研究表明,冈瓦纳的裂散、亚洲的增生和特提斯构造带的演化都受控于星球级纬向构造体系。
Study indicates that Gondwana dispersion, Asian accretion and geological evolution of the Tethyan tectonic belt were controlled by the global latitudinal tectonic system.
岩石地球化学示踪和地层学研究表明,冈底斯带石炭纪为伸展背景下的冈瓦纳陆缘裂陷环境。
Geochemical and stratigraphical studies suggest that the tectonic setting of the Gangdese region is depressional rifting to the northern margin of Gondwanaland.
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