古特提斯洋
- 网络Paleo-Tethys Ocean;Prototethys;Paleo-Tethys;Paleotethys
古特提斯洋-
泥盆纪时期，随着古特提斯洋的开启，于华南板块南、西、北缘形成被动陆缘构造背景。
The passive continental margina are formed in southern , western and northern margins of Huaxia Plate during Devonian because of the opening of Old Tethys .
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这套海相中生代地层的存在对解释南海北部中生代大地构造演化以及古特提斯洋和太平洋的关系具有重要意义。
The existence of these Mesozoic marine strata is very important for interpreting the tectonic evolution of this region and the influence of the Tethys tectonic domain on the Pacific tectonic domain during the Mesozoic .