The study on the sequence stratigraphy of Yanchang formation of Triassic in Ordos basin shows that there exist sedimentary slope break in margin of ramp belt of the basin.
通过对鄂尔多斯盆地三叠系延长组层序地层研究发现,在盆地的缓坡边缘发育沉积坡折带。
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