地质学报(英文版)2024,Vol.98Issue(1) :50-66.DOI:10.1111/1755-6724.15112

Petrogenesis and Tectonic Implications of the Early Triassic Nianzi Adakitic Granite Unit in the Yanshan Fold and Thrust Belt:New Constraints from U-Pb Geochronology and Sr-Nd-Hf Isotopes

ZHANG Huijun WU Chu HE Fubing WANG Biren CUI Yubin LIU Zhenghua YOU Shina DONG Jing
地质学报(英文版)2024,Vol.98Issue(1) :50-66.DOI:10.1111/1755-6724.15112

Petrogenesis and Tectonic Implications of the Early Triassic Nianzi Adakitic Granite Unit in the Yanshan Fold and Thrust Belt:New Constraints from U-Pb Geochronology and Sr-Nd-Hf Isotopes

ZHANG Huijun 1WU Chu 1HE Fubing 2WANG Biren 3CUI Yubin 2LIU Zhenghua 1YOU Shina 2DONG Jing2
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作者信息

  • 1. Development and Research Center of the China Geological Survey,Beijing 100037,China
  • 2. Beijing Institute of the Geological Survey,Beijing 100095,China
  • 3. Institute of Disaster Prevention,Langfang,Hebei 065201,China
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Abstract

The Nianzi granite unit,which includes the Nianzi,Xiaolianghou and Xiawopu granitic intrusions,is a significant component of the northern part of the North China Craton(NCC)and is situated in the Yanshan fold and thrust belt(YFTB).However,there is still debate regarding the tectonic evolutionary history of the YFTB during the late Permian to Triassic period,specifically regarding the timing of subduction and collision between the NCC and the Paleo-Asian Ocean.The Nianzi granite unit exhibits unique petrological,geochronological and geochemical signatures that shed light on the tectonic evolutionary history of the YFTB.This study presents detailed petrology,whole-rock geochemistry,together with Sr-Nd isotopic,zircon U-Pb dating and Lu-Hf isotopic data of the granites within the Nianzi granite unit.Our findings demonstrate that the granites primarily consist of subhedral K-feldspar,plagioclase,quartz,minor biotite and hornblende,with accessory titanite,apatite,magnetite and zircon.Zircon U-Pb dating indicates that the Xiaolianghou granite was emplaced at 247.5±0.62 Ma.Additionally,the adakitic characteristics of the Nianzi,Xiawopu and Xiaolianghou granitic intrusions,such as high Sr and Ba contents and high ratios of Sr/Y and(La/Yb)N,combined with negative Sr-Nd and Lu-Hf isotopes(87Sr/86Sr)i = 0.705681-0.7057433,εNd(t)=-21.98 to-20.97,zircon εHf(t)=-20.26 to-9.92),as well as the I-type granite features of high SiO2,Na2O and K2O/Na2O ratios,enriched Rb,K,Sr and Ba,along with depleted Th,U,Nb,Ta,P and Ti,suggest that the Nianzi granitic unit was mainly derived from the partial melting of a thickened lower crust containing hydrous,calc-alkaline to high-K calc-alkaline,mafic to intermediate metamorphic rocks.In light of these parameters,we further integrate our data with previous studies and conclude that the Nianzi granitic unit was generated in a post-collisional extensional environment during the Early Triassic.

Key words

tectonic evolution/zircon geochronology/Sr-Nd-Hf isotopes/Nianzi granite unit/Yanshan fold and thrust belt

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基金项目

National Natural Science Foundation of China(41872232)

Beijing Geological Survey Project(PXM 2016-158203-000008)

Beijing Geological Survey Project(PXM 2018-158203-000014)

Beijing Innovation Studio(Urban Geology,Active Structure,and Monitoring)()

出版年

2024
地质学报(英文版)
中国地质学会

地质学报(英文版)

CSTPCD
影响因子:1.414
ISSN:1000-9515
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