Differentiation by Deformation Revisited

Nick Petford, John Clemens

Research output: Contribution to ConferenceAbstract

Abstract

In a paper published in 1920, N.L Bowen conceived of a situation where forces acting on a crystalline mesh could extract the liquid phase from the solid and in doing so cause variations in chemistry distinct from the purely gravitational effects of fractional crystallisation. His paper was a call-to-arms to explore the deformation potential as a cause of variation in igneous rocks, but was never followed up in a rigorous way. Inspired by this, we have developed a quantitative model showing how shear deformation of a dense magma with poroelastic properties can be related quantitatively to its phase petrology during crystallisation. The critical link between the mechanics and associated compositional changes is the degree to which the magma undergoes dilation (volume increase) during shear. It is important to note the effect can only take place after the initially loose magma has undergone compaction. Key parameters governing the dilatancy effect include the permeability, mush strength, the shear modulus and the contact mechanics and geometry of the granular assemblage. Calculations show that dilation reduces the interstitial fluid (melt) pressure causing, in Bowens words, “the separation of crystals and mother liquor” via a suction effect. At strain rates in excess of the tectonic background, shear-induced melt flow can redistribute chemical components and heat between regions of crystallising magma with contrasting rheological properties, at velocities far in excess of diffusion or buoyancy forces, the latter of course the driving force behind fractional crystallisation and compaction. The local influx of hotter, less evolved melt into regions where crystallisation is more advanced may result in reverse zoning and/or resorption of crystals. Post-failure instabilities include hydraulic rupture of the mush along shear zones governed by the angles of dilation and internal friction. Evolved, compositionally distinct melt fractions removed at this late stage may for example lead to certain miarolitic alkaline rocks and intrusive granophyres in basaltic systems, as proposed by Bowen, and late stage aplites and pegmatites in granites - differentiation by deformation.
Original languageEnglish
Publication statusPublished - 8 Jan 2019
EventThe Volcanic and Magmatic Studies Group International Annual Meeting: VMSG 2019 - the University of St Andrews, Fife, United Kingdom
Duration: 8 Jan 201910 Jan 2019
https://vmsg666952477.wordpress.com/

Workshop

WorkshopThe Volcanic and Magmatic Studies Group International Annual Meeting
CountryUnited Kingdom
CityFife
Period8/01/1910/01/19
Internet address

Fingerprint

dilation
magma
melt
fractional crystallization
mechanics
compaction
crystallization
crystal
resorption
alkaline rock
dilatancy
shear modulus
strain rate
petrology
suction
igneous rock
buoyancy
zoning
shear zone
rupture

Keywords

  • magma, diatancy, mush

Cite this

Petford, N., & Clemens, J. (2019). Differentiation by Deformation Revisited. Abstract from The Volcanic and Magmatic Studies Group International Annual Meeting, Fife, United Kingdom.
Petford, Nick ; Clemens, John. / Differentiation by Deformation Revisited. Abstract from The Volcanic and Magmatic Studies Group International Annual Meeting, Fife, United Kingdom.
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Petford, N & Clemens, J 2019, 'Differentiation by Deformation Revisited', The Volcanic and Magmatic Studies Group International Annual Meeting, Fife, United Kingdom, 8/01/19 - 10/01/19.

Differentiation by Deformation Revisited. / Petford, Nick; Clemens, John.

2019. Abstract from The Volcanic and Magmatic Studies Group International Annual Meeting, Fife, United Kingdom.

Research output: Contribution to ConferenceAbstract

TY - CONF

T1 - Differentiation by Deformation Revisited

AU - Petford, Nick

AU - Clemens, John

PY - 2019/1/8

Y1 - 2019/1/8

N2 - In a paper published in 1920, N.L Bowen conceived of a situation where forces acting on a crystalline mesh could extract the liquid phase from the solid and in doing so cause variations in chemistry distinct from the purely gravitational effects of fractional crystallisation. His paper was a call-to-arms to explore the deformation potential as a cause of variation in igneous rocks, but was never followed up in a rigorous way. Inspired by this, we have developed a quantitative model showing how shear deformation of a dense magma with poroelastic properties can be related quantitatively to its phase petrology during crystallisation. The critical link between the mechanics and associated compositional changes is the degree to which the magma undergoes dilation (volume increase) during shear. It is important to note the effect can only take place after the initially loose magma has undergone compaction. Key parameters governing the dilatancy effect include the permeability, mush strength, the shear modulus and the contact mechanics and geometry of the granular assemblage. Calculations show that dilation reduces the interstitial fluid (melt) pressure causing, in Bowens words, “the separation of crystals and mother liquor” via a suction effect. At strain rates in excess of the tectonic background, shear-induced melt flow can redistribute chemical components and heat between regions of crystallising magma with contrasting rheological properties, at velocities far in excess of diffusion or buoyancy forces, the latter of course the driving force behind fractional crystallisation and compaction. The local influx of hotter, less evolved melt into regions where crystallisation is more advanced may result in reverse zoning and/or resorption of crystals. Post-failure instabilities include hydraulic rupture of the mush along shear zones governed by the angles of dilation and internal friction. Evolved, compositionally distinct melt fractions removed at this late stage may for example lead to certain miarolitic alkaline rocks and intrusive granophyres in basaltic systems, as proposed by Bowen, and late stage aplites and pegmatites in granites - differentiation by deformation.

AB - In a paper published in 1920, N.L Bowen conceived of a situation where forces acting on a crystalline mesh could extract the liquid phase from the solid and in doing so cause variations in chemistry distinct from the purely gravitational effects of fractional crystallisation. His paper was a call-to-arms to explore the deformation potential as a cause of variation in igneous rocks, but was never followed up in a rigorous way. Inspired by this, we have developed a quantitative model showing how shear deformation of a dense magma with poroelastic properties can be related quantitatively to its phase petrology during crystallisation. The critical link between the mechanics and associated compositional changes is the degree to which the magma undergoes dilation (volume increase) during shear. It is important to note the effect can only take place after the initially loose magma has undergone compaction. Key parameters governing the dilatancy effect include the permeability, mush strength, the shear modulus and the contact mechanics and geometry of the granular assemblage. Calculations show that dilation reduces the interstitial fluid (melt) pressure causing, in Bowens words, “the separation of crystals and mother liquor” via a suction effect. At strain rates in excess of the tectonic background, shear-induced melt flow can redistribute chemical components and heat between regions of crystallising magma with contrasting rheological properties, at velocities far in excess of diffusion or buoyancy forces, the latter of course the driving force behind fractional crystallisation and compaction. The local influx of hotter, less evolved melt into regions where crystallisation is more advanced may result in reverse zoning and/or resorption of crystals. Post-failure instabilities include hydraulic rupture of the mush along shear zones governed by the angles of dilation and internal friction. Evolved, compositionally distinct melt fractions removed at this late stage may for example lead to certain miarolitic alkaline rocks and intrusive granophyres in basaltic systems, as proposed by Bowen, and late stage aplites and pegmatites in granites - differentiation by deformation.

KW - magma, diatancy, mush

M3 - Abstract

ER -

Petford N, Clemens J. Differentiation by Deformation Revisited. 2019. Abstract from The Volcanic and Magmatic Studies Group International Annual Meeting, Fife, United Kingdom.