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The Information Analysis of the Sedimentary Facies in the Kazusa Group, Boso Peninsula, Japan
房総半島, 上総層群における堆積相の情報解析
1995
GEOINFORMATICS
房総半島, 上総層群における堆積相の情報解析
The vertical transition between the lithologic facies was treated as the Markov process to interpret the time-spatial change of the sedimentary sequences. An entropy analysis was conducted using the transition probability matrices of the sedimentary facies indicating the Markov process observed in the Kazusa Group, Boso Peninsula. The entropy, indicating the extent of randomness, is divided into D1-component, the amount of the difference from the state of equal probability and D2-component,
doi:10.6010/geoinformatics1990.6.4_177
fatcat:ojvnzlpyybfrvhtdm533rrzxwe