赣东南富城杂岩体的地球化学和年代学研究
Geochemistry and geochronology of the Fucheng Complex in the southeastern Jiangxi province, China
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摘要: 富城杂岩体出露于赣东南,与闽西南的红山岩体共同构成富城-红山花岗质杂岩.富城杂岩主要由富城黑云母巨斑粗粒二长花岗岩、粗石坝中粒二云母花岗岩和珠长洞含红柱石细粒花岗岩三个单元组成.富城花岗岩含较低的SiO2、Rb、Nb和较高的Al2O3、Ba、Sr、Zr、REE含量,岩石的ACNK>1.10,K2O/Na2O>1.60.粗石坝花岗岩以高SiO2、K2O,低CaO、P2O5和富Al(ACNK=1.13~1.20)为特征;岩石含较高的Rb、Nb和低的Ba、Sr、Zr、REE含量,并具有相对低的K/Rb和δ(Eu)比值.珠长洞含红柱石花岗岩的地球化学特征相似于富城花岗岩,除了更高的ACNK值(1.22~1.36)和Rb、Nb含量以及稍低的Sr、Ba、Zr、REE含量.富城单元的^87 Sr/^86 Sr初始比值是0.7135~0.7196,εNd(t)是-9.4~-10.2,Nd模式年龄是1.78Ga到1.84Ga,其中的锆石Hf模式年龄是1.70~1.89Ga,与Nd同位素一致;粗石坝单元具有与之相似的Nd-Hf同位素组成;珠长洞单元的^87 Sr/^86 Sr初始比值更高(0.7214),εNd(t)更低(-16.9),而Nd模式年龄达2.37Ga.这些地球化学特征表明富城杂岩体的源岩都是由古老物质组成的沉积岩,其中富城和粗石坝单元起源于具晚古元古代模式年龄的基底,而珠长洞单元的源区物质具有早古元古代平均地壳存留年龄.富城杂岩体的各单元之间没有显示一致的变化规律,表明它们不是单一岩浆演化的结果,它们成分的差异主要受源区成分影响.LA-ICPMS的锆石U-Pb定年显示富城黑云母花岗岩形成较早(239±17Ma),而粗石坝和珠长洞花岗岩形成稍晚(231±16 Ma和229±6.8 Ma).它们的形成时代与华南印支期早期构造-岩浆活动的峰期一致.结合地球化学和岩石组合特征,可以认为富城-红山杂岩形成于同构造背景.
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关键词:
- 地球化学 /
- 锆石U-Pb-Hf同位素 /
- 印支期岩浆活动 /
- 岩石成因 /
- 富城花岗质杂岩
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Key words:
- Geochemistry /
- Zircon U-Pb-Hf isotopes /
- Indosinian magmatism /
- Petrogenesis /
- Fucheng granitic complex
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