Early Neoproterozoic accretionary assemblage in the Cathaysia Block : Geochronological, Lu-Hf isotopic and geochemical evidence from granitoid gneisses

Yuejun WANG*, Yuzhi ZHANG, Weiming FAN, Hongyan GENG, Heping ZOU, Xianwu BI

*Corresponding author for this work

Research output: Journal PublicationsJournal Article (refereed)

60 Citations (Scopus)

Abstract

The South China Block (SCB) is composed of the Yangtze Block in the northwest and the Cathysia Block in the southeast. The earliest Neoproterozoic granitic rocks in the SCB are important for our understanding of the tectonic regime and location of this ancient continent in relation to the Rodinia supercontinent. However, such rocks have rarely been reported for the Cathaysia Block so far. In this study, six granitic gneisses from the Wuyi-Yunkai domain gave zircon U-Pb ages of 985-913Ma, indicating the presence of the early Neoproterozoic granitic magmatism in the Cathaysia interior. These granitic gneisses are peraluminous with high FeOt, MgO, TiO2 and CaO/Na2O but low SiO2, Al2O3/TiO2, Al2O3/(MgO+FeOt) and Rb/Sr ratios. They show steep REE chondrite-normalized patterns with δEu values of 0.35-0.70. These samples have strongly negative Ba, Sr, Nb-Ta, P and Ti anomalies in primitive mantle-normalized diagrams, and e{open}Nd(t) values of -9.54 to -3.81, similar to those of the Kwangsian granitic rocks and Precambrian volcanosedimentary package in the Cathysia Block. The zircon grains with the earliest Neoproterozoic age gave e{open}Hf(t) values of -9.64 to +2.78 with the peak values at -2.5 and -7.5, and Hf model ages of 1.35-2.00Ga with the two-peaks of 1.57Ga and 1.75Ga, respectively. These data suggest that the granitic gneisses originated dominantly from a binary mixing of metapelitic and metaigneous components, with insignificant input of juvenile materials. We consider that these rocks are closely related to the closure of the earliest Neoproterozoic (~980Ma) Wuyi-Yunkai back-arc basin in an accretionary continental margin setting. In combination with other data, it is proposed that the previously-defined Cathaysia block might consist of various sub-blocks separated by the arc-back-arc basin prior to the early Neoproterozoic period. The Wuyi-Yunkai arc-back-arc system was finally closed at ~920Ma, significantly younger than the classical Grenvillian Orogenic event, and thus the SCB was located on the margin of the Rodinia supercontinent.

Original languageEnglish
Pages (from-to)144-161
Number of pages18
JournalPrecambrian Research
Volume249
Early online date21 May 2014
DOIs
Publication statusPublished - Aug 2014
Externally publishedYes

Fingerprint

granitoid
Rocks
Rodinia
supercontinent
rock
zircon
Grenvillian orogeny
Tectonics
chondrite
basin
continental margin
magmatism
Precambrian
rare earth element
diagram
mantle
anomaly
tectonics

Keywords

  • Accretionary assemblage
  • Cathaysia
  • Early neoproterozoic granitic gneiss
  • Geochemistry
  • Lu-Hf isotopic composition
  • Zircon U-Pb geochronology

