地理科学 ›› 1984, Vol. 4 ›› Issue (4): 383-388.doi: 10.13249/j.cnki.sgs.1984.04.383

• 研究报道 • 上一篇    下一篇

哈尔滨荒山近期的上升运动

叶启晓1, 吴金城1, 魏正一2   

  1. 1. 黑龙江省地质局;
    2. 黑龙江省博物馆
  • 出版日期:1984-07-20 发布日期:1984-07-20

THE TECTONIC UPLIFT OCCURED IN HUANG SHAN IN THE LAST THOUSANTS OF YEAR

Ye Qixiao1, Wu Jincheng1, Wei Zhengyi2   

  1. 1. Heilungiiang Geblogy Bureau;
    2. Heilungjiang Museum
  • Online:1984-07-20 Published:1984-07-20

摘要: 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。

Abstract: According to study and inverstigation of a vast amount of informations and evidences on geology,geomorphology,fossil soil and trades of ancient human, a huge geographical variations occured in Huang Shan during the last thousands of year. The authors point out that the directional reason for the variation is the tectonic uplift in Huang Shun far back in the past. The uplift bringed a series of changes, the relief beame higher, climate from wet to dry, vegetation from luxuriance to rareness, and the pedogenesis became slower. After a Considerable period of time, progressively, various consequences and indications in Huang Shah obviously appeared. The even more serious erosion, poor soil,winddrift sand and drought were coming, so that ancient human who lived here had to leave for the existence. This important geographical event occured during the three-four thousands of year.