The Mangaroon Orogeny: Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton

Agnieszka M. Piechocka, Jian Wei Zi, Courtney J. Gregory, Stephen Sheppard, Fawna J. Korhonen, Ian C.W. Fitzsimons, Tim E. Johnson, Birger Rasmussen

Research output: Contribution to journalArticle

Abstract

The Capricorn Orogen records nearly one billion years of intraplate orogenesis within the West Australian Craton, although the processes responsible for this protracted, punctuated reworking remain unclear. Of the major tectonic events that affected the region, the 1680–1620 Ma Mangaroon Orogeny is one of the least-well understood, mainly due to a lack of direct ages for metamorphism, an absence of pressure (P)–temperature (T) constraints, and uncertainty regarding the duration of granitic magmatism that is spatially and, possibly, temporally associated with deformation. In this study we define the P–T–time (t) conditions associated with the Mangaroon Orogeny based on in situ SHRIMP U–Pb monazite and xenotime geochronology and calculated P–T pseudosections. Data from a pelitic migmatite constrain the timing of low–P, high–T metamorphism to 1691 ± 7 Ma at conditions of 665–755 °C and 2.7–4.3 kbar (~175–240 °C/kbar). Data from a garnet-bearing sillimanite–biotite pelitic gneiss suggests higher pressure during the clockwise prograde history at one locality. Furthermore, the onset of the metamorphism coincides with the oldest granites in the region (1695 ± 9 Ma), which constrain the onset of the Mangaroon Orogeny. Our results also show that deposition and burial of the precursor sediments occurred, at most, c. 70 million years before the onset of partial melting at c. 1695 Ma. Therefore, there was no long incubation period before the onset of orogenesis. We conclude that, unlike many of the Proterozoic orogenic events in Australia, the c. 1.7 Ga low-P, high-T metamorphism recorded in the upper crust in the Capricorn Orogen cannot be explained by a thermal lid model, but rather was synchronous with granitic magmatism.

Original languageEnglish
Article number105425
JournalPrecambrian Research
Volume333
DOIs
Publication statusPublished - 1 Oct 2019

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orogeny
craton
magmatism
metamorphism
Bearings (structural)
Geochronology
Garnets
Tectonics
Sediments
Melting
xenotime
migmatite
monazite
reworking
upper crust
geochronology
gneiss
partial melting
Proterozoic
garnet

Cite this

Piechocka, Agnieszka M. ; Zi, Jian Wei ; Gregory, Courtney J. ; Sheppard, Stephen ; Korhonen, Fawna J. ; Fitzsimons, Ian C.W. ; Johnson, Tim E. ; Rasmussen, Birger. / The Mangaroon Orogeny : Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton. In: Precambrian Research. 2019 ; Vol. 333.
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abstract = "The Capricorn Orogen records nearly one billion years of intraplate orogenesis within the West Australian Craton, although the processes responsible for this protracted, punctuated reworking remain unclear. Of the major tectonic events that affected the region, the 1680–1620 Ma Mangaroon Orogeny is one of the least-well understood, mainly due to a lack of direct ages for metamorphism, an absence of pressure (P)–temperature (T) constraints, and uncertainty regarding the duration of granitic magmatism that is spatially and, possibly, temporally associated with deformation. In this study we define the P–T–time (t) conditions associated with the Mangaroon Orogeny based on in situ SHRIMP U–Pb monazite and xenotime geochronology and calculated P–T pseudosections. Data from a pelitic migmatite constrain the timing of low–P, high–T metamorphism to 1691 ± 7 Ma at conditions of 665–755 °C and 2.7–4.3 kbar (~175–240 °C/kbar). Data from a garnet-bearing sillimanite–biotite pelitic gneiss suggests higher pressure during the clockwise prograde history at one locality. Furthermore, the onset of the metamorphism coincides with the oldest granites in the region (1695 ± 9 Ma), which constrain the onset of the Mangaroon Orogeny. Our results also show that deposition and burial of the precursor sediments occurred, at most, c. 70 million years before the onset of partial melting at c. 1695 Ma. Therefore, there was no long incubation period before the onset of orogenesis. We conclude that, unlike many of the Proterozoic orogenic events in Australia, the c. 1.7 Ga low-P, high-T metamorphism recorded in the upper crust in the Capricorn Orogen cannot be explained by a thermal lid model, but rather was synchronous with granitic magmatism.",
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The Mangaroon Orogeny : Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton. / Piechocka, Agnieszka M.; Zi, Jian Wei; Gregory, Courtney J.; Sheppard, Stephen; Korhonen, Fawna J.; Fitzsimons, Ian C.W.; Johnson, Tim E.; Rasmussen, Birger.

In: Precambrian Research, Vol. 333, 105425, 01.10.2019.

Research output: Contribution to journalArticle

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T2 - Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton

AU - Piechocka, Agnieszka M.

AU - Zi, Jian Wei

AU - Gregory, Courtney J.

AU - Sheppard, Stephen

AU - Korhonen, Fawna J.

AU - Fitzsimons, Ian C.W.

AU - Johnson, Tim E.

AU - Rasmussen, Birger

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AB - The Capricorn Orogen records nearly one billion years of intraplate orogenesis within the West Australian Craton, although the processes responsible for this protracted, punctuated reworking remain unclear. Of the major tectonic events that affected the region, the 1680–1620 Ma Mangaroon Orogeny is one of the least-well understood, mainly due to a lack of direct ages for metamorphism, an absence of pressure (P)–temperature (T) constraints, and uncertainty regarding the duration of granitic magmatism that is spatially and, possibly, temporally associated with deformation. In this study we define the P–T–time (t) conditions associated with the Mangaroon Orogeny based on in situ SHRIMP U–Pb monazite and xenotime geochronology and calculated P–T pseudosections. Data from a pelitic migmatite constrain the timing of low–P, high–T metamorphism to 1691 ± 7 Ma at conditions of 665–755 °C and 2.7–4.3 kbar (~175–240 °C/kbar). Data from a garnet-bearing sillimanite–biotite pelitic gneiss suggests higher pressure during the clockwise prograde history at one locality. Furthermore, the onset of the metamorphism coincides with the oldest granites in the region (1695 ± 9 Ma), which constrain the onset of the Mangaroon Orogeny. Our results also show that deposition and burial of the precursor sediments occurred, at most, c. 70 million years before the onset of partial melting at c. 1695 Ma. Therefore, there was no long incubation period before the onset of orogenesis. We conclude that, unlike many of the Proterozoic orogenic events in Australia, the c. 1.7 Ga low-P, high-T metamorphism recorded in the upper crust in the Capricorn Orogen cannot be explained by a thermal lid model, but rather was synchronous with granitic magmatism.

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KW - LPHT metamorphism

KW - Monazite

KW - Proterozoic

KW - U–Pb geochronology

KW - Xenotime

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