Tonian–Ediacaran evolution of the Brunovistulian microcontinent
(Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and
40Ar/39Ar muscovite ages

J 2023

Tonian–Ediacaran evolution of the Brunovistulian microcontinent (Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and 40Ar/39Ar muscovite ages

TIMMERMAN, Martin J.; Lukáš KRMÍČEK; Simona KRMÍČKOVÁ; Jiří SLÁMA; Masafumi SUDO et. al.

Základní údaje

Originální název

Tonian–Ediacaran evolution of the Brunovistulian microcontinent (Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and 40Ar/39Ar muscovite ages

Autoři

TIMMERMAN, Martin J.; Lukáš KRMÍČEK; Simona KRMÍČKOVÁ; Jiří SLÁMA; Masafumi SUDO a Edward SOBEL

Vydání

Precambrian Research, Elsevier, 2023, 0301-9268

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 3.200

Kód RIV

RIV/00216224:14310/23:00130408

Organizační jednotka

Přírodovědecká fakulta

DOI

https://doi.org/10.1016/j.precamres.2023.106981

UT WoS

000935239200001

EID Scopus

2-s2.0-85147263518

Klíčová slova anglicky

Brunovistulicum; Cryogenian; Ediacaran; Basal Clastics; U–Pb dating; Ar/Ar dating

Štítky

14315010, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 16. 3. 2023 10:50, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Granitoids of the Slavkov Domain of the Brunovistulian microcontinent (BVM) in the Czech Republic have Ediacaran U–Pb zircon crystallization ages with the dominant magmatic activity occurring between ca. 597 and 595 Ma. The ages overlap published ages for the adjacent Thaya Domain, showing that both domains formed coevally in the same subduction setting. The data support published models in which the Slavkov Domain formed as arc crust. The main stage of magmatism stopped after ca. 595–590 Ma and was quickly followed by cooling accompanied by intrusion of small volumes of rhyolite dykes at ca. 594 Ma. Slavkov Domain metasedimentary rocks are dominated by Cryogenian–Ediacaran detrital zircon populations and their protoliths were locally derived erosional products of Cryogenian to Ediacaran arc rocks of the Thaya and Slavkov domains. Metasedimentary rocks from the NE part of the BVM contain younger, ca. 550 Ma zircons indicating that the BVM grew northeastward by accretion of progressively younger material derived from magmatic rocks with latest Ediacaran crystallization ages. In contrast to the Thaya and Slavkov domains, the Metavolcanic Zone that lies between them formed between ca. 740 and 725 Ma in the late Tonian to early Cryogenian. It predates the main stage magmatic activity in the BVM by 135 to 150 Ma and is probably a relic of older crust that formed during rifting of the Rodinia supercontinent. At ca. 552–551 Ma in the latest Ediacaran, parts of the BVM were exposed at the surface, during which time red, terrestrial siliciclastic sediments (Basal Clastics) were deposited. These largely had (very) proximal sources such as the main stage granitoids of the Thaya and Slavkov domains. Clasts of (meta)sandstones contain much older zircon populations and provide evidence that Neoarchaean and Palaeo-, meso- and early Neoproterozoic crustal rocks were exposed in erosional position nearby.

Citovat

TIMMERMAN, Martin J.; Lukáš KRMÍČEK; Simona KRMÍČKOVÁ; Jiří SLÁMA; Masafumi SUDO a Edward SOBEL. Tonian–Ediacaran evolution of the Brunovistulian microcontinent (Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and 40Ar/39Ar muscovite ages. Precambrian Research. Elsevier, 2023, roč. 387, April, s. 1-20. ISSN 0301-9268. Dostupné z: https://doi.org/10.1016/j.precamres.2023.106981.

@article{2264277,
   author = {Timmerman, Martin J. and Krmíček, Lukáš and Krmíčková, Simona and Sláma, Jiří and Sudo, Masafumi and Sobel, Edward},
   article_number = {April},
   doi = {https://doi.org/10.1016/j.precamres.2023.106981},
   keywords = {Brunovistulicum; Cryogenian; Ediacaran; Basal Clastics; U–Pb dating; Ar/Ar dating},
   language = {eng},
   issn = {0301-9268},
   journal = {Precambrian Research},
   title = {Tonian–Ediacaran evolution of the Brunovistulian microcontinent (Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and 40Ar/39Ar muscovite ages},
   url = {https://doi.org/10.1016/j.precamres.2023.106981},
   volume = {387},
   year = {2023}
}

TY  - JOUR
ID  - 2264277
AU  - Timmerman, Martin J. - Krmíček, Lukáš - Krmíčková, Simona - Sláma, Jiří - Sudo, Masafumi - Sobel, Edward
PY  - 2023
TI  - Tonian–Ediacaran evolution of the Brunovistulian microcontinent (Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and 40Ar/39Ar muscovite ages
JF  - Precambrian Research
VL  - 387
IS  - April
SP  - 1-20
EP  - 1-20
PB  - Elsevier
SN  - 03019268
KW  - Brunovistulicum
KW  - Cryogenian
KW  - Ediacaran
KW  - Basal Clastics
KW  - U–Pb dating
KW  - Ar/Ar dating
UR  - https://doi.org/10.1016/j.precamres.2023.106981
N2  - Granitoids of the Slavkov Domain of the Brunovistulian microcontinent (BVM) in the Czech Republic have Ediacaran U–Pb zircon crystallization ages with the dominant magmatic activity occurring between ca. 597 and 595 Ma. The ages overlap published ages for the adjacent Thaya Domain, showing that both domains formed coevally in the same subduction setting. The data support published models in which the Slavkov Domain formed as arc crust. The main stage of magmatism stopped after ca. 595–590 Ma and was quickly followed by cooling accompanied by intrusion of small volumes of rhyolite dykes at ca. 594 Ma. Slavkov Domain metasedimentary rocks are dominated by Cryogenian–Ediacaran detrital zircon populations and their protoliths were locally derived erosional products of Cryogenian to Ediacaran arc rocks of the Thaya and Slavkov domains. Metasedimentary rocks from the NE part of the BVM contain younger, ca. 550 Ma zircons indicating that the BVM grew northeastward by accretion of progressively younger material derived from magmatic rocks with latest Ediacaran crystallization ages. In contrast to the Thaya and Slavkov domains, the Metavolcanic Zone that lies between them formed between ca. 740 and 725 Ma in the late Tonian to early Cryogenian. It predates the main stage magmatic activity in the BVM by 135 to 150 Ma and is probably a relic of older crust that formed during rifting of the Rodinia supercontinent. At ca. 552–551 Ma in the latest Ediacaran, parts of the BVM were exposed at the surface, during which time red, terrestrial siliciclastic sediments (Basal Clastics) were deposited. These largely had (very) proximal sources such as the main stage granitoids of the Thaya and Slavkov domains. Clasts of (meta)sandstones contain much older zircon populations and provide evidence that Neoarchaean and Palaeo-, meso- and early Neoproterozoic crustal rocks were exposed in erosional position nearby.
ER  -

TIMMERMAN, Martin J.; Lukáš KRMÍČEK; Simona KRMÍČKOVÁ; Jiří SLÁMA; Masafumi SUDO a Edward SOBEL. Tonian–Ediacaran evolution of the Brunovistulian microcontinent (Czech Republic) deciphered from LA-ICP-MS U–Pb zircon and 40Ar/39Ar muscovite ages. \textit{Precambrian Research}. Elsevier, 2023, roč.~387, April, s.~1-20. ISSN~0301-9268. Dostupné z: https://doi.org/10.1016/j.precamres.2023.106981.

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