Petrogenesis of the Caledonian granites in the northern part of Miaoershan pluton, southwestern Hunan Province: Evidence from petrology, geochemistry and zircon U-Pb age
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摘要:
苗儿山岩体位于湘西南与桂北交界处，为由晋宁期、加里东期、印支期和燕山期花岗岩组成的复式岩体。其中，加里东期花岗岩构成该复式岩体的主体，可划分为六个侵入次。本次通过锆石LA-ICP-MS测年，获得第一、第二、第六侵入次的年龄分别为（428.1±3.6）Ma、（420.3±3.4）~（421.3±3.2）Ma和（408.3±3.5）Ma。加里东期花岗岩的（87Sr/86Sr）i为0.71765，εNd（t）为-9.7，δ18O值为9.8‰，总体属壳源弱过铝-强过铝质花岗岩，形成于碰撞挤压峰期之后挤压减弱、应力松弛的后碰撞构造环境，其早期和晚期的源区岩石类型和形成温度有所区别：早期花岗岩的上地壳源区成分较为复杂，不仅存在泥岩，还有砂屑岩和/或变质火成岩，其形成温度较高（>875℃）；晚期花岗岩的源岩为上地壳泥岩，属典型的S型花岗岩，其形成温度较低（< 875℃）。
Abstract:The Miaoershan pluton, located at the junction of southwestern Hunan and Northern Guangxi, is a composite batholith composed of Jinningian, Caledonian, Indosinian and Yanshanian granites. Among them, Caledonian granites constitute the main body of the composite batholith, which can be divided into six intruding episodes. Through zircon LA-ICP-MS dating, the ages of the first, second and sixth episodic granites were measured at (428.1±3.6) Ma, (420.3±3.4)-(421.3±3.2) Ma and (408.3±3.5) Ma, respectively. The average (87Sr/86Sr)i, εNd(t) and the δ18O values of the Caledonian granites are 0.71765, -9.7, and 9.8, respectively. Caledonian granites are generally crust derived weak peraluminous-strong peraluminous granites, formed in post-collisional tectonic environment characterized by weakened compression and relaxed stress after the peak period of collision and extrusion. Their material and heat sources are different in the early and late stages. The early stage granites were derived from upper crustal metamorphic mudstone, psammite and/or metamorphic igneous rocks, and their formation temperature is relatively high(> 875℃). The late stage granites were derived from upper crustal metamorphic mudstone with lower formation temperature (< 875℃), showing the characteristics of typical S-type granites.
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图 10 加里东期花岗岩Rb/Sr-Rb/Ba图解（图例同图5；据Sylvester，1998)
Figure 10.
图 12 加里东期花岗岩微量元素构造环境判别图解(图例同图 5，据Pearce et al., 1984)
Figure 12.
表 1 加里东期花岗岩主量元素组成(%)及部分特征参数
Table 1. Major element composition (%) and some characteristic parameters of the Caledonian granites
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表 2 加里东期花岗岩微量元素丰度(Ag为10-9；其余为10-6)
Table 2. Trace element abundance of the Caledonian granites (Ag: 10-9, the other elements: 10-6)
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表 3 加里东期花岗岩稀土元素丰度(10-6)及有关参数
Table 3. REE abundance (10-6) and its related parameters of the Caledonian granites
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表 4 加里东期花岗岩样品D0026锆石U-Pb定年结果
Table 4. Zircon U-Pb dating results for the sample D0026 of Caledonian granite
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表 5 加里东期花岗岩样品D0029锆石U-Pb定年结果
Table 5. Zircon U-Pb dating results for the sample D0029 of Caledonian granite
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表 6 加里东期花岗岩样品D0035锆石U-Pb定年结果
Table 6. Zircon U-Pb dating results for the sample D0035 of Caledonian granite
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表 7 加里东期花岗岩样品D0070锆石U-Pb定年结果
Table 7. Zircon U-Pb dating results for the sample D0070 of Caledonian granite
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