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Mianluee tectonic zone and Mianluee suture zone on southern margin of Qinling-Dabie orogenic belt

机译:秦大别造山带南缘的绵鹿构造带和绵鹿缝合带

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摘要

The Mianluee tectonic zone (Mianluee zone), an ancient suture zone in addition to the Shangdan suture in the Qinling-Dabie orogenic belt, marks an important tectonic division geologically separating north from south and connecting east with west in China continent. To determine present structural geometry and kinematics in the Mianluee tectonic zone and to reconstruct the formation and evolution history involving plate subduction and collision in the Qinling-Dabie orogenic belt, through a multidisciplinary study, are significant for exploring the mountain-building orogenesis of the central orogenic system and the entire process of the major Chinese continental amalgamation during the Indosinian.
机译:绵鹿构造带(绵鹿带)是秦岭—大别造山带上丹缝合线以外的一个古老的缝合带,是中国大陆上北北南北连接的重要构造分区。通过多学科研究,确定绵鹿构造带目前的构造几何学和运动学,并重建秦岭-大别造山带板块俯冲和碰撞的形成和演化历史,对于探索中部山地造山运动具有重要意义。造山系统和印支期中国大陆主要融合的全过程。

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