Middle Ordovician clastic wedges in East Tennessee: A new look at an old basin

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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.

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Neil 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

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Field	Value
Last Updated	September 29, 2016, 15:25 (LMT)
Created	September 29, 2016, 15:25 (LMT)
Citation	Neil 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 Product	yes
Poc Email	Roy.long@netl.doe.gov
Point Of Contact	Roy Long
Program Or Project	KMD
Publication Date	2001-1-1

Middle Ordovician clastic wedges in East Tennessee: A new look at an old basin

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