| Institute of Geomechanics, Chinese Academy of Geological Sciences | Host |
| Citation: |
YANG Yuqing, GAO Peng, ZHANG Jian, LIU Xiaoguang, CHENG Changquan, YIN Changqing, QIAN Jiahui. 2024. Geochemical characteristics of apatite in metabasic rocks under different metamorphic conditions: a case study from the Paleoproterozoic Trans-North China Orogen. Journal of Geomechanics, 30(6): 991-1011. doi: 10.12090/j.issn.1006-6616.2024046
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Geochemical characteristics of apatite in metabasic rocks under different metamorphic conditions: a case study from the Paleoproterozoic Trans-North China Orogen
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Abstract
Objective Apatite is a common accessory mineral that is widely distributed in various rock types. Its U-Pb age, trace elements (particularly REE, Th, U, and Sr), and Sr-Nd isotopic compositions provide important information on its chronology and magmatism. However, the geochemical behavior at different metamorphic levels during orogenesis remains unclear. As a typical continent-to-continent collisional orogenic belt in the Paleoproterozoic, the Trans-North China Orogen (TNCO) has recorded an integrated metamorphic sequence ranging from greenschist to amphibolite to granulite facies. Therefore, it is an ideal area to study the geochemical behavior of apatite during various grades of metamorphism involving the orogenic process.
Methods In this study, we systematically collected metabasic samples of different metamorphic grades, including greenschist, amphibolite, and mafic granulite, in the Wutai-Hengshan area of the TNCO. We conducted detailed petrographic observations and geochemical analyses of apatite grains from metabasic rocks with different metamorphic grades.
Results Our results showed that the apatite grains from the greenschist samples had both magmatic and metamorphic origins. The apatite grains in the amphibolite samples were mainly of metamorphic origin. In contrast, the grains from the granulite samples were closely related to crustal anatexis, exhibiting geochemical characteristics of magmatic-origin apatite.
Conclusion This study shows that trace element variations in apatite can clearly reflect the influence of metamorphic grades, crustal anatexis, and coexisting rock-forming minerals with variations in temperature and pressure conditions during metamorphism.
Significance The results of this study provide new constraints to our understanding of elemental migration and the geochemical balance within apatite during orogeny.
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Keywords:
- North China Craton /
- Trans-North China Orogen /
- metabasic rocks /
- metamorphism /
- apatite /
- trace elements
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References
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YANG Yuqing, GAO Peng, ZHANG Jian, LIU Xiaoguang, CHENG Changquan, YIN Changqing, QIAN Jiahui. 2024. Geochemical characteristics of apatite in metabasic rocks under different metamorphic conditions: a case study from the Paleoproterozoic Trans-North China Orogen. Journal of Geomechanics, 30(6): 991-1011. doi: 10.12090/j.issn.1006-6616.2024046
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Figure 1.
Tectonic subdivision of the North China Craton (modified after Zhao et al., 2001, 2005)
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Figure 2.
Lithologic map of the Wutai-Hengshan Complex and the sampling locations in this study (modified after Zhao et al., 2007; Zhang et al., 2012)
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Figure 3.
Field photograph of metabasic rocks of different metamorphic grades in the Wutai-Hengshan Complex and the representative photos
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Figure 4.
Microscopic characteristics of the samples
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Figure 5.
Cathodoluminescence (CL) images of the representative samples
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Figure 6.
Diagram of whole rock major element of the metabasic rocks in the Wutai-Hengshan area
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Figure 7.
Diagram of whole rock trace element (standardized values according to Sun and McDonough, 1989)
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Figure 8.
Major element diagram of apatite grains of different metamorphic grades
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Figure 9.
Trace element diagram of apatite grains of different metamorphic grades
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Figure 10.
Trace element diagram of apatite of different genetic types (modified after O'Sullivan et al., 2020)
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Figure 11.
Chondrite-normalized REE patterns for solid-state recrystallization of metamorphosed zircons from the Dabie-Sulu Orogenic Belt (modified after Chen and Zheng, 2017;Reference data: Chen et al., 2010; