Geoscience Reference
In-Depth Information
de Lugt, I. R., van Wees, J. D., and Wong, Th. E. (2003). The tectonic evolution of the
southern Dutch North Sea during the Paleogene: basin inversion in distinct pulses.
In
Dynamics of Sedimentary Basin Inversion: Observations and Modelling
, ed. S. B.
Nielsen and U. Bayer.
Tectonophysics
,
373
, 141-159.
England, R. W. (1988). The Early Tertiary stress regime in NW Britain: evidence from the
patterns of volcanic activity. In
Early Tertiary Volcanism and the Opening of the NE
Atlantic
, ed. A. C. Morton and L. M. Parson, Geological Society, London, Special
Publication
39
, pp. 381-389.
Erlstrom, M., Thomas, S. A., Deeks, N., and Sivhed, U. (1997). Structure and tectonic
evolution of the Tornquist Zone and adjacent sedimentary basins in Scania and the
southern Baltic Sea area.
Tectonophysics
, 271, 191-225.
Ghosh, A., Holt, W. E., and Flesch, L. M. (2009). Contribution of gravitational potential
energy differences to the global stress field.
Geophysical Journal International
, 179,
787-812.
Gung, Y., Panning, M., and Romanowicz, B. (2003). Global anisotropy and the thickness
of continents.
Nature
, 422, 707-711, doi:10.1038/nature01559.
Gutierrez-Alonso, G., Fernandez-Suarez, J., Weil, A. B.,
et al
. (2008). Self-subduction of
the Pangaean global plate.
Nature Geosciences
, 1, 549-553
Hansen, D. L., and Nielsen, S. B. (2003). Why rifts invert in compression.
Tectonophysics
,
373, 5-24.
Harrison, J. C., Sweet, A. R., McIntyre, D. J.,
et al
. (1999). Correlation of Cenozoic
sequences of the Canadian Arctic region and Greenland: implications for the tectonic
history of northern North America.
Bulletin of Canadian Petroleum Geology
, 47,
223-254.
Heidbach, O., Fuchs, K., Muller, B.,
et al
. (2007a). The World Stress Map.
Episodes
, 30,
197-201.
Heidbach, O., Reinecker, J., Tingay, M.,
et al
. (2007b). Plate boundary forces are not
enough: second- and third-order stress patterns highlighted in the World Stress Map
database.
Tectonics
, 26, TC6014, doi:10.1029/2007TC002133.
Jones, C. H., Unruh, J. R., and Sonder, L. J. (1996). The role of gravitational potential
energy in active deformation in the southwestern United States.
Nature
, 381, 37-
41.
Kockel, F. (2003). Inversion structures in Central Europe: expressions and reasons, an open
discussion.
Netherlands Journal of Geosciences
, 82, 367-382.
Lamarche, J., Scheck, M., and Lewerenz, B. (2003). Heterogeneous inversion of the Mid-
Polish Trough related to crustal architecture, sedimentary patterns and structural inher-
itance.
Tectonophysics
, 373, 141-159.
McKenzie, D., Jackson, J., and Priestley, K. (2005). Thermal structure of oceanic and
continental lithosphere.
Earth and Planetary Science Letters
, 233, 337-349.
Lithgow-Bertelloni, C., and Guynn, J. H. (2004). Origin of the lithospheric stress field.
Journal of Geophysical Research
, 109, B01408, doi:10.1029/2003JB002467.
Nielsen, S. B., and Hansen, D. L. (2000). Physical explanation of the formation and
evolution of inversion zones and marginal troughs.
Geology
, 28, 875-878.
Nielsen, S. B., Thomsen, E., Hansen, D. L., and Clausen, O. R. (2005). Plate-wide
stress relaxation explains European Palaeocene basin inversions.
Nature
, 435, 195-
198.
Nielsen, S. B., Stephenson, R. A., and Thomsen, E. (2007). Dynamics of Mid-Palaeocene
North Atlantic rifting linked with European intra-plate deformations.
Nature
, 450,
1071-1074.
