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干旱区地理 ›› 1991, Vol. 14 ›› Issue (4): 89-93.doi: 10.13826/j.cnki.cn65-1103/x.1991.04.017

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阿尔泰山克木齐河中游阶地砂金矿的粒度特征与环境意义

史家莉, 叶玮   

  1. 中国科学院新疆地理研究所
  • 出版日期:1991-12-25 发布日期:2025-12-25

A PRELIMINARY STUDY ON THE CHARACTERISTICS OF GRAIN SIZE AND SEDIMENT ENVIRONMENT OF KEMUQI GOID-PLACER, ALTAI MOUNTAINS

Shi Jiali, Ye Wei   

  1. Xinjiang Institute of Geography, Chinese Academy of Sciences
  • Published:1991-12-25 Online:2025-12-25

摘要: 克木齐河中游Ⅲ级阶地沉积物粒度特征表明,矿层与盖层具有明显不同的沉积条件,含矿沉积物形成于高能环境下,因此分选差.粉砂粘土含量高,砾石长轴优势方向与水流平行覆盖其上的沉积物分选较好,平均粒径大,粘土粉砂含量低,应属水流较稳定环境下的产物,水流能量的这种周期性变化是导致砂金富集的有利因素之一。

关键词: 克木齐河, 砂金矿, 粒度

Abstract: Kemuqi gold-placer area is an important part of Xishan region where has been famous for producting placer-gold for a long time. A primary study on grain-size and sedimental environment of the placer shows that the deposits with rich placer golds are usually characterized by a higher percentage of silt and clay and poorly-sorting. According to the analysis, the authors believe that the deposits belong to a kind of fluvial sediment. It is different from the overlying sediment. The cause of formation of the placer is a long and complex precess. The placer-gold was mainly produced in the period when the flow had a very strong energy to transport the debris. So the flow power play an important role in transporting and depositing placer-golds in Altai Mountains.