExpress
存在比桑日群弧火山岩更早的新特提斯洋俯冲记录么?。
Subduction Record Earlier than arc volcanic rocks in the Sangri Group?
研究表明，三江中段新特提斯阶段区域流体存在两个性质不同的流体作用区域。
The result shows that there were two different fluid flow areas in "Sanjiang" middle belt during Neo Tethys.
伊朗盆地是在中新生代受古特提斯洋与新特提斯洋的扩张闭合控制下形成的被动大陆盆地。
The Iran basin is a passive continental basin formed in Meso-Cenozoic under the control of the extensional closing of Paleotethys and Neo-tethys oceans.
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