摘要
文章对图们江中游水域水底堆积物进行了物相分析,对其成因做了初步探讨,结果表明,该堆积物主要为砂质和部分磁铁矿,粘土矿物较少。
This paper describe the phase analysis to subaqueous sediment middle reachesof Tumen River,and pretiminary exploraory to the cause of its formation. The resultsshow that the sediment belong to arenose and magnetite,and contain less clays.
出处
《延边大学理工学报》
CAS
1997年第2期31-34,共4页
Journal of Yanbian University (Natural Science)