冈瓦纳古陆

地球旋转膨胀与冈瓦纳古陆裂解

The Expansion of the Rotating Earth and the Breakup of Gondwanaland

兽脚类主要产自远古的南方大陆&冈瓦纳古陆。

Theropods are mainly known from the ancient southern landmass , Gondwana .

青藏古特提斯蛇绿岩与冈瓦纳古陆北界亚洲特提斯域岩相古地理与油气聚集地质特征

Geological Characteristics of Lithofacies Paleogeography and Hydrocarbon Accumulation in Asian Tethyan Tectonic Domain

冈瓦纳古陆与太平洋古陆在中国西南部的分界及其相关地体的缝合时代

Boundary between Gondwana and Pacifica and suture age of allied terranes in southwestern China

澜沧江以西的白垩系，分布于冈瓦纳古陆和古特提斯造山带的小型山间盆地，地层层序齐全，岩性、厚度稳定，含古生物化石。

The Cretaceous west of Lancang River is distributed in Gondwana and the small intermontane basin of Tethys orogen .

摘要：埃塞俄比亚北部位于西冈瓦纳古陆北缘，是阿拉伯-努比亚地盾西南部新元古代岛弧增生带的重要组成部分。

Abstract : North of Ethiopia , located in the northern margin of west Gondwana , is an important part of Arabia-Nubian shield southwest Neoproterozoic arc accretionary zones .

摘要：尕龙格玛铜多金属矿床位于特提斯-喜马拉雅构造域的东段，冈瓦纳古陆与欧亚古陆强烈碰撞、挤压地带。

Abstract : Galonggema Cu-polymetal deposit is located in the eastern of the Tethys-Himalayan tectonic domain , which is the strong collision and extrusion zone between Gondwana and Eurasian ancient land .

根据化石记录及现代分布推断，无患子科可能在白垩纪早期起源于冈瓦纳古陆，对其可能的散布途径作了图解。

Based on the evidence of microfossils and modern distribution pattern of the family , it can be concluded that the family was possibly originated on Gondwana in very early Cretaceous , and its dispersal pathway is schematized .

随着时间的推移，冈瓦纳大陆与其他古陆分离，形成了今天的陆地格局。

Over time , Gondwana and other ancient landmasses broke up , forming the continents we see today .