Geoscience Reference
In-Depth Information
Clark, D., McPherson, A., and Allen, T. (2013). Intraplate earthquakes in Australia. Chapter
2, this topic.
Cloetingh, S. A. P. L., Wortel, M. J. R., and Vlaar, N. J. (1984). Passive margin evolution,
initiation of subduction and the Wilson cycle. Tectonophysics , 109, 147-163.
Coblentz, D. D., and Richardson, R. M. (1996). Analysis of the South American intraplate
stress field. Journal of Geophysical Research , 101(B4), 8643-8657.
Cogne, N., Cobbold, P. R., Riccomini, C., and Gallagher, K. (2012). Tectonic setting of
the Taubate Basin (southeastern Brazil): insights from regional seismic profiles and
outcrop data. Journal of South American Earth Science , 42, 194-204.
Ferreira, J. M., Oliveira, R. T., Takeya, M. K., and Assump¸ ao, M. (1998). Superposition
of local and regional stresses in NE Brazil: evidence from focal mechanisms around
the Potiguar marginal basin. Geophysical Journal International 134, 341-355.
Ferreira, J. M, Bezerra, F. H. R., Sousa, M. O. L., et al . (2008). The role of Precam-
brian mylonitic belts and present-day stress field in the coseismic reactivation of the
Pernambuco lineament, Brazil. Tectonophysics , 456, 111-126.
Gangopadhyay, A., and Talwani, P. (2003). Symptomatic features of intraplate earthquakes.
Seismological Research Letters , 74, 863-883.
Gangopadhyay, A., and Talwani, P. (2007). Two-dimensional numerical modeling suggests
that there is a preferred geometry of intersecting faults that favors intraplate earth-
quakes. In Continental Intraplate Earthquakes: Science, Hazard, and Policy Issues ,
ed. S. Stein, and S. Mazzotti. Geological Society of America Special Paper 425, pp.
87-99.
Gomes, B. S. (1992). Preliminary integration of marine gravimetric data of Petrobras
and Leplac project: Campos, Santos and Pelotas basins. In Proceedings of the 37th
Brazilian Geological Congress ,Sao Paulo, SP, Brazil, 1, 559-560 (in Portuguese).
Holdsworth, R. E., Hand, M., Miller, J. A., and Buick, I. S. (2001). Continental reactiva-
tion and reworking: an introduction. In Continental Reactivation and Reworking , ed.
J. A Miller, R. E. Holdsworth, I. S. Buick, and M. Hand. Geological Society, London,
Special Publication, 184, pp. 1-12.
Houtz, R. E., Ludwig, W. J., Milliman, J. D., and Grow, J. A. (1977). Structure of the
northern Brazilian continental margin. Geological Society of America Bulletin , 88,
711-719.
Johnston, A. C. (1996). Seismic moment assessment of earthquakes in stable conti-
nental regions: I. Instrumental seismicity. Geophysical Journal International , 124,
381-414.
Johnston, A. C., and Kanter, L. R. (1990). Earthquakes in stable continental crust. Scientific
American , 262, 68-75.
Johnston, A. C., Coppersmith, K. J., Kanter, L. R., and Cornell C. A. (1994). The Earth-
quakes of Stable Continental Regions: Assessment of Large Earthquake Potential ,
TR-102261, Vol. 1-5, ed. J. F. Schneider. Palo Alto, CA: Electric Power Research
Institute.
Kirkpatrick, J. D., Bezerra, F. H. R., Shipton, Z. K., et al . (2013). Scale-dependent influence
of pre-existing basement shear zones on rift faulting: a case study from NE Brazil.
Journal of the Geological Society (London) , 170, 237-247.
Lenardic, A., Moresi, L., andMu
hlhaus, H. (2000). The role of mobile belts for the longevity
of deep cratonic lithosphere: the crumple zone model. Geophysical Research Letters ,
27, 1235-1238.
Li, Q. S., Liu, M. A., and Stein, S. (2009). Spatiotemporal complexity of continental
intraplate seismicity: insights from geodynamic modeling and implications for seismic
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
Search WWH ::




Custom Search