Migration of the Acadian Orogen and foreland basin across the Northern Appalachians of Maine and adjacent areas
Professional Paper
1624
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Abstract
The timing of Acadian orogenesis in Maine is reassessed, on the basis of a new Silurian-Devonian time scale, new U/Pb and 40Ar/39Ar ages of Acadian plutons, new conodont and palynomorph ages of strata that constrain the age of deformation, and published information. This analysis shows that the Acadian deformation front migrated some 240 km (present distance) from southeast to northwest during a span of about 40 million years from Late Silurian to Middle Devonian time.
Suggested Citation
Bradley, D.C., Tucker, R.D., Lux, D.R., Harris, A.G., and McGregor, D.C., 2000, Migration of the Acadian Orogen and foreland basin across the Northern Appalachians of Maine and adjacent areas: U.S. Geological Survey Professional Paper 1624, 55 p., https://doi.org/10.3133/pp1624.
ISSN: 2330-7102 (online)
Study Area
| Publication type | Report |
|---|---|
| Publication Subtype | USGS Numbered Series |
| Title | Migration of the Acadian Orogen and foreland basin across the Northern Appalachians of Maine and adjacent areas |
| Series title | Professional Paper |
| Series number | 1624 |
| DOI | 10.3133/pp1624 |
| Year Published | 2000 |
| Language | English |
| Publisher | U.S. Geological Survey, |
| Contributing office(s) | Alaska Science Center |
| Description | 55 p. |
| First page | 0 |
| Last page | 55 |