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

Access to Document

10.1017/S0016756800038152

Cite this

@article{07a1a784ebef450b91ec294a4f480db8,

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.\}",

year = "1974",

doi = "10.1017/S0016756800038152",

language = "English",

volume = "111",

pages = "121--123",

journal = "Geological Magazine",

issn = "0016-7568",

publisher = "Cambridge University Press (CUP)",

number = "2",

}

TY - JOUR

T1 - Controls of mylonitic compositional layering during non-cataclastic ductile deformation

AU - Vernon, R. H.

PY - 1974

Y1 - 1974

N2 - 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.

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.

UR - https://www.scopus.com/pages/publications/84974269860

U2 - 10.1017/S0016756800038152

DO - 10.1017/S0016756800038152

M3 - Article

AN - SCOPUS:84974269860

SN - 0016-7568

VL - 111

SP - 121

EP - 123

JO - Geological Magazine

JF - Geological Magazine

IS - 2

ER -

Controls of mylonitic compositional layering during non-cataclastic ductile deformation

Abstract

Access to Document

Other files and links

Fingerprint

Cite this