| Oceanography > Issues > Archive > Volume 9 > Issue 3 |
1996, Oceanography 9(3):183–188, http://dx.doi.org/10.5670/oceanog.1996.08
Authors | First Paragraph | Full Article | Citation
Michael S. Steckler | Lamont-Doherty Earth Observatory, Palisades, NY, USA
Donald J.P. Swift | Department of Oceanography, Old Dominion University, Norfolk, VA, USA
James P. Syvitski | Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA
John A. Goff | Institute for Geophysics, The University of Texas, Austin, TX, USA
Alan W. Niedoroda | Woodward Clyde Consultants, Tallahassee, FL, USA
A key component of achieving the goals of STRATAFORM is the development of numerical models that provide a means of exploring how the multitude of physical processes active at margins create the preserved stratigraphic record. Numerical models allow study of a wider range of conditions than can be observed easily in the field, or scaled within a laboratory. They also provide tools for extracting and interpreting critical information about the preserved stratigraphy.
Steckler, M.S., D.J.P. Swift, J.P. Syvitski, J.A. Goff, and A.W. Niedoroda. 1996. Modeling the sedimentology and stratigraphy of continental margins. Oceanography 9(3):183–188, http://dx.doi.org/10.5670/oceanog.1996.08.