Geological and geochemical characteristics of the Paleoproterozoic intrusions in Bengbu uplift, southeast North China Craton
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摘要:
华北陆块是世界上最古老、最大的克拉通地块之一。蚌埠隆起作为华北陆块的组成部分，其初始陆壳的形成时限为中太古代晚期，随着扬子陆块与华北陆块碰撞、拼接，经历了较为复杂的演化过程。为了深入探讨蚌埠隆起带古元古代岩浆活动，更新补充年代学及岩石地球化学分析数据，本次通过对区内古元古代侵入体的野外观察、年代学和岩石地球化学研究，在庄子里岩体和磨盘山岩体中分别获得锆石U-Pb年龄为（2089±44）Ma、（2133±27）Ma。地球化学研究显示两岩体明显富钠贫钾，总体铝碱比偏高，钙碱比偏低，属准铝—铝过饱和类型；轻稀土相对富集，具明显的铕负异常，铈异常不明显或无异常；K、Nb、Sr、P和Ti有较明显的亏损，Rb、Th、U、Nd、Zr和Sm相对富集，成因类型具备造山后A型花岗岩特征。εNd（t）值介于-3.87~+3.20，暗示侵入体可能来源于同一源区，Nd两阶段模式年龄（2.37~2.84 Ga）与华北克拉通主体形成于太古宙，并以2.40~2.50 Ga为主体相一致。εHf（t）值介于-9.77~+9.59，且差别较大，说明其具物质起源的复杂性，古老的两阶段Hf模式年龄（2.27~2.96 Ga）说明其物质起源主要为新太古宙，与蚌埠隆起拉张背景时间上具有一致性。构造环境判别属板内花岗岩范畴，表现为非造山构造环境，暗示其伸展构造背景。
Abstract:North China landmass is the oldest landmass and one of the largest craton massifs in the world. Bengbu uplift is a part of the North China landmass, and its initial formation of continental crust is late Archean in the time limit. With the collisions and stitching of the Yangtze platform and North China continental block, the Bengbu uplift experienced complex evolution processes. In order to further explore the Paleoproterozoic magmatic activity in the Bengbu uplift, the authors updated the data of geochronologic and geochemical analysis. Based on field observation, geochronology and geochemistry of Paleoproterozoic intrusions in this area, the authors obtained zircon U-Pb ages of (2089±44)Ma and (2133±27)Ma for Zhuangzili and Muopanshan granites. The geochemical data show that granites have high-Na and low-K significantly, and belong to the quasi-aluminum supersaturated type. They are characterized by relative enrichment of LREE with a strong Eu negative anomaly and insignificant Ce anomaly. The elements of K, Nb, Sr, P and Ti are characterized by measurable depletion, and there exists relative enrichment of Rb, Th, U, Nd, Zr and Sm. Intrusion projection points are distributed in A type granite area in the discrimination diagram of genetic type. Nd twophase age (2.37-2.84 Ga) is consistent with the age of North China Craton formed in Archean, with 2.40-2.50 Ga being the main stage. εHf(t) values vary between -9.77 and +9.59, with obvious differences, suggesting the complexity of the origin of the material, and the old two-phase Hf model age (2.27-2.96 Ga) suggests that the main material was derived during Neoarchean. The tectonic environment belongs to the granite category within the plate and non-orogenic tectonic environment, which implies its extensional tectonic setting.
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图 1 蚌埠隆起地质简图(据安徽省东部1: 20万地质图; 宋利宏等, 2016修编)
Figure 1.
图 4 蚌埠隆起带古元古代侵入体全碱−硅(TAS)分类(据Middlemost, 1994)
Figure 4.
图 5 蚌埠隆起带古元古代侵入体SiO2−K2O图解(a)(实线据Peccerillo and Taylor, 1976; 虚线据Middlemost, 1985)及A/CNK-A/NK图解(b)(底图据Middlemost, 1994)
Figure 5.
图 6 蚌埠隆起带古元古代侵入体球粒陨石标准化稀土元素配分图(a)及原始地幔标准化微量元素蛛网图(b)(标准化数值据Sun and McDonough, 1989)
Figure 6.
图 8 蚌埠隆起带古元古代侵入体成因类型判别图(a)及A型花岗岩分类图(b) (a据Whalen et al., 1987; b据Eby, 1990, 1992)
Figure 8.
图 10 蚌埠隆起带古元古代侵入体(Y+Nb)-Rb及(Yb+Ta)-Rb构造环境判别图解(据Pearce et al., 1984)
Figure 10.
表 1 蚌埠隆起带古元古代侵入体主量元素组成(%)
Table 1. Major compositions of Paleoproterozoic intrusions in Bengbu uplift (%)
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表 2 蚌埠隆起古元古代侵入体微量、稀土元素组成(10-6)
Table 2. Trace element composition of Paleoproterozoic intrusions in Bengbu uplift(10-6)
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表 3 蚌埠隆起带古元古代侵入体锆石U−Pb年龄数据
Table 3. Zircon U−Pb age data of Paleoproterozoic intrusions in Bengbu uplift
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表 4 蚌埠隆起带古元古代侵入体Sm-Nd同位素组成
Table 4. Sm-Nd isotopic compositions of Paleoproterozoic intrusions in Bengbu uplift
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表 5 蚌埠隆起带古元古代侵入体Lu-Hf同位素分析结果
Table 5. Zircon Lu-Hf isotopic compositions of Paleoproterozoic intrusions in Bengbu uplift
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http://cdmd.cnki.com.cn/Article/CDMD-10183-2009091440.htm 赵越, 翟明国, 陈虹, 张拴宏. 2017.华北克拉通及相邻造山带古生代-侏罗纪早期大地构造演化[J].中国地质, 44(1):44-60. doi: 10.3969/j.issn.1672-6995.2017.01.011 http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20170104&flag=1
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