Anticlockwise P-T evolution at ~280 Ma recorded from ultrahigh-temperature metapelitic granulite in the Chinese Altai orogenic belt, a possible link with the Tarim mantle plume?

Laixi Tong, Yi Gang Xu, Peter A. Cawood, Xin Zhou, Yibing Chen, Zhao Liu

Research output: Contribution to journalArticleResearchpeer-review

Abstract

An ultrahigh-temperature (UHT) metapelitic granulite assemblage consisting of garnet(g)-spinel(sp)-orthopyroxene(opx)-sillimanite(sil)-cordierite(cd)-ilmenite(ilm)-biotite(bi)-plagioclase(pl)-quartz(q) occurs within migmatitic paragneiss near Kalasu in the Chinese Altai, NW China. Textural relations, mineral compositions and P-T estimates, indicate three stages of mineral assemblages: (1) pre-peak prograde stage (M1) consisting of a sp-sil-bearing or sp-opx-bearing inclusion assemblage, with low-Al2O3 contents (4-5wt.%) in orthopyroxene and P-T conditions of ~7kbar and ~890°C, (2) peak UHT stage (M2) comprising a g-opx-cd-bearing coarse-grained assemblage, with high-Al2O3 contents (8-9wt.%) in orthopyroxene and peak conditions of ~8kbar and ~970°C, and (3) post-peak HT stage (M3) containing an oriented opx-bi-sil-bearing assemblage in matrix, with moderate amounts of Al2O3 (6-7wt.%) in orthopyroxene and P-T conditions of 8-9kbar and ~870°C. The three discrete stages define an anticlockwise P-T path involving initial prograde heating and post-peak near isobaric cooling. Such a near isobaric cooling anticlockwise P-T path suggests that UHT metamorphism likely occurred in an overall extensional tectonic setting with associated underplating of mantle-derived mafic magma. A SHRIMP zircon U-Pb age of 278±2Ma obtained from the metapelitic granulite indicates UHT metamorphism in the Altai orogen occurred during the Permian, coeval with spacially associated mantle-derived mafic intrusions (~280Ma) and the Tarim mantle plume (~275Ma). Thus, the Permian UHT metamorphism of the Chinese Altai is likely associated with underplating and heating of mantle-derived mafic magma as a result of the Tarim mantle plume.

Original languageEnglish
Pages (from-to)1-11
Number of pages11
JournalJournal of Asian Earth Sciences
Volume94
DOIs
Publication statusPublished - 2014
Externally publishedYes

Keywords

  • Mantle plume
  • P-T path
  • The Chinese Altai
  • U-Pb age
  • Ultrahigh-temperature metamorphism

Cite this

@article{a51ccfabc2da48ff9e58bfcb90f5e479,
title = "Anticlockwise P-T evolution at ~280 Ma recorded from ultrahigh-temperature metapelitic granulite in the Chinese Altai orogenic belt, a possible link with the Tarim mantle plume?",
abstract = "An ultrahigh-temperature (UHT) metapelitic granulite assemblage consisting of garnet(g)-spinel(sp)-orthopyroxene(opx)-sillimanite(sil)-cordierite(cd)-ilmenite(ilm)-biotite(bi)-plagioclase(pl)-quartz(q) occurs within migmatitic paragneiss near Kalasu in the Chinese Altai, NW China. Textural relations, mineral compositions and P-T estimates, indicate three stages of mineral assemblages: (1) pre-peak prograde stage (M1) consisting of a sp-sil-bearing or sp-opx-bearing inclusion assemblage, with low-Al2O3 contents (4-5wt.{\%}) in orthopyroxene and P-T conditions of ~7kbar and ~890°C, (2) peak UHT stage (M2) comprising a g-opx-cd-bearing coarse-grained assemblage, with high-Al2O3 contents (8-9wt.{\%}) in orthopyroxene and peak conditions of ~8kbar and ~970°C, and (3) post-peak HT stage (M3) containing an oriented opx-bi-sil-bearing assemblage in matrix, with moderate amounts of Al2O3 (6-7wt.{\%}) in orthopyroxene and P-T conditions of 8-9kbar and ~870°C. The three discrete stages define an anticlockwise P-T path involving initial prograde heating and post-peak near isobaric cooling. Such a near isobaric cooling anticlockwise P-T path suggests that UHT metamorphism likely occurred in an overall extensional tectonic setting with associated underplating of mantle-derived mafic magma. A SHRIMP zircon U-Pb age of 278±2Ma obtained from the metapelitic granulite indicates UHT metamorphism in the Altai orogen occurred during the Permian, coeval with spacially associated mantle-derived mafic intrusions (~280Ma) and the Tarim mantle plume (~275Ma). Thus, the Permian UHT metamorphism of the Chinese Altai is likely associated with underplating and heating of mantle-derived mafic magma as a result of the Tarim mantle plume.",
keywords = "Mantle plume, P-T path, The Chinese Altai, U-Pb age, Ultrahigh-temperature metamorphism",
author = "Laixi Tong and Xu, {Yi Gang} and Cawood, {Peter A.} and Xin Zhou and Yibing Chen and Zhao Liu",
year = "2014",
doi = "10.1016/j.jseaes.2014.07.043",
language = "English",
volume = "94",
pages = "1--11",
journal = "Journal of Asian Earth Sciences",
issn = "1367-9120",
publisher = "Elsevier",

}

Anticlockwise P-T evolution at ~280 Ma recorded from ultrahigh-temperature metapelitic granulite in the Chinese Altai orogenic belt, a possible link with the Tarim mantle plume? / Tong, Laixi; Xu, Yi Gang; Cawood, Peter A.; Zhou, Xin; Chen, Yibing; Liu, Zhao.

