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Nicobar earthquake 2010

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Journal Article
Published: 01 October 2011
Bulletin of the Seismological Society of America (2011) 101 (5): 2568–2577.
... further support reactivation of preexisting tectonic features on the subducting plate and their deeper continuity within the subducting slab. On 12 June 2010, a large ( M w  7.5) earthquake occurred off Car Nicobar, with its source located within the rupture zone of the 2004 Andaman–Sumatra M w...
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Source parameters of the <b>2010</b> Car <b>Nicobar</b> <b>earthquake</b>; (a) moment rate funct...
Published: 06 June 2017
Figure 5. Source parameters of the 2010 Car Nicobar earthquake; (a) moment rate function in N · m plotted versus time (in seconds); (b) the focal mechanism obtained from the moment tensor inversion showing both possible fault planes. The shaded quadrants are the compressional quadrants
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Distribution of Incorporated Research Institutions for Seismology (IRIS) br...
Published: 06 June 2017
Figure 3. Distribution of Incorporated Research Institutions for Seismology (IRIS) broadband seismograph stations used for (a) the 2005 M w  7.2 Car Nicobar earthquake and (b) the 2010 M w  7.5 Car Nicobar earthquake, with station names labeled. The large star represents
Journal Article
Published: 29 January 2019
Bulletin of the Seismological Society of America (2019) 109 (2): 797–811.
.... , 2006 , 2010 ; Grevemeyer and Tiwari, 2006 ; Bilek, 2007 ; Mishra et al. , 2011 ; Carter and Bandopadhyay, 2017 ). Further, the stress imparted from the 2004 Aceh and 2005 Nias earthquakes has significantly modified the seismicity pattern in the Andaman–Nicobar and Sumatra segments ( Engdahl et...
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Journal Article
Published: 06 June 2017
Bulletin of the Seismological Society of America (2017) 107 (4): 1569–1581.
...Figure 5. Source parameters of the 2010 Car Nicobar earthquake; (a) moment rate function in N · m plotted versus time (in seconds); (b) the focal mechanism obtained from the moment tensor inversion showing both possible fault planes. The shaded quadrants are the compressional quadrants...
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Journal Article
Published: 22 January 2020
Seismological Research Letters (2020) 91 (2A): 803–813.
... by the strumming of head buoys due to seafloor currents initiated by oceanic tides in the Andaman–Nicobar region. * Corresponding author: pdewangan@nio.org 29 March 2019 © Seismological Society of America A large number of earthquakes occur at plate boundaries under the oceans, whereas...
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Journal Article
Published: 01 July 2012
Seismological Research Letters (2012) 83 (4): 686–696.
... 2010/02/12 9 Kamorta KAMO 8°2′23.42″N 93°32′32.89″E Reftek 151–120 2010/05/05 The Andaman–Nicobar Islands form the central part of the 5,000-km-long Burma–Sunda–Java subduction complex. The islands, situated to the southwest of the Indian subcontinent, currently overlie one...
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Journal Article
Published: 01 April 2011
Bulletin of the Seismological Society of America (2011) 101 (2): 506–514.
...Vanessa Andrade; Kusala Rajendran Abstract The 1300-km rupture of the 2004 interplate earthquake terminated at around 15° N, in the northernmost segment of the Andaman–Nicobar subduction zone. This part of the plate boundary is noted for its generally lower level seismicity, compared...
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Journal Article
Published: 01 October 2012
Bulletin of the Seismological Society of America (2012) 102 (5): 2063–2076.
...Sreevalsa Kolathayar; T. G. Sitharam Abstract An updated catalog of earthquakes has been prepared for the Andaman–Nicobar and adjoining regions. The catalog was homogenized to a unified magnitude scale, and declustering of the catalog was performed to remove aftershocks and foreshocks. Eleven...
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Journal Article
Published: 09 December 2020
Seismological Research Letters (2021) 92 (2A): 1052–1068.
... by long‐period waves oriented in the north–south direction. The ocean‐bottom seismometer (OBS) data were acquired for the Andaman‐Nicobar region under the Council of Scientific and Industrial Research—Geodynamics and Earthquake generating processes in northeast India and Andaman Subduction zone...
