摘要
文章将龙门山地区泥盆系划分为四个沉积旋回,即四个地层层序,建立了该区泥盆纪海相碳酸盐锶、碳同位素地层曲线,并将同位素演化与沉积旋回结合起来研究该区泥盆纪的海平面变化。
This paper divided Devonian strata of the Longmen Mountain into four sedimentary cycles or four sequences and established Sr and C isotope stratigraphic curves for marine carbonates of Devonian. The sea level fluctuation of Devonian can be studied according to the combination of isotope evolution and sedimentary cycles.
基金
国家自然科学基金
关键词
同位素
海平面变化
泥盆纪
锶
碳
isotope, sea level fluctuation, sedimentary cycle, Devonian, Longmen Mountain
