Publication: [476] Paleogeographic and paleotectonic implications of Mesozoic stratigraphy and structure




Documented Paleocurrents


# Continental Area Stratigraphic Level Total Records Period Latitude Longitude Tectonic Plate Deposition Environment Paleocurrent Type Lithology Formation
1
Data RefID #12906
[Rec № 476] Paleogeographic and paleotectonic implications of Mesozoic stratigraphy and structure
Dickenson, W. & Thayer, T.
In: D. Howell & K. McDougall(ed) Meso.Paleog.W.US.Pac.CoastPaleoSymp., 1977, , Vol 2
Pages 147 - 162 , Total Record: 5
North American Paleocene 5 41015 35 -119 North American alluvial crossbedding sandstone
2
Data RefID #12907
[Rec № 476] Paleogeographic and paleotectonic implications of Mesozoic stratigraphy and structure
Dickenson, W. & Thayer, T.
In: D. Howell & K. McDougall(ed) Meso.Paleog.W.US.Pac.CoastPaleoSymp., 1977, , Vol 2
Pages 147 - 162 , Total Record: 5
North American Paleocene 5 41015 37 -122 North American alluvial crossbedding sandstone
3
Data RefID #12908
[Rec № 476] Paleogeographic and paleotectonic implications of Mesozoic stratigraphy and structure
Dickenson, W. & Thayer, T.
In: D. Howell & K. McDougall(ed) Meso.Paleog.W.US.Pac.CoastPaleoSymp., 1977, , Vol 2
Pages 147 - 162 , Total Record: 5
North American Paleocene 5 41015 35 -119 North American alluvial crossbedding sandstone
4
Data RefID #12909
[Rec № 476] Paleogeographic and paleotectonic implications of Mesozoic stratigraphy and structure
Dickenson, W. & Thayer, T.
In: D. Howell & K. McDougall(ed) Meso.Paleog.W.US.Pac.CoastPaleoSymp., 1977, , Vol 2
Pages 147 - 162 , Total Record: 5
North American Paleocene 5 41015 36 -120 North American alluvial crossbedding sandstone
5
Data RefID #12910
[Rec № 476] Paleogeographic and paleotectonic implications of Mesozoic stratigraphy and structure
Dickenson, W. & Thayer, T.
In: D. Howell & K. McDougall(ed) Meso.Paleog.W.US.Pac.CoastPaleoSymp., 1977, , Vol 2
Pages 147 - 162 , Total Record: 5
North American Paleocene 5 41015 35 -120 North American alluvial crossbedding sandstone