Unified model for intraplate earthquakes - Intraplate Earthquakes - page 300

Jing, S., and Stephansson, O. (1990). Numerical modelling of intraplate earthquakes
by 2-dimensional distinct element method. Gerlands Beitrage zur Geophysik , 99,
463-472.
Johnston, A. C. (1989). The seismicity of 'Stable Continental Interiors'. In Earthquakes
at North-Atlantic Passive Margins: Neotectonic and Post-Glacial Rebound , ed. S.
Gregersen and P.W. Basham. Boston, MA: Kluwer Academic, pp. 299-327.
Johnston, A. C., and Kanter, L. R. (1990). Earthquakes in stable continental crust. Scientific
American , 262, 68-75.
Kane, M. F. (1977). Correlation of major earthquake centers withmafic/ultramafic basement
masses. U.S. Geological Survey ProfessionalPaper 1028-O, pp. 199-204.
Kato, A., Kurashimo, E., Igarashi, T., et al . (2009). Reactivation of ancient rift system
triggers devastating intraplate earthquakes. Geophysical Research Letters , 36, L05301,
doi:10.1029/2008GL036450.
Kawanishi, R., Iio, Y., Yukutake, Y., Shibutani, T., and Katao, H. (2009). Local stress
concentration in the seismic belt along Japan Sea coast inferred from precise focal
mechanisms: implications for the stress accumulation process on intraplate faults.
Journal of Geophysical Research , 114, doi:10.1029/2008JB005765.
Kenner, S. J., and Segall, P. A. (2000). A mechanical model for intraplate earthquakes:
application to the New Madrid seismic zone. Science , 289, 2329-2332.
King, G. C. P. (1986). Speculations on the geometry of the initiation and termination process
of earthquake rupture and its relation to morphological and geological structure. Pure
and Applied Geophysics , 124, 567-585.
Liu, L., and Zoback, M. D. (1997). Lithospheric strength and intraplate seismicity in the
New Madrid seismic zone. Tectonics , 16, 585-595.
Liu, M., Stein, S., andWang, H. (2011). 2000 years of migrating earthquakes in north China:
how earthquakes in midcontinents differ from those at plate boundaries. Lithosphere ,
3, 128-132.
Long, L. T. (1976). Speculations concerning southeastern earthquakes, mafic intrusions,
gravity anomalies and stress amplification. Earthquake Notes , 47, 29-35.
Mandal, P. (2013). Seismogenesis of the uninterrupted occurrence of the aftershock activity
in the 2001 Bhuj earthquake zone, Gujarat, India, during 2001-2010. Nature Hazards ,
65, 1063-1083.
Mareschal J.-C., and Kuang, J. (1986). Intraplate stresses and seismicity: the role of topog-
raphy and density heterogeneities. Tectonophysics , 132, 153-162.
Mazarbaud, Y., Bethoux, N., Guilbert, J., and Bellier, O. (2005). Evidence for short-scale
stress field variations within intraplate central-western France. Geophysical Journal
International , 160, 161-178.
Mazzotti, S., and Townend, J. (2010). State of stress in central and eastern North America
seismic zones. Lithosphere , 2, 76-83.
Mazzotti, S., James, T. S., Henton, J., and Adams, J. (2005). GPS crustal strain, post-
glacial rebound, and seismic hazard in eastern North America: the Saint Lawrence
valley example. Journal of Geophysical Research , 110, B11301, doi:10.1029/
2004JB003590.
McKeown, F. A. (1978). Hypothesis: many earthquakes in central and southeastern United
States are causally related to mafic intrusive bodies. Journal of Research, U.S. Geo-
logical Survey , 6, 41-50.
Mooney, W. D., Andrews, M. C., Ginzburg, A., Peters, D. A., and Hamilton, R. M. (1983).
Crustal structure of the northern Mississippi embayment and a comparison with other
rift zones. Tectonophysics , 94, 327-348.