Garnet pyroxenite from Nilgiri Block, southern India: Vestiges of a Neoarchean volcanic arc

Vinod O. Samuel, Sanghoon Kwon, M. Santosh, K. Sajeev

Research output: Contribution to journalArticle

6 Citations (Scopus)

Abstract

Southern peninsular India preserves records of Late Neoarchean−Early Paleoproterozoic continental building and cratonization. A transect from the Paleoarchean Dharwar Craton to the Neoarchean arc magmatic complex in the Nilgiri Block across the intervening Moyar Suture Zone reveals an arc-accretionary complex composed of banded iron formation (BIF), amphibolite, metatuff, garnet-kyanite schist, metagabbro, pyroxenite and charnockite. Here we investigate the petrology, geochronology and petrogenesis of the pyroxenite and garnet-clinopyroxenite. The pyroxenite is mainly composed of orthopyroxene and clinopyroxene with local domains/pockets enriched in a clinopyroxene-garnet assemblage. Thermobarometric calculations and phase equilibria modeling suggest that the orthopyroxene- and clinopyroxene-rich domains formed at 900–1000 °C, 1−1.2 GPa whereas the garnet- and clinopyroxene-rich domains record higher pressure of about 1.8−2 GPa at similar temperature conditions (900−1000 °C). Zircon U–Pb SHRIMP dating show weighted mean 207Pb–206Pb age of 2532 ± 22 Ma, with metamorphic overgrowth at 2520 ± 27 Ma and 2478 ± 27 Ma. We propose a tectonic model involving decoupling and break-off of the oceanic plate along the southern flanks of the Dharwar Craton, which initiated oceanic plate subduction. Slab melting eventually built the Nilgiri volcanic arc on top of the over-riding plate along the flanks of the Dharwar Craton. Our study supports an active plate tectonic regime at the end of the Archean Era, aiding in the growth of paleo-continents and their assembly into stable cratons.

Original languageEnglish
Pages (from-to)120-135
Number of pages16
JournalLithos
Volume310-311
DOIs
Publication statusPublished - 2018 Jun

Fingerprint

pyroxenite
Garnets
clinopyroxene
island arc
craton
garnet
Tectonics
orthopyroxene
Geochronology
SHRIMP dating
Petrology
metagabbro
charnockite
banded iron formation
kyanite
suture zone
phase equilibrium
amphibolite
petrogenesis
plate tectonics

All Science Journal Classification (ASJC) codes

  • Geology
  • Geochemistry and Petrology

Cite this

Samuel, Vinod O. ; Kwon, Sanghoon ; Santosh, M. ; Sajeev, K. / Garnet pyroxenite from Nilgiri Block, southern India : Vestiges of a Neoarchean volcanic arc. In: Lithos. 2018 ; Vol. 310-311. pp. 120-135.
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abstract = "Southern peninsular India preserves records of Late Neoarchean−Early Paleoproterozoic continental building and cratonization. A transect from the Paleoarchean Dharwar Craton to the Neoarchean arc magmatic complex in the Nilgiri Block across the intervening Moyar Suture Zone reveals an arc-accretionary complex composed of banded iron formation (BIF), amphibolite, metatuff, garnet-kyanite schist, metagabbro, pyroxenite and charnockite. Here we investigate the petrology, geochronology and petrogenesis of the pyroxenite and garnet-clinopyroxenite. The pyroxenite is mainly composed of orthopyroxene and clinopyroxene with local domains/pockets enriched in a clinopyroxene-garnet assemblage. Thermobarometric calculations and phase equilibria modeling suggest that the orthopyroxene- and clinopyroxene-rich domains formed at 900–1000 °C, 1−1.2 GPa whereas the garnet- and clinopyroxene-rich domains record higher pressure of about 1.8−2 GPa at similar temperature conditions (900−1000 °C). Zircon U–Pb SHRIMP dating show weighted mean 207Pb–206Pb age of 2532 ± 22 Ma, with metamorphic overgrowth at 2520 ± 27 Ma and 2478 ± 27 Ma. We propose a tectonic model involving decoupling and break-off of the oceanic plate along the southern flanks of the Dharwar Craton, which initiated oceanic plate subduction. Slab melting eventually built the Nilgiri volcanic arc on top of the over-riding plate along the flanks of the Dharwar Craton. Our study supports an active plate tectonic regime at the end of the Archean Era, aiding in the growth of paleo-continents and their assembly into stable cratons.",
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Garnet pyroxenite from Nilgiri Block, southern India : Vestiges of a Neoarchean volcanic arc. / Samuel, Vinod O.; Kwon, Sanghoon; Santosh, M.; Sajeev, K.

In: Lithos, Vol. 310-311, 06.2018, p. 120-135.

Research output: Contribution to journalArticle

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T1 - Garnet pyroxenite from Nilgiri Block, southern India

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AU - Samuel, Vinod O.

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AB - Southern peninsular India preserves records of Late Neoarchean−Early Paleoproterozoic continental building and cratonization. A transect from the Paleoarchean Dharwar Craton to the Neoarchean arc magmatic complex in the Nilgiri Block across the intervening Moyar Suture Zone reveals an arc-accretionary complex composed of banded iron formation (BIF), amphibolite, metatuff, garnet-kyanite schist, metagabbro, pyroxenite and charnockite. Here we investigate the petrology, geochronology and petrogenesis of the pyroxenite and garnet-clinopyroxenite. The pyroxenite is mainly composed of orthopyroxene and clinopyroxene with local domains/pockets enriched in a clinopyroxene-garnet assemblage. Thermobarometric calculations and phase equilibria modeling suggest that the orthopyroxene- and clinopyroxene-rich domains formed at 900–1000 °C, 1−1.2 GPa whereas the garnet- and clinopyroxene-rich domains record higher pressure of about 1.8−2 GPa at similar temperature conditions (900−1000 °C). Zircon U–Pb SHRIMP dating show weighted mean 207Pb–206Pb age of 2532 ± 22 Ma, with metamorphic overgrowth at 2520 ± 27 Ma and 2478 ± 27 Ma. We propose a tectonic model involving decoupling and break-off of the oceanic plate along the southern flanks of the Dharwar Craton, which initiated oceanic plate subduction. Slab melting eventually built the Nilgiri volcanic arc on top of the over-riding plate along the flanks of the Dharwar Craton. Our study supports an active plate tectonic regime at the end of the Archean Era, aiding in the growth of paleo-continents and their assembly into stable cratons.

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