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中国沙漠 ›› 1995, Vol. 15 ›› Issue (4): 374-377.

• 论文 • 上一篇    下一篇

兰州“930505”特大尘暴沉积物重矿物研究

陈国英1, 戴雪荣2, 张铭杰1   

  1. 1. 兰州大学地质系, 兰州 730000;
    2. 兰州大学地理科学系, 兰州 730000
  • 收稿日期:1995-02-24 修回日期:1995-06-16 出版日期:1995-12-20 发布日期:1995-12-20
  • 通讯作者: 戴雪荣
  • 基金资助:
    国家自然科学青年基金资助项目(49201016)成果之一

STUDY ON THE HEAVY MINERALS IN THE DUSTFALL OF THE SEVERE DUSTSTORM NUMBERED 930505 IN LANZHOU AREA,GANSU PROVINCE

Chen Guoying1, Dai Xuerong2, Zhang Mingjie1   

  1. 1. Department of Geology, Lanxhou University, Lanzhou, 730000;
    2. Department of Geographical Science, Lanxhou University, Lanzhou, 730000
  • Received:1995-02-24 Revised:1995-06-16 Online:1995-12-20 Published:1995-12-20

摘要: 本文对兰州"930505"特大尘暴沉积物进行了重矿物研究,鉴定重矿物共27种,其中不稳定矿物3种、较稳定矿物11种、稳定矿物6种和极稳定矿物7种。重矿物组合及含量特征指示特大尘暴沉积物主要来自中酸性花岗质侵入岩并混有变质岩的风化产物。从而可以认为尘暴物源区应在甘肃北山及其东邻沙漠地带,与特大尘暴开始"起沙成暴"的主要地区基本一致。若与兰州马兰黄土之重矿物组合特征相比,现代尘暴之物源区较之末次冰期时不同。

关键词: 特大尘暴沉积物, 重矿物, 兰州

Abstract: This paper studies the heavy minerals in the dustfall of a catastrophic duststorm that took place on May 5, 1993 in Lanzhou Area, Gansu Province. Detailed determination under,microscope reveals that there are totally 27 kinds of the heavy minerals, of which 3 kinds are of unstable,11kinds of less stable, 5 kinds of stable, and 8 kinds of extremely stable. According to the components and the conbination characteristics of heavy minerals and also the formation area of the duststorm,it suggests that the wind-blown deposits are mainly derived from the sedentary products of neutral and acidic granolite and some sedentary products of metamorphic rocks.Clearly,the main source area of the dustfall deposits must be Beishan mountains(in Gansu)and the adjacent desert areas to the east.The source areas of the duststorm deposists differ from those of the Malan loess deposited in the last glacial period.

Key words: Severe duststorm, Heavy minerals, Lanzhou