节点文献
内蒙古中西部多岛海构造演化
ISLANDS-OCEAN STRUCTURAL EVOLUTION OF MID-WESTERN CONTINENT IN INNER MONGULIA
【摘要】 内蒙古中西部大陆由一个微大陆、三条弧后盆地和三条火山岛弧,即华北微大陆、白云鄂 傅弧后盆地、白乃庙火山岛弧、温都尔庙弧后盆地、苏尼特左-锡林浩特火山岛弧、贺根山弧后盆 地和二连浩特-锡林郭勒火山岛弧组成。经过了长期而复杂的微大陆和火山弧的裂解、弧后盆地 的消减衰亡及弧-陆和弧-弧碰拉等构造演化,才最终形成今天所见到的这种构造样式。
【Abstract】 The continent in mid-westhern Inner Mongolia is composed of a microcontinent, three volcanic island arcs and three back-arc basins, which are North China microcontinent, Baiyun Obo back-arc basin, Bainaimiao volcanic island arc, Wendurmiao back-arc basin, Sunitezue-Xilinhaote volcanic island arc, Hegenshan back-arc basin and Erlianhaote-Xilinguole volcanic island arc respectively. At last they have being formed the tectonic framework, after breakup of the volcanic island arcs, subduction, decline and fall of the back-arc basins and arc-microcontinent and arc-arc collision had finished.
【Key words】 Islands-ocean structural; microcontinent; volcanic island arc; back-arc basin; ophiolite melange zone;
- 【文献出处】 大地构造与成矿学 ,Geotectonica Et Metallogenia , 编辑部邮箱 ,2001年04期
- 【分类号】P542
- 【被引频次】47
- 【下载频次】380