Oblique convergence of the crust driven by basal forcing: implications for length-scales of deformation and strain partitioning in orogens

Details Oblique convergence of the crust driven by basal forcing: implications for length-scales of deformation and strain partitioning in orogens Oblique convergence of the crust driven by basal forcing: implications for length-scales of deformation and strain partitioning in orogens

Jan 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995geoji.120...24e&link_type=ejournal

Geophysical Journal International, vol. 120, issue 1, pp. 24-44

Physics

25

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