role of multifractal analysis in understanding the preparation zone for large size earthquake in the north-western himalaya region
Clicks: 186
ID: 197400
2011
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Steady Performance
30.0
/100
186 views
16 readers
AI Quality Assessment
Not analyzed
Readership in this journal
SteadyRanked #74 of 169 articles by views in BMC research notes
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 169 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
Seismicity has power law in space, time and magnitude distributions and same is expressed by the fractal dimension <i>D</i>, Omori's exponent <i>p</i> and <i>b</i>-value. The spatio-temporal patterns of epicenters have heterogeneous characteristics. As the crust gets self-organised into critical state, the spatio-temporal clustering of epicenters emerges to heterogeneous nature of seismicity. To understand the heterogeneous characteristics of seismicity in a region, multifractal studies hold promise to characterise the dynamics of region. Multifractal study is done on seismicity data of the North-Western Himalaya region which mainly involve seismogenic region of 1905 Kangra great earthquake in the North-Western Himalaya region. The seismicity data obtained from USGS catalogue for time period 1973–2009 has been analysed for the region which includes the October 2005 Muzafrabad-Kashmir earthquake (<i>M</i><sub>w</sub> =7.6). Significant changes have been observed in generalised dimension <i>D<sub>q</sub></i>, <i>D<sub>q</sub></i> spectra and <i>b</i>-value. The significant temporal changes in generalised dimension <i>D<sub>q</sub></i>, <i>b</i>-value and <i>D<sub>q</sub>−q</i> spectra prior to occurrence of Muzaffrabad-Kashmir earthquake relates to distribution of epicenters in the region. The decrease in generalised dimension and <i>b</i>-value observed in our study show the relationship with the clustering of seismicity as is expected in self-organised criticality behaviour of earthquake occurrences. Such study may become important in understanding the preparation zone of large and great size earthquake in various tectonic regions.
| Reference Key |
teotia2011nonlinearrole
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;S. S. Teotia;D. Kumar |
| Journal | BMC research notes |
| Year | 2011 |
| DOI |
10.5194/npg-18-111-2011
|
| URL | |
| Keywords |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.