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contributor authorAlex Rafalovich
contributor authorRonald C. Chaney
date accessioned2017-05-08T20:35:34Z
date available2017-05-08T20:35:34Z
date copyrightNovember 1990
date issued1990
identifier other%28asce%290733-9410%281990%29116%3A11%281744%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/20571
description abstractAn analysis of the apparent overconsolidation properties of deep-sea abyssal plain sediments taken from holes DSDP 576A and MPG-1 is presented. Apparent overconsolidation is believed to be caused by interparticle bonding, or cementation. The cementation can be caused by any one or a combination of the following: silica, potassium, calcium carbonate, ferric oxide, manganese, or biological excretions. Plotting OCR versus depth is shown to result in a ``spurious correlation'' because both depth and OCR have the same independent variable in common, namely depth (
publisherAmerican Society of Civil Engineers
titleCorrelation between OCR and Depth for Deep‐Sea Sediments
typeJournal Paper
journal volume116
journal issue11
journal titleJournal of Geotechnical Engineering
identifier doi10.1061/(ASCE)0733-9410(1990)116:11(1744)
treeJournal of Geotechnical Engineering:;1990:;Volume ( 116 ):;issue: 011
contenttypeFulltext


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