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EFFECT OF EROSION ON PALEOCLIMATIC AND TOPOGRAPHIC CORRECTIONS TO HEAT-FLOW

Abstract:

The increase of surface temperature following a recent period of glaciation lowers the heat flow at shallow depths. At greater depths, increase of heat flow above the steady-state value might be expected, reflecting lowered surface temperature during the glacial period itself. Thus a plot of the climatic perturbation to heat flow against depth should have a sigmate form. The fact that measurable negative and positive deviation in heat flow (measurable amplitude of the sigmate variation) has n...

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Publication status:
Published

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Journal:
EARTH AND PLANETARY SCIENCE LETTERS More from this journal
Volume:
39
Issue:
3
Pages:
427-434
Publication date:
1978-01-01
DOI:
ISSN:
0012-821X
Language:
English
Pubs id:
pubs:205384
UUID:
uuid:c749344b-7b7a-4815-be53-5e2ca7471db3
Local pid:
pubs:205384
Source identifiers:
205384
Deposit date:
2012-12-19

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