interglacial deposit

基本解釋

Although loess deposition started as early as in the Middle Pleistocene, most of the loess deposit in the eastern part of the plateau was deposited since the last interglacial.
研究區(qū)黃土沉積雖始于中更新世，但目前分布最廣泛的黃土沉積主要是末次間冰期以來的產(chǎn)物。
The gravels in deposits of different glacial epochs and interglacial stages show obviously different rock characteristics, gravel forms, deposit thicknesses and weathering degrees.
每次冰期及間冰期沉積物中的礫石及其巖性，礫態(tài)，沉積厚度，風(fēng)化程度等都有明顯區(qū)別。