| contributor author | Alex Rafalovich | |
| contributor author | Ronald C. Chaney | |
| date accessioned | 2017-05-08T20:35:34Z | |
| date available | 2017-05-08T20:35:34Z | |
| date copyright | November 1990 | |
| date issued | 1990 | |
| identifier other | %28asce%290733-9410%281990%29116%3A11%281744%29.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl/handle/yetl/20571 | |
| description abstract | An 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 ( | |
| publisher | American Society of Civil Engineers | |
| title | Correlation between OCR and Depth for Deep‐Sea Sediments | |
| type | Journal Paper | |
| journal volume | 116 | |
| journal issue | 11 | |
| journal title | Journal of Geotechnical Engineering | |
| identifier doi | 10.1061/(ASCE)0733-9410(1990)116:11(1744) | |
| tree | Journal of Geotechnical Engineering:;1990:;Volume ( 116 ):;issue: 011 | |
| contenttype | Fulltext | |