English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 78818/78818 (100%)
造訪人次 : 34764603      線上人數 : 1364
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜尋範圍 查詢小技巧:
  • 您可在西文檢索詞彙前後加上"雙引號",以獲取較精準的檢索結果
  • 若欲以作者姓名搜尋,建議至進階搜尋限定作者欄位,可獲得較完整資料
  • 進階搜尋


    請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/27581


    題名: An electrostratigraphic study of the Hsinying-Matou coastal plain, southwestern Taiwan
    作者: Cheng,PH;Yang,CH;Huang,YS;Liu,TK;Sung,QC
    貢獻者: 地球物理研究所
    日期: 1999
    上傳時間: 2010-06-29 18:41:17 (UTC+8)
    出版者: 中央大學
    摘要: One hundred and two vertical electric soundings were conducted in the Hsinying-Matou coastal plain in southwestern Taiwan, for the study of electrostratigraphy and the changes in sedimentary environments. The sounding data were interpreted using the 1-D inversion method. The results indicate that the strata from the surface to 180 meters depth can be divided into three electrostratigraphic units. They are designated, from top to bottom, as the T, S, and R facies. The T- facies is a combination of thin layers of resistivity ranging from 5 to 45 ohm-m, and is 10 to 60 meters thick. The S- facies is characterized by thick layers of resistivity lower than 5 ohm-m, and is 80 to more than 130 meters thick in the west but absent in the east. The R- facies is characterized by thick layers of resistivity ranging from 5 to 50 ohm-m. These three units are similar in lithology; they are mainly composed of clay, mud, silt, and fine sand. The S- facies was sedimented in lagoonal, beach, and shallow marine environments. The T and the R facies were sedimented in non-marine environments in the east, and in lagoonal and estuarine environments in the west. The resistivity of stratum is controlled mainly by the salinity of formation water where the water is saline, and by the grain size and the amount of clay contained where the water is fresh. It is inferred that the period from 40 to 8 Ka is transgressive dominant, and the period since 8 Ka is regressive dominant. The mouth of the Tsengwenchi stream was located about 20 Km east of the present coastline at 9 Ka. The Tsengwenchi stream developed westwardly since 9 Ka till recent times, and then changed southwestwardly to the present location.
    關聯: TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES
    顯示於類別:[地球物理研究所] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML533檢視/開啟


    在NCUIR中所有的資料項目都受到原著作權保護.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明