| Graphic correlation<ref name=ch17r79>Shaw, A., B., 1964, Time in Stratigraphy: New York, McGraw-Hill, 365 p.</ref> is a widely accepted deterministic technique for ranking fossil occurrences according to the geological time represented in a set of reference sections. This approach has broad applications to solving biostratigraphic and sedimentologic problems (see Mann & Lane<ref name=ch17r61>Mann, K., O., Lane, H., R., eds., 1995, Graphic Correlation: SEPM (Society for Sedimentary Geology) Special Publication 53, 263 p.</ref>). | | Graphic correlation<ref name=ch17r79>Shaw, A., B., 1964, Time in Stratigraphy: New York, McGraw-Hill, 365 p.</ref> is a widely accepted deterministic technique for ranking fossil occurrences according to the geological time represented in a set of reference sections. This approach has broad applications to solving biostratigraphic and sedimentologic problems (see Mann & Lane<ref name=ch17r61>Mann, K., O., Lane, H., R., eds., 1995, Graphic Correlation: SEPM (Society for Sedimentary Geology) Special Publication 53, 263 p.</ref>). |