Zircon LA-ICP-MS U-Pb dating of granites in Qiashui area, Guangdong Province: Constraints on the ~100 Ma tectonic setting of interior of South China
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摘要:
研究目的 东南沿海地区发育大量~100Ma的岩浆岩，在华南内陆该期岩浆作用虽报道较少但往往与成矿有关。查明该期岩浆作用在华南内陆的分布，将为该区晚燕山期构造背景的研究及相关找矿勘查提供科学依据。
研究方法 基于1︰5万区域地质调查和详细的岩相学研究，对位于华南内陆的郴州—临武断裂附近的洽水地区花岗岩，划分为5个侵入次：（1）粗—中粒斑状含角闪石黑云母二长花岗岩；（2）中—细粒斑状含角闪石黑云母二长花岗岩；（3）中—细粒斑状黑云母二长花岗岩；（4）中—细粒含斑黑云母二长花岗岩；（5）细粒含斑黑云母正长花岗岩。然后系统地对不同侵入次的代表性岩石进行锆石LA-ICP-MS U-Pb定年。
研究结果 获得第一到第五侵入次的年龄为102~97Ma，均属早—晚白垩世之交（~100Ma）侵入岩。
结论 综合分析对比华南内陆及东南沿海地区~100Ma的岩浆事件，认为华南内陆该期岩浆活动的动力学机制是：古太平洋板块俯冲后撤引发的弧后及陆内岩石圈伸展，导致郴州—临武等古深大断裂重新活化拉张，引起软流圈上涌和岩石圈减薄，进而产生较强烈的幔源和壳源岩浆活动。
Abstract:This paper is the result of geological survey engineering.
Objective A large amount of ~ 100 Ma magmatic rocks are developed in the southeast margin of South China. Shifting to interior of South China, although the period of magmatism has been reported sparingly, they were often related to metal mineralization. Determination of the distribution of magmatism of ~ 100 Ma in the interior of South China would provide a scientific basis for the study of the late Yanshanian tectonic setting, and related ore prospecting and exploration.
Methods Based on the 1︰50000 regional geological survey and detailed petrographic study, the granites in Qiashui area, which are located near the Chenzhou-Linwu fault in the interior of South China, were divided into five intrusive episodes, including (1) porphyritic coarse-medium-grained amphibole-biotite monzogranite, (2) porphyritic medium-fine-grained amphibole-bearing biotite monzogranite, (3) porphyritic medium-fine-grained biotite monzogranite, (4) medium-fine-grained biotite monzogranite with rare porphyrites and (5) fine-grained biotite syenogranite with rare porphyrites, respectively. Zircon LA-ICP-MS U-Pb dating was carried out systematically for the representative rocks of these intrusions.
Results U-Pb dating yield ages of the first to fifth intrusive episodes ranges from 102 Ma to 97 Ma, which is at the transition of the Early and Late Cretaceous.
Conclusions According to comprehensive analysis and comparison of the ~100 Ma magmatic events in the interior and southeast coastal regions of South China, it shows that the geodynamic mechanism of the magmatism of ~100 Ma in the interior of South China might be related to back arc and intracontinental lithospheric extension resulting from Paleo-Pacific plate subduction retreation. It led to reactivation and extension of ancient deep faults such as the Chenzhou Linwu fault, and then the intensive mantle and crust magmatism.
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图 1 华南主要构造单元和中生代岩浆岩分布图(a, 据Zhou and Li, 2000; Wang et al., 2013修改)、连阳岩体地质简图(b, 据高剑峰等, 2005修改；同位素年龄数据马星华等, 2014)及研究区地质简图与采样位置图(c, 据袁永盛等, 2020修改)
Figure 1.
图 4 洽水地区花岗岩的黑云母成分分类图（a, 底图据Foster, 1960）和角闪石成分分类图（b, 底图据Leake et al., 1997）
Figure 4.
图 9 华南燕山期火成岩同位素年龄统计图（据Li et al., 2010; 贾丽辉, 2018修改）
Figure 9.
图 10 华南110~90 Ma花岗岩类和玄武质岩石分布图（底图据Zhou and Li, 2000; Wang et al., 2013修改）
Figure 10.
表 1 洽水地区第一至第五次花岗岩锆石 LA-ICP-MS U-Pb 测年结果
Table 1. Zircon LA-ICP-MS U-Pb data of the first to fifth episodes granites in Qiashui region
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表 2 华南 110~90 Ma 花岗岩类年代学资料
Table 2. Geochronological data of the 110-90 Ma granitoids in South China
下载: 导出CSV
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