U-Pb age and genesis of the Hejiazhuang-Laohuyao intrusion in West Qinling and limitation of plate subduction time
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摘要:
何家庄—老虎窑岩体位于勉略缝合带以北,靠近秦岭微板块北部的商丹断裂带西段内部,两者的主体岩性为花岗闪长岩。本文对何家庄—老虎窑岩体进行了LA-ICP-MS锆石U-Pb同位素定年和地球化学特征以及Hf同位素特征研究。结果表明,西部何家庄附近花岗闪长岩侵位时间为235~240 Ma,东部老虎窑附近花岗岩侵位时间为239 Ma,两者均侵位于早三叠世。何家庄—老虎窑岩体花岗闪长岩均为高钾钙碱性系列,表现出强过铝质特征,属于I型花岗岩。两者岩浆锆石的εHf(t)值都是以负值为主,包含一到两个正值,地壳模式年龄为中元古代(1255~1754 Ma),指示它们的源岩有地幔物质的加入,可能是以中元古代古老地壳的部分熔融为主的壳源物质与地幔物质混合的岩浆。且表现出与埃达克质岩相似的地球化学特征,反映其岩浆可能起源于俯冲洋壳在高压环境下部分熔融产生的溶体与由于底侵作用被橄榄岩混染的下地壳部分熔融产生的高钾溶体的岩浆混合。两者的侵位年龄和成因证明了扬子板块与秦岭微板块在235~240 Ma的这个期间处于俯冲阶段。
Abstract:The Hejiazhuang-Laohuyao intrusions are located in the north of the Mianlue suture zone, close to the west section of the Shangdan fault zone in the north of the Qinling microplate, and their main lithology is granodiorite. The authors studied the LA-ICP-MS zircon U-Pb ages, geochemical characteristics and Hf isotope characteristics of the Hejiazhuang-Laohuyao intrusions. The results show that the emplacement time of the Hejiazhuang intrusion is 235-240 Ma and that of the Laohuyao intrusions is 239 Ma, suggesting that their emplacement epochs were the early Triassic. The granodiorite in the Hejiazhuang and Laohuyao intrusions are both high-potassium calcareous and alkaline series, showing strong over-aluminum characteristics and belonging to type I granite. The εHf (t) values of both magmatic zircons are mostly negative and contain one or two positive values. The model age of the crust is Mesoproterozoic (1255-1754 Ma), indicating that their source rocks experienced the addition of mantle materials, which might have been magma mixed with mantle materials dominated by partial melting of Mesoproterozoic ancient crust, showing similar geochemical characteristics to adakianrocks and indicating that the magma might have originated from high potassium solution magma mixing produced by partial melting of subducted oceanic crust under high pressure and partial melting of lower crust contaminated by peridotite due to bottom transgression. The emplacement time and genesis of them indicate that the Yangtze plate and Qinling microplates were subducted during the period of 235-240 Ma.
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图 1 秦岭造山带三叠纪花岗岩分布(a)(据杨朋涛等,2013)与采样位置简图(b)(据1:50000地质图)
Figure 1.
图 6 何家庄—老虎窑岩体中花岗闪长岩原始地幔标准化微量元素蛛网图(a)和球粒陨石标准化稀土配分模式图(b)(标准化值据Sun and McDonough, 1989)
Figure 6.
图 7 何家庄—老虎窑岩体中花岗闪长岩的εHf(t)-t(a)和(176Hf/177Hf)-t(b)图解(据袁永盛等,2018)
Figure 7.
图 12 Th/Yb-Ta/Yb图解(据李佐臣等,2013)
Figure 12.
表 1 花岗闪长岩LA-ICP-MS锆石U-Pb同位素分析结果
Table 1. LA-ICP-MS zircon U-Pb data of the granodiorite
表 2 何家庄—老虎窑岩体中花岗闪长岩主量(%)和微量(10-6)分析结果
Table 2. Analytical results of major(%) and trace element(10-6) of the granodiorite in the Hejiazhuang-Laohuyao intrusions
表 3 花岗闪长岩锆石Hf同位素组成
Table 3. Zircon Hf isotopic compositions of the granodiorite
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