One kilometre-thick ultramylonite, Sierra de Quilmes, Sierras Pampeanas, NW Argentina

M A Finch, R F Weinberg, M G Fuentes, P Hasalova, R Becchio

Research output: Contribution to journalArticleResearchpeer-review

12 Citations (Scopus)

Abstract

We describe a 1km-thick ultramylonite forming the high strain base of the >3.5km-thick El Pichao shear zone in the Sierra de Quilmes. This shear zone thrusted granulite facies migmatites onto amphibolite facies rocks during the 470Ma Famatinian orogeny. Strain grades upwards from ultramylonites to weakly sheared migmatites across the 3.5km-zone and the mylonitic rocks define a geochemical field narrower than the protolith, suggesting they underwent mixing and homogenization through shearing. Ultramylonites this thick are uncommon. The width of a shear zone, in the absence of significant compositional rheological contrasts controlling strain localization, is controlled by the balance between shear heat generation and diffusion. Under typical crustal conditions a strain rate of 10-12s-1 is required to form a 1km-thick ultramylonite, and this is achieved when large movement velocities are imposed across the shear zone. We postulate that the El Pichao shear zone and its thick ultramylonite accommodated a significant fraction of convergence velocities driving the orogeny, and that the wide mylonitic shear zones characteristic of the Cambrian-Ordovician deformation of the Sierras Pampeanas result from the convergent movement being taken up by only a few active major shear zones.
Original languageEnglish
Pages (from-to)33-54
Number of pages22
JournalJournal of Structural Geology
Volume72
DOIs
Publication statusPublished - 2015

Keywords

  • Famatinian orogeny
  • Shear zone width
  • Sierra de Quilmes
  • Sierras Pampeanas
  • Ultramylonite

Cite this

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title = "One kilometre-thick ultramylonite, Sierra de Quilmes, Sierras Pampeanas, NW Argentina",
abstract = "We describe a 1km-thick ultramylonite forming the high strain base of the >3.5km-thick El Pichao shear zone in the Sierra de Quilmes. This shear zone thrusted granulite facies migmatites onto amphibolite facies rocks during the 470Ma Famatinian orogeny. Strain grades upwards from ultramylonites to weakly sheared migmatites across the 3.5km-zone and the mylonitic rocks define a geochemical field narrower than the protolith, suggesting they underwent mixing and homogenization through shearing. Ultramylonites this thick are uncommon. The width of a shear zone, in the absence of significant compositional rheological contrasts controlling strain localization, is controlled by the balance between shear heat generation and diffusion. Under typical crustal conditions a strain rate of 10-12s-1 is required to form a 1km-thick ultramylonite, and this is achieved when large movement velocities are imposed across the shear zone. We postulate that the El Pichao shear zone and its thick ultramylonite accommodated a significant fraction of convergence velocities driving the orogeny, and that the wide mylonitic shear zones characteristic of the Cambrian-Ordovician deformation of the Sierras Pampeanas result from the convergent movement being taken up by only a few active major shear zones.",
keywords = "Famatinian orogeny, Shear zone width, Sierra de Quilmes, Sierras Pampeanas, Ultramylonite",
author = "Finch, {M A} and Weinberg, {R F} and Fuentes, {M G} and P Hasalova and R Becchio",
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One kilometre-thick ultramylonite, Sierra de Quilmes, Sierras Pampeanas, NW Argentina. / Finch, M A; Weinberg, R F; Fuentes, M G; Hasalova, P; Becchio, R.

In: Journal of Structural Geology, Vol. 72, 2015, p. 33-54.

Research output: Contribution to journalArticleResearchpeer-review

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T1 - One kilometre-thick ultramylonite, Sierra de Quilmes, Sierras Pampeanas, NW Argentina

AU - Finch, M A

AU - Weinberg, R F

AU - Fuentes, M G

AU - Hasalova, P

AU - Becchio, R

PY - 2015

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N2 - We describe a 1km-thick ultramylonite forming the high strain base of the >3.5km-thick El Pichao shear zone in the Sierra de Quilmes. This shear zone thrusted granulite facies migmatites onto amphibolite facies rocks during the 470Ma Famatinian orogeny. Strain grades upwards from ultramylonites to weakly sheared migmatites across the 3.5km-zone and the mylonitic rocks define a geochemical field narrower than the protolith, suggesting they underwent mixing and homogenization through shearing. Ultramylonites this thick are uncommon. The width of a shear zone, in the absence of significant compositional rheological contrasts controlling strain localization, is controlled by the balance between shear heat generation and diffusion. Under typical crustal conditions a strain rate of 10-12s-1 is required to form a 1km-thick ultramylonite, and this is achieved when large movement velocities are imposed across the shear zone. We postulate that the El Pichao shear zone and its thick ultramylonite accommodated a significant fraction of convergence velocities driving the orogeny, and that the wide mylonitic shear zones characteristic of the Cambrian-Ordovician deformation of the Sierras Pampeanas result from the convergent movement being taken up by only a few active major shear zones.

AB - We describe a 1km-thick ultramylonite forming the high strain base of the >3.5km-thick El Pichao shear zone in the Sierra de Quilmes. This shear zone thrusted granulite facies migmatites onto amphibolite facies rocks during the 470Ma Famatinian orogeny. Strain grades upwards from ultramylonites to weakly sheared migmatites across the 3.5km-zone and the mylonitic rocks define a geochemical field narrower than the protolith, suggesting they underwent mixing and homogenization through shearing. Ultramylonites this thick are uncommon. The width of a shear zone, in the absence of significant compositional rheological contrasts controlling strain localization, is controlled by the balance between shear heat generation and diffusion. Under typical crustal conditions a strain rate of 10-12s-1 is required to form a 1km-thick ultramylonite, and this is achieved when large movement velocities are imposed across the shear zone. We postulate that the El Pichao shear zone and its thick ultramylonite accommodated a significant fraction of convergence velocities driving the orogeny, and that the wide mylonitic shear zones characteristic of the Cambrian-Ordovician deformation of the Sierras Pampeanas result from the convergent movement being taken up by only a few active major shear zones.

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