Andalusite-sillimanite-quartz veins as indicators of low-pressure-high-temperature deformation during late-stage unroofing of a metamorphic core complex, Turkey

D. L. Whitney, Y. Dilek

Research output: Contribution to journalArticlepeer-review

30 Scopus citations

Abstract

Ductilely deformed veins consisting of quartz + andalusite, in which the andalusite is partially replaced by fibrous sillimanite, locally occur in garnet-sillimanite schist near a margin of the Nigde metamorphic core complex in south-central Turkey. Mineral assemblages, reaction textures and structural features of the veins record low-pressure-high-temperature deformation during exhumation of mid-crustal rocks. The partial replacement of andalusite by sillimanite may indicate a late-stage increase in temperature and/or fluid pressure, possibly related to Miocene magmatism, during extensional unroofing of the core complex. Aluminosilicate-bearing veins are observed at the eastern margin of the massif where metapelitic rocks were deformed during unroofing of the core complex. Veins formed in aluminous rocks where deformation-enhanced permeability allowed fluid flow during extensional shear. The cm-scale veins are typically boundinaged and form asymmetric lenses concordant with the host rock foliation and are parallel to the down-dip lineation defined by sillimanite and stretched biotite. Aluminosilicate-bearing boudins record top-to-the-east shear sense, which is compatible with the extensional shear sense displayed by structures in the host rock.

Original languageEnglish (US)
Pages (from-to)59-66
Number of pages8
JournalJournal of Metamorphic Geology
Volume18
Issue number1
DOIs
StatePublished - Jan 2000

Keywords

  • Andalusite
  • Core complex
  • Sillimanite
  • Turkey
  • Veins

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