Application of Balankin Fractal Model to the Fractal Volcanic Activity Model
Wedi'i Gadw mewn:
| Awdur: | |
|---|---|
| Fformat: | artículo original |
| Statws: | Versión publicada |
| Dyddiad Cyhoeddi: | 2014 |
| Disgrifiad: | The Sequential Fragmentation Theory (SFT, Brown, 1989) is based on sequential fragmentation at macroscopic level. Fractal model proposed by Brenes & Alvarado (2013), with the help of Hurst coefficient H, includes vesicle coalescence and their degassing, thus systematizing the whole process. In this work Balankin fractal fracture model is added. Volcanic fragmentation process is then explained from the micro to the macro level. The existence of two universal fracture values, already experimentally found, is predicted. |
| Gwlad: | Portal de Revistas UCR |
| Sefydliad: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| Iaith: | Español |
| OAI Identifier: | oai:archivo.portal.ucr.ac.cr:article/15109 |
| Mynediad Ar-lein: | https://archivo.revistas.ucr.ac.cr/index.php/geologica/article/view/15109 |
| Allweddair: | Fractura fractal modelo de Balankin exponentes universales Irazú erupción de 1723 Costa Rica |