U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong

This paper carried out a study on U–Th–Pb behavior of zircons in a “dry” rock system during high-grade metamorphism in the Archean basement of eastern Shandong. The studied sample has a mineral assemblage of plagioclase + K-feldspar + clinopyroxene + biotite + quartz and its protolith is considered...

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Main Authors: Yusheng Wan, Dunyi Liu, Chunyan Dong, Shoujie Liu, Shijin Wang, Enxiu Yang
Format: Article
Language:English
Published: Elsevier 2011-04-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987111000259
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author Yusheng Wan
Dunyi Liu
Chunyan Dong
Shoujie Liu
Shijin Wang
Enxiu Yang
author_facet Yusheng Wan
Dunyi Liu
Chunyan Dong
Shoujie Liu
Shijin Wang
Enxiu Yang
author_sort Yusheng Wan
collection DOAJ
description This paper carried out a study on U–Th–Pb behavior of zircons in a “dry” rock system during high-grade metamorphism in the Archean basement of eastern Shandong. The studied sample has a mineral assemblage of plagioclase + K-feldspar + clinopyroxene + biotite + quartz and its protolith is considered to be diorite. The zircons are stubby, equant or irregular in shape and show fir-leaf, sectorial, banded or oscillatory zoning. They contain inclusions, including mineral assemblages of clinopyroxene + orthopyroxene + hornblende + quartz and plagioclase + K-feldspar + biotite + quartz. Fifty SHRIMP analyses were performed on 34 zircon grains, which commonly yielded high Th/U ratios (mostly >0.5). Most analyses are distributed along concordia from 2.54 to 2.25 Ga, with the youngest age being ∼1.95 Ga. Compositions and ages show large variations even in a same zircon grain. Combined with early studies, conclusions can be drawn as follows: 1) the diorite underwent two episodes of high-grade metamorphism, at the end of the Neoarchean and the Paleoproterozoic (∼2.50 Ga and ∼1.95 Ga or slightly later); 2) high-grade metamorphism in a “dry” rock system may partially reset the U–Th–Pb system of zircons and, in this case, the ages between the oldest and youngest are chronologically meaningless; and 3) high Th/U ratios may be common features of zircons formed during high-grade metamorphic conditions.
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spelling doaj.art-cdf488d4dbb8459e8feb61fb1f93c8dd2023-08-02T08:23:36ZengElsevierGeoscience Frontiers1674-98712011-04-012213714610.1016/j.gsf.2011.02.004U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern ShandongYusheng Wan0Dunyi Liu1Chunyan Dong2Shoujie Liu3Shijin Wang4Enxiu Yang5Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaBeijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaBeijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaBeijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, ChinaShandong Geological Survey, Jinan 250013, ChinaShandong Geological Survey, Jinan 250013, ChinaThis paper carried out a study on U–Th–Pb behavior of zircons in a “dry” rock system during high-grade metamorphism in the Archean basement of eastern Shandong. The studied sample has a mineral assemblage of plagioclase + K-feldspar + clinopyroxene + biotite + quartz and its protolith is considered to be diorite. The zircons are stubby, equant or irregular in shape and show fir-leaf, sectorial, banded or oscillatory zoning. They contain inclusions, including mineral assemblages of clinopyroxene + orthopyroxene + hornblende + quartz and plagioclase + K-feldspar + biotite + quartz. Fifty SHRIMP analyses were performed on 34 zircon grains, which commonly yielded high Th/U ratios (mostly >0.5). Most analyses are distributed along concordia from 2.54 to 2.25 Ga, with the youngest age being ∼1.95 Ga. Compositions and ages show large variations even in a same zircon grain. Combined with early studies, conclusions can be drawn as follows: 1) the diorite underwent two episodes of high-grade metamorphism, at the end of the Neoarchean and the Paleoproterozoic (∼2.50 Ga and ∼1.95 Ga or slightly later); 2) high-grade metamorphism in a “dry” rock system may partially reset the U–Th–Pb system of zircons and, in this case, the ages between the oldest and youngest are chronologically meaningless; and 3) high Th/U ratios may be common features of zircons formed during high-grade metamorphic conditions.http://www.sciencedirect.com/science/article/pii/S1674987111000259ZirconsU–Th–Pb systemResetHigh-grade metamorphismSHRIMP datingEarly Precambrian
spellingShingle Yusheng Wan
Dunyi Liu
Chunyan Dong
Shoujie Liu
Shijin Wang
Enxiu Yang
U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong
Geoscience Frontiers
Zircons
U–Th–Pb system
Reset
High-grade metamorphism
SHRIMP dating
Early Precambrian
title U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong
title_full U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong
title_fullStr U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong
title_full_unstemmed U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong
title_short U–Th–Pb behavior of zircons under high-grade metamorphic conditions: A case study of zircon dating of meta-diorite near Qixia, eastern Shandong
title_sort u th pb behavior of zircons under high grade metamorphic conditions a case study of zircon dating of meta diorite near qixia eastern shandong
topic Zircons
U–Th–Pb system
Reset
High-grade metamorphism
SHRIMP dating
Early Precambrian
url http://www.sciencedirect.com/science/article/pii/S1674987111000259
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