A rock-magnetic and geomagnetic secular variation record from late-Pleistocene Lake Estancia, New Mexico [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT):Exposed sediments of Late Pleistocene Lake Estancia contain a high resolution record of regional climate variability for the period about 12,000 to 32,000 years. A detailed rock-magnetic study is being performed on this well-dated, well-preserved sedimentary sequence to determine how the magnetic signature of sediments responded to regional climate change.

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Bibliographic Details
Main Authors: Rowe, H.D., Geissman, J.W., Allen, Bruce D., Anderson, Roger Y.
Format: conference_item biblioteca
Language:English
Published: 1996
Subjects:Earth Sciences, Limnology, PACLIM,
Online Access:http://hdl.handle.net/1834/31633
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Summary:EXTRACT (SEE PDF FOR FULL ABSTRACT):Exposed sediments of Late Pleistocene Lake Estancia contain a high resolution record of regional climate variability for the period about 12,000 to 32,000 years. A detailed rock-magnetic study is being performed on this well-dated, well-preserved sedimentary sequence to determine how the magnetic signature of sediments responded to regional climate change.