新特提斯 meaning in Chinese
neo-tethys
Examples
- Is there a neo - tethys subduction record earlier than arc volcanic rocks in the sangri group
存在比桑日群弧火山岩更早的新特提斯洋俯冲记录么 - The internal mineral separates and whole - rock sm - nd isochron age for gabbro dikes from the dangqiong ophiolite is 373 ? 8ma , inferring a magmatic activity during late devonian , which end ( t ) = + 3 . 3 suggests that its tectonic setting was probably oceanic island
其nd ( t ) = + 3 . 3 ，认为其时形成环境为洋岛，可能代表了新特提斯蛇绿岩形成时所携带的古老洋壳。 - The authors put forward that daba - xiugugabu ophiolite belt originated from an ancient oceanic crust fragment of india continental northern marginal ocean basin , that was approximately synchronous with the formation and evolution period of the neo - tethys ocean
笔者提出该区蛇绿岩来源于印度大陆北缘洋盆的洋壳碎片，这个陆缘洋盆与新特提斯洋主体的形成和演化准同步。 - During subduction northward of neo - tethys oceanic plate , ayla - zhongba micro - continental , the marginal ocean basin and india continental drifted northward all together , the marginal ocean basin was gradually contracted and closed by compressed of india continental
在新特提斯洋板块向北俯冲消减过程中，阿依拉仲巴微陆块、陆缘洋盆和印度大陆一起随着向北漂移，在印度大陆向北挤压作用下洋盆逐渐收缩以致最终闭合。 - The main continent rift developed in mid - late proterozoic ; the paleo - asian tectonic dynamic system played an important role in the paleozoic period ; the combination of tethys - paleopacific tectonic dynamic system influenced the basin in mesozoic . during that period , the tethyan dynamic system affected the basin in the early stage ( t ) while paleo - pacific dynamic system affected it in the latter stage ( js - k ) ; the new tethyan - circum pacific tectonic dynamic system dominated in cenozoic period
中新元古代为大陆裂谷集中发育阶段；古生代主要受控于古亚洲构造动力学体系；中生代主要受控于中特提斯?古太平洋构造动力体系的联合作用和影响，其中早期( t )主要受特提斯动力体系影响，晚期( j _ 3 - k )主要受古太平洋动力体系影响；新生代主要受控于新特提斯?今太平洋构造动力体系的联合作用和影响。