南安普敦大学的一项研究发现,地壳板块碎裂导致地球深波,影响大陆升高、气候、生物多样性和人类住区模式。 A University of Southampton study finds that tectonic plate breakup causes deep Earth waves, influencing continental uplift, climate, biodiversity, and human settlement patterns.
南安普敦大学的一项新研究显示,当构造板块破裂时,地球深处的强波导致大陆表面上升一公里以上。 A new study by the University of Southampton reveals that when tectonic plates break apart, powerful waves deep within Earth cause continental surfaces to rise over a kilometer. 这些波浪是板块碎裂期间大陆地壳延伸引发的,扰乱了地球的地壳和影响因素,如区域气候、生物多样性和人类住区模式。 These waves, triggered by stretching of the continental crust during plate breakup, disturb Earth's mantle and influence factors such as regional climates, biodiversity, and human settlement patterns. 以前稳定的大陆地区已被发现受到大幅度的提升和侵蚀,形成称为高原的高原高地。 Previously stable continental areas have been found to undergo substantial uplift and erosion, forming elevated regions known as plateaus. 调查结果显示,同样一系列的动乱造成钻石从地球深处上升,在形成大陆地貌方面也发挥了重要作用。 The findings demonstrate that the same chain of disturbances that cause diamonds to rise from Earth's deep interior also play a significant role in shaping continental landscapes.