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Thermal development of low-pressure metamorphic belts: Results from two-dimensional numerical models

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title

Thermal development of low-pressure metamorphic belts: Results from two-dimensional numerical models (English)

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R. Brooks Hanson

1

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Mark D. Barton

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Mark D. Barton

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language of work or name

English

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publication date

10 August 1989

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published in

Journal of Geophysical Research

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volume

94

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issue

B8

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page(s)

10363-10377

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cites work

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Thermal evolution of plutons: a parameterized approach.

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Role of plutonism in low-pressure metamorphic belt formation

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Continental rifts as a setting for regional metamorphism

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Cordilleran Metamorphic Core Complexes -- From Arizona to Southern Canada

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Magmatism and the development of low-pressure metamorphic belts: Implications from the western United States and thermal modeling

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Metamorphic bathozones and bathograds; a measure of the depth of post-metamorphic uplift and erosion on the regional scale

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Influence of deformation on pressure-temperature paths of metamorphism

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Pressure--Temperature--Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental Crust

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Some thermal and tectonic models for crustal melting in continental collision zones

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Possible thermal buffering by crustal anatexis in collisional orogens: Thermobarometric evidence from the Nepalese Himalaya

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On the mechanics of igneous diapirism, stoping, and zone melting

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On the distribution and separation of crystals in convecting magma

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Thermal effects of metamorphic fluids in subduction zones

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Links between magma-tectonic rate balances, plutonism, and volcanism

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Pressure--Temperature--Time Paths of Regional Metamorphism II. Their Inference and Interpretation using Mineral Assemblages in Metamorphic Rocks

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Structural history of continental volcanic arc rocks, eastern Sierra Nevada, California: A case for extensional tectonics

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Identifiers

DOI

10.1029/JB094IB08P10363

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ADS bibcode

1989JGR....9410363H

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Dimensions Publication ID

1011277975

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(Q57852005)

Thermal development of low-pressure metamorphic belts: Results from two-dimensional numerical models

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