Three main facies have been identified: laminated diatomaceous mud, massive-to-bioturbated diatomaceous mud, and terrigenous mud. These facies exhibit a gradation in properties, with the laminated diatomaceous mud having very high liquid limit, water content, and shear strength, compared to the terrigenous facies, and with the massive-to-bioturbated facies showing intermediate properties. -from Authors
CITATION STYLE
Hill, P. R., & Marsters, J. C. (1990). Controls on physical properties of Peru continental margin sediments and their relationship to deformation styles. Proc., Scientific Reports, ODP, Leg 112, Peru Continental Margin, 623–632. https://doi.org/10.2973/odp.proc.sr.112.168.1990
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