摘要
从青藏板块中发现的石炭纪含砾冰水沉积与桉属植物群的分布对比研究,认为青藏板块仍属南大陆范畴。青藏板块复杂多变,活动强烈,是现代造山运动的结果。
Pebble-bearing glaciofluvial deposit and eucalyptus florizone in the Carboniferous in the Qinghai-Tibet plate indicate that the Qinghai-Tibet plate belongs to the Gondwana land.The Qinghai-Tibet plate is characterized by strong activity due to the recent orogeny.
出处
《四川地质学报》
2009年第S2期56-57,共2页
Acta Geologica Sichuan