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isostasy
Noun
sự cân bằng đẳng tĩnh, trạng thái cân bằng đẳng tĩnh
the gravitational balance between Earth's rigid lithosphere and the underlying, semi-fluid asthenosphere, influencing variations in surface elevation
"Isostasy is a fundamental principle in geophysics, guiding our understanding of the dynamic balance between Earth's rigid and fluid layers."