Seismic b-Value and the Assessment of Ambient Stress in Northeast India

Seismicity data of northeast India, recorded between 1986 and 1999 by a local network, are analysed for estimation of b -values. Based on the obtained values, viz. low ( b  ≤ 0.5), moderate (0.5  0.7), the study area is classified into different seismic-domains. An assessment of stress level is also...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Pure and applied geophysics 2011-10, Vol.168 (10), p.1693-1706
Hauptverfasser: Khan, Prosanta Kumar, Ghosh, Manoj, Chakraborty, Partha Pratim, Mukherjee, Debdeep
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Seismicity data of northeast India, recorded between 1986 and 1999 by a local network, are analysed for estimation of b -values. Based on the obtained values, viz. low ( b  ≤ 0.5), moderate (0.5  0.7), the study area is classified into different seismic-domains. An assessment of stress level is also carried out in identifying seismic-domains. Seismic activities, though mostly confined in some sectors, are presumably triggered by mutual interaction of the Shillong Plateau, Mikir Hills, Indo-Burman Ranges and the easternmost part of the Himalayas, and the contributions from deep-seated fractures cannot be ignored. The results resemble the seismic character of a foreland setting adjacent to a convergent margin. The b -values estimated for 240 square grids of dimension 0.6° × 0.6° over five seismic domains indicate wide variation. An analysis of cumulative seismic moment release ( M O ) in different layers also indicates an anomaly in reference to the total seismic-energy budget of the five zones. The lower b -value and higher M O recorded at relatively lower depth (~30 km) towards the southwest of the study area might be associated with upward bulging of a strong lithosphere. The bulging is perhaps regionally compensated by the downward flexing of the descending Indian lithosphere beneath the Upper Assam area; features unequivocally observed in any foreland setup. Towards the north and east of the study area, random variations of in both b -value and M O along the converging zone suggest a varied tectonic environment with active interaction between the tectonic elements in these areas.
ISSN:0033-4553
1420-9136
DOI:10.1007/s00024-010-0194-x