Evidence For A Northern Transitional Continental Margin Flora In The Cretaceous (Campanian To Maastrichtian) Matanuska Formation, Talkeetna Mountains, Southcentral Alaska
Dissertation (Ph.D.) University of Alaska Fairbanks, 2007 The Late Cretaceous Matanuska Formation contains shallow and deep marine sediments and nonmarine sediment derived from the Talkeetna volcanic island arc. The sediment accumulated in the Matanuska Seaway, a tectonically active basin on the sou...
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Format: | Doctoral or Postdoctoral Thesis |
Language: | unknown |
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2007
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Online Access: | http://hdl.handle.net/11122/8942 |