蚌埠隆起区古元古代钾长花岗岩的成因: 岩石地球化学、锆石U-Pb年代学与Hf同位素的制约

杨德彬; 许文良; 裴福萍; 王清海

蚌埠隆起区古元古代钾长花岗岩的成因: 岩石地球化学、锆石U-Pb年代学与Hf同位素的制约

1.
吉林大学地球科学学院, 吉林长春 130061
2.
吉林大学东北亚国际地学研究与教学中心, 吉林长春 130026

基金项目:

国家自然科学基金项目 90814003

国家自然科学基金项目 40472033

详细信息

作者简介:
杨德彬(1979-), 男, 博士研究生, 矿物学、岩石学、矿床学专业

通讯作者:
许文良, E-mail: xuwl@jlu.edu.cn

中图分类号: P597
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出版历程
- 收稿日期: 2008-10-10
- 刊出日期: 2009-01-25

Petrogenesis of the Paleoproterozoic K-Feldspar Granites in Bengbu Uplift: Constraints from Petro-Geochemistry, Zircon U-Pb Dating and Hf Isotope

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
International Centre for Geoscience Research and Education in Northeast Asia, Jilin University, Changchun 130026, China

摘要

摘要: 对蚌埠隆起区庄子里和磨盘山钾长花岗岩进行了系统的年代学和地球化学以及锆石Hf同位素的研究, 以便对其岩石成因进行约束.研究结果表明, 庄子里和磨盘山钾长花岗岩中锆石发育震荡生长环带, 且具有较高的Th/U比值(0.13~1.47), 反映了岩浆成因特征.对庄子里和磨盘山钾长花岗岩中岩浆锆石进行的LA-ICP-MSU-Pb定年结果(上交点年龄) 分别为2104±20Ma和2196±190Ma, 这表明蚌埠隆起区钾长花岗岩的形成时代为古元古代.钾长花岗岩的SiO₂和K₂O含量分别介于69.65%~77.95%和4.98%~5.17%之间; 该类岩石富集轻稀土元素和Zr、Hf、Rb、Th、U等元素, 明显亏损Ba、Sr、Eu、P和Ti等元素; 它们的ε_Nd(t) 值变化于-3.4~+3.2之间, Nd的模式年龄变化于2.31~2.79Ga之间; 钾长花岗岩中锆石的ε_Hf(t) 值和Hf同位素两阶段模式年龄分别介于-5.1~+7.8和2.26~2.83Ga之间.上述特征表明, 蚌埠隆起区钾长花岗岩的原始岩浆起源于有少量古老地壳物质涉入的新生下地壳的部分熔融.庄子里和磨盘山钾长花岗岩为A型花岗岩, 形成于伸展的构造背景.
- 古元古代 /
- 钾长花岗岩 /
- 年代学 /
- 地球化学 /
- Hf同位素 /
- 蚌埠隆起
Abstract: The study on the chronology, geochemistry and zircon Hf isotopes of the Zhuangzili and Mopanshan K-feldspar granites in Bengbu uplift was carried out in order to constrain their petrogenesis.Zircons from the intrusions display oscillatory zoning and high Th/U ratios (0.13-1.47), implying their magmatic origin.Zircon LA-ICP-MS, U-Pb dating results of the Zhuangzili and Mopanshan K-feldspar granites indicate that they formed in Paleoproterozoic with the upper intercept ages of 2104±20Ma and 2196±190Ma, respectively.Their SiO₂ and K₂O contents range from 69.65 to 77.95% and 4.98 to 5.17%, respectively.Moreover, the K-feldspar granites are enriched with light rare earth elements as well as Zr, Hf, Rb, Th, and U, while markedly depleted in Ba, Sr, Eu, P and Ti.Their ε_Nd(t) values vary from-3.4 to +3.2 and Nd model ages range from 2.31 to 2.79Ga.Their initial Hf isotope ratios and Hf two-stage model ages range from-5.1 to +7.8 and 2.26 to 2.83Ga, respectively.Taken together, it is suggested that the primary magma for the K-feldspar granites could be mainly derived from partial melting of the Paleoproterzoic and Neoarchean juvenile crust and that a small amount of ancient crustal material was involved in their origin.Chemically, these K-feldspar granites are A-type ones, implying that they formed under an extensional tectonic setting.
- Paleoproterozoic /
- K-feldspar granite /
- geochronology /
- geochemistry /
- Hf isotope /
- Bengbu uplift

