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哈尔滨东郊的荒山是我国东北区较早开展第四纪研究的地点之一。1956年裴文中在荒山发现梅氏犀(Rhinoceros merkeri)下颌骨化石,遂使荒山成为东北区中更新统标准剖面的所在地。此后,对荒山的研究引起了更广泛的兴趣。但以往的工作多侧重地层划分对比、堆积物成因和时代、古生物及考古等方面,对荒山本身的形成和演变问题尚无人论及。本文拟就此提出初浅看法,望指正。
The barren hills in the eastern outskirts of Harbin are one of the sites where the Quaternary studies were started earlier in Northeast China. In 1956, Pei Wenzhong found the Rhinoceros merkeri mandibular fossils on the barren hills, making the barren hills the location of the middle-Pleistocene standard section in Northeast China. Since then, research on barren hills has drawn a wider interest. However, in the past, most of the work focused on the stratigraphic division and contrast, the origin of the deposits and the era, paleontology and archeology, and so far no one had discussed the formation and evolution of the barren hills themselves. This article is intended to put forward preliminary views on this, hope correct.