Cretaceous Superplume and the Mississippi Embayment
http://rock.geosociety.org/docs/absindex/annual/2000/51168.htm

Cox Randel, University of Memphis


When last checked this resource was offline Our automated link checker has alerted the folks responsible for the part of our site where this problematic link is referenced. If you have further information about the link (e.g. a new location where the information can be found) please let us know.

You may be able to find previous versions at the Internet Archive.

In this abstract for the 2000 Annual Meeting of the Geological Society of America, Cox and Van Arsdale suggest that pronounced uplift of the Mississippi Valley Graben region associated with Bermuda hotspot volcanism may have been a result of an increased hotspot flux during the Cretaceous superplume interval (~120 to 65 Ma).


Subject: Geoscience:Geology:Structural Geology
Topics: Time/Earth History, Solid Earth:Structural Geology