HTML全文

图 1 蚌埠隆起区地质略图

Fig. 1. Geological sketch map showing the Bengbu uplift

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图 2 蚌埠隆起区钾长花岗岩的显微照片

Kf.钾长石; Ms.白云母; Pl.斜长石; Q.石英

Fig. 2. Microphotographs for the K-feldspar granites in the Bengbu uplift

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图 3 蚌埠隆起区钾长花岗岩中锆石CL图像

63 μm圆圈为Hf同位素分析点; 30 μm圆圈为U-Pb年龄分析点; 括号内数字为ε_Hf (t) 值; 其他为U-Pb年龄及分析点号

Fig. 3. CL images of selected zircons for the K-feldspar granites in the Bengbu uplift

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图 4 蚌埠隆起区钾长花岗岩中锆石LA-ICP-MS U-Pb年龄谐和图

Fig. 4. U-Pb Concordia diagrams summarizing the LA-ICP-MS zircon data for the K-feldspar granites in the Bengbu uplift

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图 5 蚌埠隆起区钾长花岗岩的SiO₂-K₂O图(a)和含铝指数图(b)

TH.KD.LJ.为辽吉花岗岩; TH.据路孝平等, 2004a; KD.据孙敏等, 1996; LJ.据郝德峰等, 2004

Fig. 5. SiO₂ vs. K₂O and aluminous index diagrams for the K- feldspar granites in the Bengbu uplift

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图 6 蚌埠隆起区钾长花岗岩的球粒陨石标准化稀土元素(a)和原始地幔标准化微量元素(b)变异图

球粒陨石标准化值据Boynton(1984); 原始地幔标准化值据Sun and Mc Donough(1989); TH.KD.IJ数据来源见图 5

Fig. 6. Chondrite normalized REE patterns (a) and primitive mantle normalized trace element spider diagrams (b) for the K-feldspar granites in the Bengbu uplift

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图 7 蚌埠隆起区钾长花岗岩的t-ε_Nd (t)变异图

亏损地幔演化线据Goldstein et al. (1984); KD和LJ数据来源见图 5

Fig. 7. t vs. ε_Nd (t) diagram for the K-feldspar granites in the Bengbu uplift

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图 8 蚌埠隆起区钾长花岗岩的Hf同位素组成

Fig. 8. Zircon Hf isotopic compositions for the K-feldspar granites in the Bengbu uplift

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图 9 蚌埠隆起区钾长花岗岩的Hf同位素特征

Fig. 9. Zircon Hf isotopic features for the K-feldspar granites in the Bengbu uplift

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图 10 蚌埠隆起区钾长花岗岩的成因类型判别(据Whalen et al., 1987)

FG.分异的I、S型花岗岩类分布区; OGT.未分异的I、S、M型花岗岩类分布区; A.A型花岗岩类分布区; TH、KD、LJ数据来源见图 5

Fig. 10. Genetic type discrimination for the K-feldspar granites in the Bengbu uplift

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图 11 微量元素Y+Nb-Rb和Y-Nb构造环境判别图解(据Pearce et al., 1984)

ORG.大洋中脊花岗岩; WPG.板内花岗岩; VAG.火山弧花岗岩; Syn-COLG.同碰撞花岗岩; TH、KD、LJ数据来源见图 5

Fig. 11. Y+Nb-Rb and Y-Nb discrimination diagram of tectonic setting

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表 1 蚌埠隋起区钾长花岗岩中锆石LA-ICP-MS U-Pb定年数据

Table 1. LA-ICP-MS zircon U-Pb dating results for the K-feldspar granites in the Bengbu uplift

表 2 蚌埠隆起区钾长花岗岩的主量元素(%)和微量元素(10^-6)及Nd同位素组成

Table 2. Major(%), trace elements(10^-6)and Nd isotopic compositions for the K-feldspar granites in the Bengbu uplift

表 3 蚌埠隆起区钾长花岗岩中锆石Hf同位素分析结果

Table 3. Zircon Hf isotopic data for the K-feldspar granites in the Bengbu uplift

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