In: Journal of Asian Earth Sciences, Vol. 94, 2014, p. 1-11.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - Anticlockwise P-T evolution at ~280 Ma recorded from ultrahigh-temperature metapelitic granulite in the Chinese Altai orogenic belt, a possible link with the Tarim mantle plume?

AU - Tong, Laixi

AU - Xu, Yi Gang

AU - Cawood, Peter A.

AU - Zhou, Xin

AU - Chen, Yibing

AU - Liu, Zhao

PY - 2014

Y1 - 2014

N2 - An ultrahigh-temperature (UHT) metapelitic granulite assemblage consisting of garnet(g)-spinel(sp)-orthopyroxene(opx)-sillimanite(sil)-cordierite(cd)-ilmenite(ilm)-biotite(bi)-plagioclase(pl)-quartz(q) occurs within migmatitic paragneiss near Kalasu in the Chinese Altai, NW China. Textural relations, mineral compositions and P-T estimates, indicate three stages of mineral assemblages: (1) pre-peak prograde stage (M1) consisting of a sp-sil-bearing or sp-opx-bearing inclusion assemblage, with low-Al2O3 contents (4-5wt.%) in orthopyroxene and P-T conditions of ~7kbar and ~890°C, (2) peak UHT stage (M2) comprising a g-opx-cd-bearing coarse-grained assemblage, with high-Al2O3 contents (8-9wt.%) in orthopyroxene and peak conditions of ~8kbar and ~970°C, and (3) post-peak HT stage (M3) containing an oriented opx-bi-sil-bearing assemblage in matrix, with moderate amounts of Al2O3 (6-7wt.%) in orthopyroxene and P-T conditions of 8-9kbar and ~870°C. The three discrete stages define an anticlockwise P-T path involving initial prograde heating and post-peak near isobaric cooling. Such a near isobaric cooling anticlockwise P-T path suggests that UHT metamorphism likely occurred in an overall extensional tectonic setting with associated underplating of mantle-derived mafic magma. A SHRIMP zircon U-Pb age of 278±2Ma obtained from the metapelitic granulite indicates UHT metamorphism in the Altai orogen occurred during the Permian, coeval with spacially associated mantle-derived mafic intrusions (~280Ma) and the Tarim mantle plume (~275Ma). Thus, the Permian UHT metamorphism of the Chinese Altai is likely associated with underplating and heating of mantle-derived mafic magma as a result of the Tarim mantle plume.

AB - An ultrahigh-temperature (UHT) metapelitic granulite assemblage consisting of garnet(g)-spinel(sp)-orthopyroxene(opx)-sillimanite(sil)-cordierite(cd)-ilmenite(ilm)-biotite(bi)-plagioclase(pl)-quartz(q) occurs within migmatitic paragneiss near Kalasu in the Chinese Altai, NW China. Textural relations, mineral compositions and P-T estimates, indicate three stages of mineral assemblages: (1) pre-peak prograde stage (M1) consisting of a sp-sil-bearing or sp-opx-bearing inclusion assemblage, with low-Al2O3 contents (4-5wt.%) in orthopyroxene and P-T conditions of ~7kbar and ~890°C, (2) peak UHT stage (M2) comprising a g-opx-cd-bearing coarse-grained assemblage, with high-Al2O3 contents (8-9wt.%) in orthopyroxene and peak conditions of ~8kbar and ~970°C, and (3) post-peak HT stage (M3) containing an oriented opx-bi-sil-bearing assemblage in matrix, with moderate amounts of Al2O3 (6-7wt.%) in orthopyroxene and P-T conditions of 8-9kbar and ~870°C. The three discrete stages define an anticlockwise P-T path involving initial prograde heating and post-peak near isobaric cooling. Such a near isobaric cooling anticlockwise P-T path suggests that UHT metamorphism likely occurred in an overall extensional tectonic setting with associated underplating of mantle-derived mafic magma. A SHRIMP zircon U-Pb age of 278±2Ma obtained from the metapelitic granulite indicates UHT metamorphism in the Altai orogen occurred during the Permian, coeval with spacially associated mantle-derived mafic intrusions (~280Ma) and the Tarim mantle plume (~275Ma). Thus, the Permian UHT metamorphism of the Chinese Altai is likely associated with underplating and heating of mantle-derived mafic magma as a result of the Tarim mantle plume.

KW - Mantle plume

KW - P-T path

KW - The Chinese Altai

KW - U-Pb age

KW - Ultrahigh-temperature metamorphism

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U2 - 10.1016/j.jseaes.2014.07.043

DO - 10.1016/j.jseaes.2014.07.043

M3 - Article

VL - 94

SP - 1

EP - 11

JO - Journal of Asian Earth Sciences

JF - Journal of Asian Earth Sciences

SN - 1367-9120

ER -