Title of article :
Geochemistry, zircon U–Pb age and Hf isotope compositions of Paleoproterozoic aluminous A-type granites from the Kongling terrain, Yangtze Block: Constraints on petrogenesis and geologic implications
Author/Authors :
Peng، نويسنده , , Min and Wu، نويسنده , , Yuanbao and Gao، نويسنده , , Shan and Zhang، نويسنده , , Hongfei and Wang، نويسنده , , Jing and Liu، نويسنده , , Xiaochi and Gong، نويسنده , , Hujun and Zhou، نويسنده , , Lian and Hu، نويسنده , , Zhaochu and Liu، نويسنده , , Yongsheng and Yuan، نويسنده , , Honglin، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2012
Pages :
12
From page :
140
To page :
151
Abstract :
An integrated study of petrology, zircon U–Pb age, and geochemistry was reported for a Paleoproterozoic granitic pluton from the Kongling terrain in the northern part of the Yangtze Block. The Quanqitang pluton is composed mainly of alkali feldspar, quartz, biotite and plagioclase. Zircon U–Pb dating yields a 207Pb/206Pb age of ca.1.85 Ga, which represents its intrusion age. The Quanqitang pluton has high SiO2 (72.6–74.4 wt.%), K2O (5.09–5.56 wt.%) and Na2O (3.02–3.36 wt.%), and low Fe2O3 (2.56–3.19 wt.%) and MgO (0.25–0.37 wt.%). It is metaluminous (A/CNK = 0.93–0.98) and belongs to the high-K calc-alkaline series. On the chondrite-normalized REE diagram, all the samples invariably show a relatively enrichment in light rare earth elements (LREEs) with high (La/Yb)N ratios (10.6–21.7) and strong negative Eu anomalies. Their primitive-mantle normalized spidergrams display negative Ba, Nb, Ta, Sr, P, Eu and Ti anomalies. The calculated zirconium saturation temperatures range from 802 to 861 °C with an average of 845 °C. Zircons from the granites have εHf(t) values ranging from − 17.6 to − 20.9, corresponding to two-stage Hf modal ages of 3.6 to 3.8 Ga. Based on the geochemical features, it is inferred that the granites were generated by the dehydration melting of Archean tonalitic gneisses with a plagioclase-rich residual assemblage. The granites chemically belong to the A2-type granites, and have an intrusion age younger than the possible ca. 2.0 Ga collisional event in the Yangtze Block. This suggests that they formed in a post-collisional tectonic setting, and thus a tectonic regime switch from collision to extension might have occurred in the Yangtze Block before ca. 1.85 Ga. The occurrence of the A2-type granite indicates that the Kongling microcontinental block became a stabilized craton at ca. 1.85 Ga.
Keywords :
Yangtze Block , Paleoproterozoic , Aluminous A-type granite , Post-collisional , Cratonization
Journal title :
Gondwana Research
Serial Year :
2012
Journal title :
Gondwana Research
Record number :
2364272
Link To Document :
بازگشت