ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青岛即墨温泉喷流沉积物及其沉积模式
  
关键词:XRD determinaytion  division of Quaternary deposits  depositional model of the warm spring  geothermal geology
基金项目:青岛海洋大学科技处自拟课题
作者单位
栾光忠 青岛海洋大学山东青岛266003 
王文正 青岛海洋大学山东青岛266003 
刘东生 青岛海洋大学山东青岛266003 
刘激 青岛海洋大学山东青岛266003 
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摘要:
The Eruptive Flow Sediments in Jimo Warm Spring of Qingdao and Its Depositional Model
      The Quaternary deposits are divided into Layer I, Layer II1, Layer II2 and layer III by means of XRD determinnation, stratigraphy and biostratigraphy. According to the spatial distribution of autogenetic minerals (gypsum and salt rock), Quaternary cmollusa (Gyraulus chihliensis)and microfossils( Illyocypri s sp. )in the sediments and the spatial distribution of these sediments, Layer II1 is considered to be the eruptive flow sediments of the warm spring formed through the erosion, transportation and deposition of Layer I and Layer II2 under the action of high mineralized thermal water at the eruptive flow area of the warm spring. According to spatial distribution of the sediments, the depositional model of the sediments in Jimo warm spring is established.
LUAN Guang-zhong,WANG Wen-zheng,LIU Dong-sheng,LIU Ji.2003.The Eruptive Flow Sediments in Jimo Warm Spring of Qingdao and Its Depositional Model[J].Acta Geoscientica Sinica,24(4):357-360.
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