The Past Earth's Rotation
| dc.creator | Arbab, A. I. | |
| dc.date | 1999-05-25 | |
| dc.date | 2001-06-22 | |
| dc.date.accessioned | 2026-07-07T05:57:01Z | |
| dc.date.available | 2026-07-07T05:57:01Z | |
| dc.description | We have proposed a model to obtain the length of the day and month at any geologic time. The day is found to increase by 0.002 sec/century since the seventeenth century. The lengthening of the day is attributed entirely to the increasing gravitational constant ($G$) with time that manifested its self in tidal forces. The data obtained are consistent with those found from Palaeontology. The length of the day 4500 million years ago was 6 hours and the synodic month was 56.26 present epoch days. | |
| dc.description | Presented at the 9th UNESCO / ESA Workshop on Basic Space Science, 27-30 June 2000, Toulouse-France | |
| dc.identifier | https://arxiv.org/abs/physics/9905049 | |
| dc.identifier | http://arxiv.org/abs/physics/9905049 | |
| dc.identifier.uri | http://salesiana.dossiersoluciones.com/handle/123456789/87831 | |
| dc.subject | General Physics | |
| dc.subject | Geophysics | |
| dc.title | The Past Earth's Rotation | |
| dc.type | text |