Controls of mylonitic compositional layering during non-cataclastic ductile deformation

R. H. Vernon

doi:10.1017/S0016756800038152

Controls of mylonitic compositional layering during non-cataclastic ductile deformation

R. H. Vernon^*

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

20 Citations (Scopus)

Abstract

Lenticular compositional layering and/or rodding in blastomylonitic rocks, in the simplest situations, can be controlled by (i) the presence of more than one mineral in the parent rock and (ii) relative large grain-size of the parent rock. Deformation and recrystallization during non-cataclastic ductile deformation can produce compositional layering, without chemical segregation.

Original language	English
Pages (from-to)	121-123
Number of pages	3
Journal	Geological Magazine
Volume	111
Issue number	2
DOIs	https://doi.org/10.1017/S0016756800038152
Publication status	Published - 1974

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title = "Controls of mylonitic compositional layering during non-cataclastic ductile deformation",

abstract = "Lenticular compositional layering and/or rodding in blastomylonitic rocks, in the simplest situations, can be controlled by (i) the presence of more than one mineral in the parent rock and (ii) relative large grain-size of the parent rock. Deformation and recrystallization during non-cataclastic ductile deformation can produce compositional layering, without chemical segregation.",

author = "Vernon, {R. H.}",

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AB - Lenticular compositional layering and/or rodding in blastomylonitic rocks, in the simplest situations, can be controlled by (i) the presence of more than one mineral in the parent rock and (ii) relative large grain-size of the parent rock. Deformation and recrystallization during non-cataclastic ductile deformation can produce compositional layering, without chemical segregation.

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DO - 10.1017/S0016756800038152

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Controls of mylonitic compositional layering during non-cataclastic ductile deformation

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