Abstract
With the possible exception of pumice-rich material, unlithified volcaniclastics behave much like detrital deep-sea sediments. In contrast, lithified volcaniclastic sediments display unique physical properties, such as higher electrical resistivity and velocity than expected from porosity values. The primary cause of these phenomena is a lack of interconnectedness of the pore spaces and cementation of the volcaniclastic particles. -from Authors
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CITATION STYLE
Dadey, K. A., & Klaus, A. (1992). Physical properties of volcaniclastic sediments in the Izu-Bonin area. Proc., Scientific Results, ODP, Leg 126, Bonin Arc/Trench System, 543–550. https://doi.org/10.2973/odp.proc.sr.126.156.1992
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