Lattice preferred orientation of quartz inclusions within garnet porphyroblasts from the Imjingang belt, South Korea

W. S. Jung, Jin-Han Lee, Y. Park, S. H. Choi

Research output: Contribution to journalArticle

6 Citations (Scopus)

Abstract

Quartz inclusions within intertectonic garnet porphyroblasts of metapelites from the southern Imjingang belt have a lattice preferred orientation. c-Axis fabrics of the quartz inclusions tend to show a single girdle pattern at a high angle to an earlier foliation together with a submaximum subparallel to an earlier lineation. This lattice preferred orientation of the quartz inclusions might result from intracrystalline deformation together with solution creep prior to the garnet growth or from selective entrapment of quartz grains with a specific lattice orientation during the garnet growth.

Original languageEnglish
Pages (from-to)557-565
Number of pages9
JournalJournal of Structural Geology
Volume24
Issue number3
DOIs
Publication statusPublished - 2002 Jan 16

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porphyroblast
preferred orientation
garnet
quartz
metapelite
lineation
foliation
creep

ASJC Scopus subject areas

  • Geology

Cite this

Lattice preferred orientation of quartz inclusions within garnet porphyroblasts from the Imjingang belt, South Korea. / Jung, W. S.; Lee, Jin-Han; Park, Y.; Choi, S. H.

In: Journal of Structural Geology, Vol. 24, No. 3, 16.01.2002, p. 557-565.

Research output: Contribution to journalArticle

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