Cite this

@article{02e2a27f3c814e428126c8fa8fead738,
title = "Early Neoproterozoic accretionary assemblage in the Cathaysia Block : Geochronological, Lu-Hf isotopic and geochemical evidence from granitoid gneisses",
abstract = "The South China Block (SCB) is composed of the Yangtze Block in the northwest and the Cathysia Block in the southeast. The earliest Neoproterozoic granitic rocks in the SCB are important for our understanding of the tectonic regime and location of this ancient continent in relation to the Rodinia supercontinent. However, such rocks have rarely been reported for the Cathaysia Block so far. In this study, six granitic gneisses from the Wuyi-Yunkai domain gave zircon U-Pb ages of 985-913Ma, indicating the presence of the early Neoproterozoic granitic magmatism in the Cathaysia interior. These granitic gneisses are peraluminous with high FeOt, MgO, TiO2 and CaO/Na2O but low SiO2, Al2O3/TiO2, Al2O3/(MgO+FeOt) and Rb/Sr ratios. They show steep REE chondrite-normalized patterns with δEu values of 0.35-0.70. These samples have strongly negative Ba, Sr, Nb-Ta, P and Ti anomalies in primitive mantle-normalized diagrams, and e{open}Nd(t) values of -9.54 to -3.81, similar to those of the Kwangsian granitic rocks and Precambrian volcanosedimentary package in the Cathysia Block. The zircon grains with the earliest Neoproterozoic age gave e{open}Hf(t) values of -9.64 to +2.78 with the peak values at -2.5 and -7.5, and Hf model ages of 1.35-2.00Ga with the two-peaks of 1.57Ga and 1.75Ga, respectively. These data suggest that the granitic gneisses originated dominantly from a binary mixing of metapelitic and metaigneous components, with insignificant input of juvenile materials. We consider that these rocks are closely related to the closure of the earliest Neoproterozoic (~980Ma) Wuyi-Yunkai back-arc basin in an accretionary continental margin setting. In combination with other data, it is proposed that the previously-defined Cathaysia block might consist of various sub-blocks separated by the arc-back-arc basin prior to the early Neoproterozoic period. The Wuyi-Yunkai arc-back-arc system was finally closed at ~920Ma, significantly younger than the classical Grenvillian Orogenic event, and thus the SCB was located on the margin of the Rodinia supercontinent.",
keywords = "Accretionary assemblage, Cathaysia, Early neoproterozoic granitic gneiss, Geochemistry, Lu-Hf isotopic composition, Zircon U-Pb geochronology",
author = "Yuejun WANG and Yuzhi ZHANG and Weiming FAN and Hongyan GENG and Heping ZOU and Xianwu BI",
year = "2014",
month = "8",
doi = "10.1016/j.precamres.2014.05.003",
language = "English",
volume = "249",
pages = "144--161",
journal = "Precambrian Research",
issn = "0301-9268",
publisher = "Elsevier",

}

Early Neoproterozoic accretionary assemblage in the Cathaysia Block : Geochronological, Lu-Hf isotopic and geochemical evidence from granitoid gneisses. / WANG, Yuejun; ZHANG, Yuzhi; FAN, Weiming; GENG, Hongyan; ZOU, Heping; BI, Xianwu.

In: Precambrian Research, Vol. 249, 08.2014, p. 144-161.

Research output: Journal PublicationsJournal Article (refereed)

TY - JOUR

T1 - Early Neoproterozoic accretionary assemblage in the Cathaysia Block : Geochronological, Lu-Hf isotopic and geochemical evidence from granitoid gneisses

