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通过穆斯堡尔方法研究了黄海和东海沉积物中的海绿石化过程,区分了Fe的价态和晶位,并且将初始基质向海绿石的发展过程与穆斯堡尔参数联系了起来。
The Mossbauer method was used to study the sea-green petrification process in the sediments of the Yellow Sea and the East China Sea, distinguishing the valences and the crystal sites of Fe, and linking the development of the initial matrix to the glauconite with the Mössbauer parameters .