The organic maturity of lower Palaeozoic in the eastern Yangzi Gorges area is studied by means of a new technique of kerogen infrared spectroscopy,combined with conodont color alteration index.

 
  • 應用干酪根紅外光譜技術(shù),結合牙形石色變指數分析了峽東地區下古生界有機質(zhì)成熟度。探討了在缺乏鏡質(zhì)體的前泥盆紀地層和海相地層中分析有機質(zhì)成熟度或古地溫的另一有效途徑。
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目錄 附錄 查詞歷史
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