Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches
Regular seismic hazard assessment requires essentially an updated and refined homogenous earthquake catalogue for the study region. Here, we have compiled the earthquake data for Northeast region of India in a chronological order from International Seismological Centre and Global Centroid Moment Ten...
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doaj-bb6fc609d8c94476a44ea4070ca605042020-11-25T01:28:19ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132017-12-01821477149110.1080/19475705.2017.13457941345794Homogeneous earthquake catalogue for Northeast region of India using robust statistical approachesAuchitya Kumar Pandey0Prasanta Chingtham1P. N. S. Roy2Indian Institute of Technology (Indian School of Mines)National Center for Seismology, Ministry of Earth SciencesIndian Institute of Technology (Indian School of Mines)Regular seismic hazard assessment requires essentially an updated and refined homogenous earthquake catalogue for the study region. Here, we have compiled the earthquake data for Northeast region of India in a chronological order from International Seismological Centre and Global Centroid Moment Tensor databases during the period 1 January 1900 to 31 April 2016. For this purpose, the regression techniques such as least square (SR), inverse least square (ISR), orthogonal (OR) and generalized orthogonal (GOR) which is the best one, out of that are employed for converting different types of magnitude scales, such as surface-wave magnitude (MS), body-wave magnitude (mb) and local magnitude (ML) into a single homogenized moment magnitude, MW. The homogenized catalogue is then treated with ‘runs test’ to estimate p-value of 0.8421 which suggest no spurious reporting on the catalogue. The prepared catalogue has also been declustered using standard procedure. Furthermore, the magnitude of completeness for space and time with 90% confidence level has been achieved. The seismicity parameters, namely magnitude of completeness MC, a-value and b-value are found to be 4.6, 7.50 and 0.95(±0.023), respectively. The observed low b-value implies that the study region is tectonically very active with the presence of asperity.http://dx.doi.org/10.1080/19475705.2017.1345794generalized orthogonal regressionhomogenizationmca-value and b-valuenortheast india |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Auchitya Kumar Pandey Prasanta Chingtham P. N. S. Roy |
spellingShingle |
Auchitya Kumar Pandey Prasanta Chingtham P. N. S. Roy Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches Geomatics, Natural Hazards & Risk generalized orthogonal regression homogenization mc a-value and b-value northeast india |
author_facet |
Auchitya Kumar Pandey Prasanta Chingtham P. N. S. Roy |
author_sort |
Auchitya Kumar Pandey |
title |
Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches |
title_short |
Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches |
title_full |
Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches |
title_fullStr |
Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches |
title_full_unstemmed |
Homogeneous earthquake catalogue for Northeast region of India using robust statistical approaches |
title_sort |
homogeneous earthquake catalogue for northeast region of india using robust statistical approaches |
publisher |
Taylor & Francis Group |
series |
Geomatics, Natural Hazards & Risk |
issn |
1947-5705 1947-5713 |
publishDate |
2017-12-01 |
description |
Regular seismic hazard assessment requires essentially an updated and refined homogenous earthquake catalogue for the study region. Here, we have compiled the earthquake data for Northeast region of India in a chronological order from International Seismological Centre and Global Centroid Moment Tensor databases during the period 1 January 1900 to 31 April 2016. For this purpose, the regression techniques such as least square (SR), inverse least square (ISR), orthogonal (OR) and generalized orthogonal (GOR) which is the best one, out of that are employed for converting different types of magnitude scales, such as surface-wave magnitude (MS), body-wave magnitude (mb) and local magnitude (ML) into a single homogenized moment magnitude, MW. The homogenized catalogue is then treated with ‘runs test’ to estimate p-value of 0.8421 which suggest no spurious reporting on the catalogue. The prepared catalogue has also been declustered using standard procedure. Furthermore, the magnitude of completeness for space and time with 90% confidence level has been achieved. The seismicity parameters, namely magnitude of completeness MC, a-value and b-value are found to be 4.6, 7.50 and 0.95(±0.023), respectively. The observed low b-value implies that the study region is tectonically very active with the presence of asperity. |
topic |
generalized orthogonal regression homogenization mc a-value and b-value northeast india |
url |
http://dx.doi.org/10.1080/19475705.2017.1345794 |
work_keys_str_mv |
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