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一、前言 如同中欧其他地区一样,更新世时在图林根沉淀了冰缘气候产生的,主要是固流体成因的覆盖层。这个覆盖着相应基岩及其松土带的覆盖层在本地区见于两种不同的母体,即风化了的杂色砂岩和玉木冰期的黄土。覆盖层共分成三个不同的层次:上覆盖层1(由杂色砂岩物质组成);上覆盖层2(杂色砂岩与黄土混合)和下覆盖层(杂色砂岩)。在中层有黄
I. INTRODUCTION Like other parts of Central Europe, the Pleistocene precipitated a marginal ice-rim climate in Thuringia, mainly a cover of solid fluid origin. The cover, which covers the corresponding bedrock and its loamy zone, is found in the area in two different matrices, the weathered variegated sandstone and the loess of the Tamaglo ice age. Cover is divided into three different levels: the upper cover 1 (composed of variegated sandstone material); the upper cover 2 (variegated sandstone mixed with loess) and the lower cover (variegated sandstone). Yellow in the middle