Zircons from ultra-high pressure (UHP) metamorphic metabasite and metafelsic rock in Dabie orogen were investigated by cathodoluminescence and Laser Raman spectrometry.
利用阴极发光和激光拉曼研究了大别山俯沖带超高压基性和长英质变质巖中的锆石。
Sediments in the Hefei basin to the north of the Dabie orogen are important records of unroofing history for the orogen.
位于大别造山带北部的合肥盆地,其中的沉积是造山带剥露历史的重要记录。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。