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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Main Authors: Auchitya Kumar Pandey, Prasanta Chingtham, P. N. S. Roy
Format: Article
Language:English
Published: Taylor & Francis Group 2017-12-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
mc
Online Access:http://dx.doi.org/10.1080/19475705.2017.1345794
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spelling 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
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AT pnsroy homogeneousearthquakecataloguefornortheastregionofindiausingrobuststatisticalapproaches
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