Corrected Late Triassic latitudes for continents adjacent to the North Atlantic

Publication Type  Journal Article
Year of Publication  2005
Authors  Kent, D. V.; Tauxe, L.
Journal Title  Science
Volume  307
Issue  5707
Pages  240-244
Journal Date  Jan 14
ISBN Number  0036-8075
Accession Number  ISI:000226361900038
Key Words  paleomagnetic correlation; geomagnetic-field; sedimentary-rocks; inclination error; shallow bias; dipole field; fundy basin; pangea-b; america; reconstruction
Abstract  

We use a method based on a statistical geomagnetic field model to recognize and correct for inclination error in sedimentary rocks from early Mesozoic rift basins in North America, Greenland, and Europe. The congruence of the corrected sedimentary results and independent data from igneous rocks on a regional scale indicates that a geocentric axial dipole field operated in the Late Triassic. The corrected paleolatitudes indicate a faster poleward drift of similar to0.6 degrees per million years for this part of Pangea and suggest that the equatorial humid belt in the Late Triassic was about as wide as it is today.

Notes  

888GJTimes Cited:16Cited References Count:44

URL  <Go to ISI>://000226361900038
DOI  DOI 10.1126/science.1105826