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Isotopic and palaeomagnetic evidence for rates of cooling, uplift and erosion

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Date

1985

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Abstract

The use of isotopic and magnetic blocking temperatures to infer cooling history is reviewed in the light of kinetic models of the blocking process. Published isotopic estimates of cooling and uplift (erosion) rates are based upon (a) vertical gradients of fission track ages, (b) age differences amongst isotopic-mineral systems with different blocking temperatures and

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https://dspace-test.anu.edu.au/handle/1885/733727504

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DevOps Pure Testing

Source

Geological Society Memoir

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Article

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DOI

10.1144/GSL.MEM.1985.010.01.26

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