Petrogenesis and Tectonic Implications of the Kwangsian Orogen: Constraints from Geochemistry and Sr-Nd-Hf Isotopic Compositions of the Early Paleozoic Peraluminous and Aluminous Granitoids in Northern Guangdong, SE China

IF 3.7 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Xiaohui JIA, Xiaodi WANG, Xiaofei QIU, Wenqiang YANG
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Abstract

This study presents whole-rock major, trace elements and Sr-Nd-Hf isotopic compositions, as well as zircon U-Pb geochronological data, for the peraluminous and aluminous granitoids in northern Guangdong Province, South China, in order to investigate their petrogenesis and tectonic implications. The Qingzhou granodiorites (458.5–455.4 Ma) are peraluminous (A/CNK = 1.05–1.96). They have relatively high initial 87Sr/86Sr ratios (ISr = 0.7087–0.7148), low εNd(t) values (–11.2 to –10.1) and a variety of zircon εHf(t) values in the range –13.4 to +4.81. By contrast, the Damaoshan granodiorites (458.1 Ma) are metaluminous (A/CNK = 0.79–0.94) in composition, with ISr values of 0.7083 to 0.7110, εNd(t) values of –7.92 to –5.28 and zircon εHf(t) values of –8.69 to –2.06. The Gaoshou quartz diorites (449 Ma) are metaluminous-peraluminous. Their ISr values vary from 0.7104 to 0.7111 with εNd(t) values from –9.64 to –8.63. Geochemical data and Sr-Nd-Hf isotope compositions indicate that the Qingzhou, Damaoshan and Gaoshou intrusions are primarily derived from the partial melting of metagreywackes, tonalitic rocks and amphibolite, respectively. The crustal materials in northern Guangdong, from top to bottom, consist of Paleozoic sequences, metasediments with a Vp of < 6.0 km/s, metaigneous rocks with a Vp of 6.3–6.7 km/s and amphibolite with a Vp of ∼7.03 km/s.

Abstract Image

广仙造山带的岩石成因及其构造意义:粤北早古生代过铝质和铝质花岗岩类地球化学和Sr-Nd-Hf同位素组成的制约
本文通过对粤北过铝质和铝质花岗岩的全岩主量、微量元素、Sr-Nd-Hf同位素组成及锆石U-Pb年代学资料的研究,探讨了其岩石成因和构造意义。青州花岗闪长岩(458.5 ~ 455.4 Ma)为过铝质(A/CNK = 1.05 ~ 1.96)。它们具有较高的初始87Sr/86Sr比值(ISr = 0.7087 ~ 0.7148),较低的εNd(t)值(-11.2 ~ -10.1),锆石εHf(t)值介于-13.4 ~ +4.81之间。大茂山花岗闪长岩(458.1 Ma)主要为铝质(A/CNK = 0.79 ~ 0.94), ISr值为0.7083 ~ 0.7110,εNd(t)值为-7.92 ~ -5.28,锆石εHf(t)值为-8.69 ~ -2.06。高寿石英闪长岩(449 Ma)为金属-过铝质。ISr值为0.7104 ~ 0.7111,εNd(t)值为-9.64 ~ -8.63。地球化学资料和Sr-Nd-Hf同位素组成表明,青州岩体、大茂山岩体和高寿岩体主要来源于偏长辉砾岩、调质岩和角闪岩的部分熔融作用。粤北地壳物质由上至下依次为古生代层序、Vp为<的变质沉积;6.0 km/s, Vp为6.3-6.7 km/s的变质岩和Vp为~ 7.03 km/s的角闪岩。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Acta Geologica Sinica ‐ English Edition
Acta Geologica Sinica ‐ English Edition 地学-地球科学综合
CiteScore
3.00
自引率
12.10%
发文量
3039
审稿时长
6 months
期刊介绍: Acta Geologica Sinica mainly reports the latest and most important achievements in the theoretical and basic research in geological sciences, together with new technologies, in China. Papers published involve various aspects of research concerning geosciences and related disciplines, such as stratigraphy, palaeontology, origin and history of the Earth, structural geology, tectonics, mineralogy, petrology, geochemistry, geophysics, geology of mineral deposits, hydrogeology, engineering geology, environmental geology, regional geology and new theories and technologies of geological exploration.
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