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Paleomagnetism of the Silurian-Devonian Andreas redbeds: Evidence for an Early Devonian supercontinent?

John D. Miller; Dennis V. Kent

Title:
Paleomagnetism of the Silurian-Devonian Andreas redbeds: Evidence for an Early Devonian supercontinent?
Author(s):
Miller, John D.
Kent, Dennis V.
Date:
Type:
Articles
Department:
Lamont-Doherty Earth Observatory
Volume:
16
Permanent URL:
Book/Journal Title:
Geology
Abstract:
Two components of magnetization were isolated in the Silurian-Devonian Andreas redbeds of the central Appalachians of Pennsylvania (lat 40.75 degrees N, long 75.78 degrees W): a thermally distributed, synfolding B component, and a thermally discrete, pre-Alleghenian-age folding C component. The C component mean direction and associated pole position correspond to a Silurian-Devonian paleolatitude for the Andreas location of about 35 degrees S, which, in conjunction with Early Devonian results from Gondwana, is consistent with an Early Devonian supercontinent configuration.
Subject(s):
Geology
Publisher DOI:
http://dx.doi.org/10.1130/0091-7613(1988)016%3c0195:POTSDA%3e2.3.CO;2
Item views:
63
Metadata:
text | xml
Suggested Citation:
John D. Miller, Dennis V. Kent, 1988, Paleomagnetism of the Silurian-Devonian Andreas redbeds: Evidence for an Early Devonian supercontinent?, Columbia University Academic Commons, http://hdl.handle.net/10022/AC:P:12324.

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