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“长江中下游转换构造结”是特提斯构造体制与太平洋构造体制交汇、衔接和转换的焦点部位,主要包括大别造山带、郯庐断裂带、长江中下游成矿带三大著名的构造单元,是中国东部中新生代大陆动力学深部过程与浅表响应的经典地区。将大陆造山带、大型断层、矿集区结合起来,瞄准板内变形、运动学和动力学,建立区内大陆动力学的系统研究框架,研究两大构造体制转换的精细过程,分析陆内构造演化和动力学的深部过程与浅部效应,将有助于大陆动力学理论的新突破,指导“第二成矿空间”的深部找矿。
“The structural transformation of the middle and lower reaches of the Yangtze River” is the focal point for the convergence, convergence and transformation of the Tethys structural system and the Pacific tectonics, and includes the Dabie orogenic belt, the Tanlu fault zone and the three famous metallogenic belt in the middle and lower reaches of the Yangtze River The tectonic unit is a classic area of Mesozoic and Cenozoic continental dynamics in eastern China. Combining the continental orogenic belts, large-scale faults and ore-concentrating areas, aiming at the deformation, kinematics and dynamics in the plate, a systematic framework for the study of the continental dynamics in the area is established. The fine process of the conversion of the two structural systems is studied, The deep processes and shallow effects of evolution and dynamics will help the continental dynamics theory to make new breakthroughs and guide the deep prospecting of the Second Metallogenic Space.