10,372
edits
Changes
Jump to navigation
Jump to search
Line 62:
Line 62: − The figure below shows the paleogeography of the Mississippi River depositional system from approximately 6 Ma to 4 Ma (interval A). Deposition consists of net sand isopach thicks on the shelf and intraslope basins that are interpreted to be deepwater “fan” complexes.+
Example: mapping depocenters through time (view source)
Revision as of 20:05, 28 March 2014
, 20:05, 28 March 2014→Interval A paleogeography
==Interval A paleogeography==
==Interval A paleogeography==
[[:file:sedimentary-basin-analysis_fig4-13.png|Figure 5]] shows the paleogeography of the Mississippi River depositional system from approximately 6 Ma to 4 Ma (interval A). Deposition consists of net sand isopach thicks on the shelf and intraslope basins that are interpreted to be deepwater “fan” complexes.
==Interval B paleogeography==
==Interval B paleogeography==