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Journal Article
Published: 03 December 2013
Bulletin of the Seismological Society of America (2014) 104 (1): 587–591.
... B. Catherine J. K. Kumar S. ( 2006 ). Constraints on 2004 Sumatra–Andaman earthquake rupture from GPS measurements in Andaman–Nicobar islands , Earth Planet. Sci. Lett. 242 , nos.  3–4 , 365 – 374 . Herring T. A. King R. W. McClusky S. C. ( 2010...
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(a) Map of the Sumatra–Andaman subduction zone showing large ( M  w &gt;7) ...
Published: 01 October 2011
is its rupture extent with the Nicobar segment marked. (b) The residuals of the tide gauge data from Trincomalee, Sri Lanka, recorded ∼2 hrs after the 12 June 2010 event.
Journal Article
Published: 01 February 2012
Bulletin of the Seismological Society of America (2012) 102 (1): 343–351.
... surface deformation long after a great earthquake. 8 March 2011 The 26 December 2004 M w  9.2 Sumatra–Andaman earthquake ruptured more than 1300 km of the subduction megathrust along the eastern boundary of the Indian and Australian plates (e.g., Shearer and Bürgmann, 2010...
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Journal Article
Published: 17 March 2021
Seismological Research Letters (2021) 92 (4): 2255–2269.
... earthquakes of 1881 ( M w  7.9) and 1941 ( M w  8.1), also depicted in Figure  1 . However, in recent times, the 26 December 2004 megathrust earthquake ( M w  9.3) along the Indian plate near Andaman–Nicobar Islands has been the most devastating event in the region; it also generated...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 April 2011
Lithosphere (2011) 3 (2): 170–172.
... and the Andaman and Nicobar Islands, to determine the slip distribution of the Sumatra-Andaman earthquake with FEM-generated Green's functions and linear inverse methods ( Masterlark and Hughes, 2008 ; Hughes et al., 2010 ). It is the stress and pore-fluid pressure fields generated by this coseismic slip...
FIGURES
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(a) Map of the Sumatra–Andaman subduction zone and the adjoining ocean plat...
Published: 06 June 2017
w  7.9 and 1941 M w  7.7 earthquakes. Location and mechanisms of significant earthquakes discussed in the text are shown. (b) Aftershock distribution (National Earthquake Information Center [NEIC]) (in the fortnight following each event) for the 2005 and (c) 2010 Car Nicobar earthquakes
Journal Article
Journal: Geology
Published: 22 March 2019
Geology (2019) 47 (5): 483–486.
.... , Henstock , T.J. , Bull , J.M. , Gulick , S.P. , Austin , J.A. , Bangs , N.L. , Djajadihardja , Y.S. , and Permana , H. , 2010 , Contrasting décollement and prism properties over the Sumatra 2004–2005 earthquake rupture boundary : Science , v. 329 , p. 207 – 210 , https...
FIGURES
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(a) Location of the 24 July 2005 <b>earthquake</b> and its aftershocks during the ...
Published: 01 October 2011
Figure 4. (a) Location of the 24 July 2005 earthquake and its aftershocks during the seven days that followed. (b, c) Location and depthwise distribution of the 12 June 2010 Nicobar earthquake and its aftershocks during the fortnight that followed. Black and gray filled circles are event
Journal Article
Journal: Geology
Published: 01 June 2011
Geology (2011) 39 (6): 559–562.
... in that it was accompanied by subsidence (as much as 1 m) but not by strong shaking near Port Blair. If event II was the A.D. 1762 Arakan earthquake, the laminated sand and mud provide the first evidence that this earthquake was associated with a tsunami. * E-mail: javed@iitk.ac.in . 27 8 2010 15 1 2011...
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Series: Geological Society, London, Memoirs, Geological Society, London, Memoirs
Published: 01 January 2017
EISBN: 9781786203007
... with a similar focal mechanism, the 12 June 2010 ( M w 7.5) earthquake, is the most recent large earthquake along the Andaman–Nicobar segment. These earthquakes occurred in the subducting plate and were generated by left-lateral strike-slip faulting on NNE–SSW-oriented near-vertical faults ( Rajendran et al...