AU - WANG, Yuejun

AU - ZHANG, Yuzhi

AU - FAN, Weiming

AU - GENG, Hongyan

AU - ZOU, Heping

AU - BI, Xianwu

PY - 2014/8

Y1 - 2014/8

N2 - The South China Block (SCB) is composed of the Yangtze Block in the northwest and the Cathysia Block in the southeast. The earliest Neoproterozoic granitic rocks in the SCB are important for our understanding of the tectonic regime and location of this ancient continent in relation to the Rodinia supercontinent. However, such rocks have rarely been reported for the Cathaysia Block so far. In this study, six granitic gneisses from the Wuyi-Yunkai domain gave zircon U-Pb ages of 985-913Ma, indicating the presence of the early Neoproterozoic granitic magmatism in the Cathaysia interior. These granitic gneisses are peraluminous with high FeOt, MgO, TiO2 and CaO/Na2O but low SiO2, Al2O3/TiO2, Al2O3/(MgO+FeOt) and Rb/Sr ratios. They show steep REE chondrite-normalized patterns with δEu values of 0.35-0.70. These samples have strongly negative Ba, Sr, Nb-Ta, P and Ti anomalies in primitive mantle-normalized diagrams, and e{open}Nd(t) values of -9.54 to -3.81, similar to those of the Kwangsian granitic rocks and Precambrian volcanosedimentary package in the Cathysia Block. The zircon grains with the earliest Neoproterozoic age gave e{open}Hf(t) values of -9.64 to +2.78 with the peak values at -2.5 and -7.5, and Hf model ages of 1.35-2.00Ga with the two-peaks of 1.57Ga and 1.75Ga, respectively. These data suggest that the granitic gneisses originated dominantly from a binary mixing of metapelitic and metaigneous components, with insignificant input of juvenile materials. We consider that these rocks are closely related to the closure of the earliest Neoproterozoic (~980Ma) Wuyi-Yunkai back-arc basin in an accretionary continental margin setting. In combination with other data, it is proposed that the previously-defined Cathaysia block might consist of various sub-blocks separated by the arc-back-arc basin prior to the early Neoproterozoic period. The Wuyi-Yunkai arc-back-arc system was finally closed at ~920Ma, significantly younger than the classical Grenvillian Orogenic event, and thus the SCB was located on the margin of the Rodinia supercontinent.

AB - The South China Block (SCB) is composed of the Yangtze Block in the northwest and the Cathysia Block in the southeast. The earliest Neoproterozoic granitic rocks in the SCB are important for our understanding of the tectonic regime and location of this ancient continent in relation to the Rodinia supercontinent. However, such rocks have rarely been reported for the Cathaysia Block so far. In this study, six granitic gneisses from the Wuyi-Yunkai domain gave zircon U-Pb ages of 985-913Ma, indicating the presence of the early Neoproterozoic granitic magmatism in the Cathaysia interior. These granitic gneisses are peraluminous with high FeOt, MgO, TiO2 and CaO/Na2O but low SiO2, Al2O3/TiO2, Al2O3/(MgO+FeOt) and Rb/Sr ratios. They show steep REE chondrite-normalized patterns with δEu values of 0.35-0.70. These samples have strongly negative Ba, Sr, Nb-Ta, P and Ti anomalies in primitive mantle-normalized diagrams, and e{open}Nd(t) values of -9.54 to -3.81, similar to those of the Kwangsian granitic rocks and Precambrian volcanosedimentary package in the Cathysia Block. The zircon grains with the earliest Neoproterozoic age gave e{open}Hf(t) values of -9.64 to +2.78 with the peak values at -2.5 and -7.5, and Hf model ages of 1.35-2.00Ga with the two-peaks of 1.57Ga and 1.75Ga, respectively. These data suggest that the granitic gneisses originated dominantly from a binary mixing of metapelitic and metaigneous components, with insignificant input of juvenile materials. We consider that these rocks are closely related to the closure of the earliest Neoproterozoic (~980Ma) Wuyi-Yunkai back-arc basin in an accretionary continental margin setting. In combination with other data, it is proposed that the previously-defined Cathaysia block might consist of various sub-blocks separated by the arc-back-arc basin prior to the early Neoproterozoic period. The Wuyi-Yunkai arc-back-arc system was finally closed at ~920Ma, significantly younger than the classical Grenvillian Orogenic event, and thus the SCB was located on the margin of the Rodinia supercontinent.

KW - Accretionary assemblage

KW - Cathaysia

KW - Early neoproterozoic granitic gneiss

KW - Geochemistry

KW - Lu-Hf isotopic composition

KW - Zircon U-Pb geochronology

UR - http://www.scopus.com/inward/record.url?scp=84901746805&partnerID=8YFLogxK

U2 - 10.1016/j.precamres.2014.05.003

DO - 10.1016/j.precamres.2014.05.003

M3 - Journal Article (refereed)

AN - SCOPUS:84901746805

VL - 249

SP - 144

EP - 161

JO - Precambrian Research

JF - Precambrian Research

SN - 0301-9268

ER -