A special issue of Palaeogeography in Xinjiang

• 出 处: 新疆地质
• 发表日期: 2000年04期
• 关键词: Tianshan carbonate facies Silurian Ordovician volcanic shallow sedimentary Carbo

Since Archaean Xinjiang Continental Block has experienced a process of divergence convergence cracking and spliting． The crustal movements and tectonic frameworks caused by the process directly controlled the variation of the palaeogeographic environ

Since Archaean Xinjiang Continental Block has experienced a process of divergence convergence cracking and spliting. The crustal movements and tectonic frameworks caused by the process directly controlled the variation of the palaeogeographic environ