The geology of this part of the Andes is a result of the eastward subduction of the Nazca tectonic plate underneath South America.
该区域安第斯山脉的地质结构是纳斯卡板块向东俯冲,下穿垫在南美版块之下。
Per the Zetas, this was due to the nature of the plate adjustments, which involved subduction, a lateral movement, rather than rising or falling land under water.
根据齐塔人的说法,这取决于板块调整的横向运动和俯冲特性,而不是海底发生了升降。
Subduction and collision theory of Plate tectonics is a basement of the study of granite tectonic dyna mics and geodynamics.
板块俯冲碰撞理论曾是花岗岩构造动力学、地球动力学研究的主线。
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