Standard

Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton) : U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes. / Shatsky, V. S.; Malkovets, V. G.; Belousova, E. A. и др.

в: Precambrian Research, Том 282, 01.09.2016, стр. 1-20.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Shatsky, VS, Malkovets, VG, Belousova, EA, Tretiakova, IG, Griffin, WL, Ragozin, AL, Gibsher, AA & O'Reilly, SY 2016, 'Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton): U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes', Precambrian Research, Том. 282, стр. 1-20. https://doi.org/10.1016/j.precamres.2016.06.022

APA

Shatsky, V. S., Malkovets, V. G., Belousova, E. A., Tretiakova, I. G., Griffin, W. L., Ragozin, A. L., Gibsher, A. A., & O'Reilly, S. Y. (2016). Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton): U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes. Precambrian Research, 282, 1-20. https://doi.org/10.1016/j.precamres.2016.06.022

Vancouver

Shatsky VS, Malkovets VG, Belousova EA, Tretiakova IG, Griffin WL, Ragozin AL и др. Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton): U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes. Precambrian Research. 2016 сент. 1;282:1-20. doi: 10.1016/j.precamres.2016.06.022

Author

Shatsky, V. S. ; Malkovets, V. G. ; Belousova, E. A. и др. / Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton) : U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes. в: Precambrian Research. 2016 ; Том 282. стр. 1-20.

BibTeX

@article{e6c035653b6d4244a21c53386be96365,
title = "Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton): U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes",
abstract = "U–Pb age and Hf-isotope data were collected on zircons from crustal xenoliths from the Late Devonian kimberlite pipes of Markha terrane. The xenoliths include mafic garnet granulites (Gt+Pl+Cpx±Opx±Amp±Bt±Scp) and garnet–biotite gneisses (Grt+Bt+Pl+Kfs+Qtz±Scp). The data from this study demonstrate that the crust of the Markha terrane experienced several tectonothermal events. Zircons with Archean Hf model ages (TDM = 3.13–2.5 Ga) are predominant in all xenoliths with one exception. These data imply that most of the lower and middle crust beneath the Markha terrane was produced in the Archean time. Later this Paleoarchean crust was significantly reworked in several tectonothermal events, including a Neoarchean stage (2.9–2.5 Ga), and several Paleoproterozoic metamorphic stages (1.98, 1.9 and 1.8 Ga). There is very little evidence for generation of juvenile crust associated with these metamorphic events. Importantly, crustal xenoliths from kimberlite pipes of the Markha terrane record all the same events that occurred in the adjacent Daldyn and Magan terranes.",
keywords = "Continental crust evolution, Crustal xenoliths, Lu–Hf isotope system, U–Pb dating, Yakutian kimberlite province, Zircon",
author = "Shatsky, {V. S.} and Malkovets, {V. G.} and Belousova, {E. A.} and Tretiakova, {I. G.} and Griffin, {W. L.} and Ragozin, {A. L.} and Gibsher, {A. A.} and O'Reilly, {S. Y.}",
year = "2016",
month = sep,
day = "1",
doi = "10.1016/j.precamres.2016.06.022",
language = "English",
volume = "282",
pages = "1--20",
journal = "Precambrian Research",
issn = "0301-9268",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Tectonothermal evolution of the continental crust beneath the Yakutian diamondiferous province (Siberian craton)

T2 - U–Pb and Hf isotopic evidence on zircons from crustal xenoliths of kimberlite pipes

AU - Shatsky, V. S.

AU - Malkovets, V. G.

AU - Belousova, E. A.

AU - Tretiakova, I. G.

AU - Griffin, W. L.

AU - Ragozin, A. L.

AU - Gibsher, A. A.

AU - O'Reilly, S. Y.

PY - 2016/9/1

Y1 - 2016/9/1

N2 - U–Pb age and Hf-isotope data were collected on zircons from crustal xenoliths from the Late Devonian kimberlite pipes of Markha terrane. The xenoliths include mafic garnet granulites (Gt+Pl+Cpx±Opx±Amp±Bt±Scp) and garnet–biotite gneisses (Grt+Bt+Pl+Kfs+Qtz±Scp). The data from this study demonstrate that the crust of the Markha terrane experienced several tectonothermal events. Zircons with Archean Hf model ages (TDM = 3.13–2.5 Ga) are predominant in all xenoliths with one exception. These data imply that most of the lower and middle crust beneath the Markha terrane was produced in the Archean time. Later this Paleoarchean crust was significantly reworked in several tectonothermal events, including a Neoarchean stage (2.9–2.5 Ga), and several Paleoproterozoic metamorphic stages (1.98, 1.9 and 1.8 Ga). There is very little evidence for generation of juvenile crust associated with these metamorphic events. Importantly, crustal xenoliths from kimberlite pipes of the Markha terrane record all the same events that occurred in the adjacent Daldyn and Magan terranes.

AB - U–Pb age and Hf-isotope data were collected on zircons from crustal xenoliths from the Late Devonian kimberlite pipes of Markha terrane. The xenoliths include mafic garnet granulites (Gt+Pl+Cpx±Opx±Amp±Bt±Scp) and garnet–biotite gneisses (Grt+Bt+Pl+Kfs+Qtz±Scp). The data from this study demonstrate that the crust of the Markha terrane experienced several tectonothermal events. Zircons with Archean Hf model ages (TDM = 3.13–2.5 Ga) are predominant in all xenoliths with one exception. These data imply that most of the lower and middle crust beneath the Markha terrane was produced in the Archean time. Later this Paleoarchean crust was significantly reworked in several tectonothermal events, including a Neoarchean stage (2.9–2.5 Ga), and several Paleoproterozoic metamorphic stages (1.98, 1.9 and 1.8 Ga). There is very little evidence for generation of juvenile crust associated with these metamorphic events. Importantly, crustal xenoliths from kimberlite pipes of the Markha terrane record all the same events that occurred in the adjacent Daldyn and Magan terranes.

KW - Continental crust evolution

KW - Crustal xenoliths

KW - Lu–Hf isotope system

KW - U–Pb dating

KW - Yakutian kimberlite province

KW - Zircon

UR - http://www.scopus.com/inward/record.url?scp=84978063174&partnerID=8YFLogxK

U2 - 10.1016/j.precamres.2016.06.022

DO - 10.1016/j.precamres.2016.06.022

M3 - Article

AN - SCOPUS:84978063174

VL - 282

SP - 1

EP - 20

JO - Precambrian Research

JF - Precambrian Research

SN - 0301-9268

ER -

ID: 25794262