The Thermal Background to Metamorphism I. Simple One-Dimensional Conductive Models. / Nisbet, E. G.; Fowler, C. M. R.

In: Geoscience Canada, Vol. 9, No. 3, 1982, p. 161-164.

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The Thermal Background to Metamorphism I. Simple One-Dimensional Conductive Models. / Nisbet, E. G.; Fowler, C. M. R.

In: Geoscience Canada, Vol. 9, No. 3, 1982, p. 161-164.

Research output: Contribution to journalArticlepeer-review

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@article{be3f02c9a1b649c6ae9397139fcaa0b4,
title = "The Thermal Background to Metamorphism I. Simple One-Dimensional Conductive Models",
abstract = "Simple conductive geotherm calculations provide a useful way of illustrating the thermal constraints on metamorphism in teaching senior undergraduate classes. In this article a variety of one-dimensional problems is examined to show the effects of variation in conductivity, heat production and mantle contribution, and also to show the time needed for a rock column to reequilibrate thermally after erosion.",
author = "Nisbet, {E. G.} and Fowler, {C. M. R.}",
year = "1982",
language = "English",
volume = "9",
pages = "161--164",
journal = "Geoscience Canada",
number = "3",

}

RIS

TY - JOUR

T1 - The Thermal Background to Metamorphism I. Simple One-Dimensional Conductive Models

AU - Nisbet, E. G.

AU - Fowler, C. M. R.

PY - 1982

Y1 - 1982

N2 - Simple conductive geotherm calculations provide a useful way of illustrating the thermal constraints on metamorphism in teaching senior undergraduate classes. In this article a variety of one-dimensional problems is examined to show the effects of variation in conductivity, heat production and mantle contribution, and also to show the time needed for a rock column to reequilibrate thermally after erosion.

AB - Simple conductive geotherm calculations provide a useful way of illustrating the thermal constraints on metamorphism in teaching senior undergraduate classes. In this article a variety of one-dimensional problems is examined to show the effects of variation in conductivity, heat production and mantle contribution, and also to show the time needed for a rock column to reequilibrate thermally after erosion.

M3 - Article

VL - 9

SP - 161

EP - 164

JO - Geoscience Canada

JF - Geoscience Canada

IS - 3

ER -