文中系统综述了板块构造启动时间的不同观点及其依据,并探讨了板块构造启动的三个必备条件:刚性岩石圈、俯冲作用、地幔对流循环的起源,进而探讨了前寒武纪俯冲作用、板块构造体制与现代俯冲作用、板块体制的差异。板块构造体制启动的三个缺一不可的条件:刚性、俯冲和地幔对流,直到27-21亿年期间才在全球不同地点同时满足。但现代板块构造体制起始的时间为10(或19)-8(或6)亿年,其标志性物质记录或识别标志依然是蛇绿岩建造、高压-超高压变质、岛弧型岩浆建造等。最后,系统描述了板块构造可能的启动机制和过程,为认识前板块构造和板块构造差异提供一个约束,也为推动地球动力学统一理论的思考和探索提供一些最新认识。
This paper summarizes different views and their corresponding evidence of the starting time of plate tectonics,and explores three requirements of starting plate tectonic system:rigid plate,subduction and mantle convection,and then further discusses the differences between the Precambrian subduction or plate tectonics regime and modern-style subduction or plate tectonics regime.The three requirements of starting plate tectonic system met at the same time until during 2.7-2.1Ga in different places around the world.But the modernstyle plate tectonic system and regime have a starting time of between 1.0(or 1.9)to 0.8(or 0.6)Ga;the remarked material records or identification markers are still ophiolite suites,HP-UHP metamorphic rocks,and arc magmatic rocks.At last,we describe possible starting mechanisms and processes of plate tectonics to provide a constraint for understanding the differences of pre-plate tectonics and plate tectonics,and to provide some latest insights for promoting thoughts and explorations of a unified theory of geodynamics as well.