Multi-stage metamorphism by progressive accretion of
continental blocks, example from the Western Hindu Kush

J 2020

Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush

MOINY, Hezbullah; Shah Wali FARYAD; Renata ČOPJAKOVÁ a Radim JEDLICKA

Základní údaje

Originální název

Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush

Autoři

MOINY, Hezbullah; Shah Wali FARYAD; Renata ČOPJAKOVÁ (203 Česká republika, garant, domácí) a Radim JEDLICKA

Vydání

Journal of metamorphic Geology, Hoboken, Wiley, 2020, 0263-4929

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 4.850

Kód RIV

RIV/00216224:14310/20:00116227

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.1111/jmg.12535

UT WoS

000545791300001

EID Scopus

2-s2.0-85087319746

Klíčová slova anglicky

crustal xenoliths; granitoids; Hindu Kush suture; metamorphism

Štítky

rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 15. 9. 2020 15:04, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Basement rocks from the Western Hindu Kush preserve evidence of multiple metamorphic and magmatic events that occurred along the boundary between the Archean-Proterozoic Afghan Central and Afghan-Tajik Blocks. To verify the different metamorphic stages or events, mineral textures and phase equilibria in metamorphic basement rocks and their age relations to magmatic episodes have been investigated. Quartzofeldspathic gneiss and migmatite with lenses of amphibolite (with assumed Proterozoic age for their metamorphism) are intruded by the Triassic Hindu Kush granitoid batholith and small Cretaceous and Oligocene granite intrusions. The age of thermal overprint (210-170 Ma) by the Triassic batholith is confirmed by new monazite data. Both Triassic and Cretaceous granitoids and surrounding basement rocks underwent subsequent metamorphism up to epidote-amphibolite facies. The degree of this metamorphism increases southward at the contact to the Kabul Block, which under-plates the Western Hindu Kush from the south. An early Miocene age was obtained by Pb-Th analyses in thorite and huttonite, which are close or slightly younger than the Oligocene granite in this area. The Cretaceous meta-granodiorite near the border with the Kabul Block contains xenoliths of granulite facies rocks that could come from the Neoarchean granulite facies basement of the Kabul Block. The multi-stage metamorphic and magmatic evolution classifies the Hindu Kush mountain belt as a long-lived suture zone that was active since the early Palaeozoic. The results of this study support the interpretation about possible relations of the Afghan Central Blocks to the southern margin of Eurasia during the evolution of Para- and Neotethys.

Citovat

MOINY, Hezbullah; Shah Wali FARYAD; Renata ČOPJAKOVÁ a Radim JEDLICKA. Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush. Journal of metamorphic Geology. Hoboken: Wiley, 2020, roč. 38, č. 7, s. 693-717. ISSN 0263-4929. Dostupné z: https://doi.org/10.1111/jmg.12535.

@article{1674657,
   author = {Moiny, Hezbullah and Faryad, Shah Wali and Čopjaková, Renata and Jedlicka, Radim},
   article_location = {Hoboken},
   article_number = {7},
   doi = {https://doi.org/10.1111/jmg.12535},
   keywords = {crustal xenoliths; granitoids; Hindu Kush suture; metamorphism},
   language = {eng},
   issn = {0263-4929},
   journal = {Journal of metamorphic Geology},
   title = {Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush},
   url = {https://doi.org/10.1111/jmg.12535},
   volume = {38},
   year = {2020}
}

TY  - JOUR
ID  - 1674657
AU  - Moiny, Hezbullah - Faryad, Shah Wali - Čopjaková, Renata - Jedlicka, Radim
PY  - 2020
TI  - Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush
JF  - Journal of metamorphic Geology
VL  - 38
IS  - 7
SP  - 693-717
EP  - 693-717
PB  - Wiley
SN  - 02634929
KW  - crustal xenoliths
KW  - granitoids
KW  - Hindu Kush suture
KW  - metamorphism
UR  - https://doi.org/10.1111/jmg.12535
L2  - https://doi.org/10.1111/jmg.12535
N2  - Basement rocks from the Western Hindu Kush preserve evidence of multiple metamorphic and magmatic events that occurred along the boundary between the Archean-Proterozoic Afghan Central and Afghan-Tajik Blocks. To verify the different metamorphic stages or events, mineral textures and phase equilibria in metamorphic basement rocks and their age relations to magmatic episodes have been investigated. Quartzofeldspathic gneiss and migmatite with lenses of amphibolite (with assumed Proterozoic age for their metamorphism) are intruded by the Triassic Hindu Kush granitoid batholith and small Cretaceous and Oligocene granite intrusions. The age of thermal overprint (210-170 Ma) by the Triassic batholith is confirmed by new monazite data. Both Triassic and Cretaceous granitoids and surrounding basement rocks underwent subsequent metamorphism up to epidote-amphibolite facies. The degree of this metamorphism increases southward at the contact to the Kabul Block, which under-plates the Western Hindu Kush from the south. An early Miocene age was obtained by Pb-Th analyses in thorite and huttonite, which are close or slightly younger than the Oligocene granite in this area. The Cretaceous meta-granodiorite near the border with the Kabul Block contains xenoliths of granulite facies rocks that could come from the Neoarchean granulite facies basement of the Kabul Block. The multi-stage metamorphic and magmatic evolution classifies the Hindu Kush mountain belt as a long-lived suture zone that was active since the early Palaeozoic. The results of this study support the interpretation about possible relations of the Afghan Central Blocks to the southern margin of Eurasia during the evolution of Para- and Neotethys.
ER  -

MOINY, Hezbullah; Shah Wali FARYAD; Renata ČOPJAKOVÁ a Radim JEDLICKA. Multi-stage metamorphism by progressive accretion of continental blocks, example from the Western Hindu Kush. \textit{Journal of metamorphic Geology}. Hoboken: Wiley, 2020, roč.~38, č.~7, s.~693-717. ISSN~0263-4929. Dostupné z: https://doi.org/10.1111/jmg.12535.

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