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Structure of a Variscan migmatite-granite transition zone (N Sardinia, Italy)

Author

Listed:
  • M. De Luca
  • N. Ruberti
  • G. Oggiano
  • Ph. Rossi
  • V. Pascucci
  • L. Casini

Abstract

This paper presents the structural map of the Barrabisa Complex, an E-W ribbon-like migmatitic massif exposed in the northern part of Sardinia. The migmatites consist of metatexites and diatexites with variable melt proportion, grading in the central part of the complex to a foliated peraluminous granodiorite. Xenotime/monazite dating indicates that the foliated granodiorite pluton emplaced in upper Carboniferous times (≈307–313 Ma) within a narrow E-W ductile top-to-the east shear zone cutting through a Variscan high-grade metamorphic basement composed of orthogneisses, metasedimentary-derived migmatites and subordinate amphibolites. Field geological mapping, coupled with structural and micro-structural analysis, allowed us to distinguish the granodioritic pluton and three metamorphic units characterized by variable melt to protholith ratio, that represent a continuous transition from metatexite to diatexite with high melt concentration, to foliated granodiorite.

Suggested Citation

  • M. De Luca & N. Ruberti & G. Oggiano & Ph. Rossi & V. Pascucci & L. Casini, 2023. "Structure of a Variscan migmatite-granite transition zone (N Sardinia, Italy)," Journal of Maps, Taylor & Francis Journals, vol. 19(1), pages 2182721-218, December.
  • Handle: RePEc:taf:tjomxx:v:19:y:2023:i:1:p:2182721
    DOI: 10.1080/17445647.2023.2182721
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