Modeling Sedimentary Deposits on the Continental Margin

نویسنده

  • Donald J. P. Swift
چکیده

A first objective is to investigate the fabric (pattern) of seabed stratification on continental margins at small time and space scales (1 cm-50 cm depth into the seabed; 1 hr-3 yrs sedimentary record). To this end, we are testing the hypothesis that on muddy shelves such as the northern California shelf, Holocene event stratigraphy consists of the deposits of high-concentration storm regimes associated with river floods, alternating with deposits of low-concentration storm regimes. In order to conduct the test, we have developed several “deterministic” algorithms, in collaboration with our subcontractors, Alan Niedoroda and Chris Reed, at URL Greiner Woodward Clyde, Tallahassee. These algorithms, (EVENT, RESUSPEND, and TRANSPORT), that are driven directly by STRATAFORM and NOAA current meter records.

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تاریخ انتشار 2015