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Middle Ordovician clastic wedges in East Tennessee: A new look at an old basin
L o a d i n g
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National Energy Technology Laboratory (NETL) - view all
Update frequencyunknown
Last updatedover 2 years ago
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Overview

The Sevier basin could be either a foredeep or backbulge. Transport directions in the Chapman Ridge do not identify the source clearly. Thickness obtained via detailed structural mapping are similar to thickness of Shanmugam and Walker.

kmd
Additional Information
KeyValue
CitationNeil E. Whitmer, Robert D. Hatcher, S. Christopher Whisner, Jennifer B Whisner, J. Ryan Thigpen, John Bultman ---- Roy Long, Middle Ordovician clastic wedges in East Tennessee: A new look at an old basin, 2016-09-29, https://edx.netl.doe.gov/dataset/middle-ordovician-clastic-wedges-in-east-tennessee-a-new-look-at-an-old-basin
Netl Productyes
Poc EmailRoy.long@netl.doe.gov
Point Of ContactRoy Long
Program Or ProjectKMD
Publication Date2001-1-1
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Files
  • 15341 Middle Ordovician Clastic Wedges Slides.pdf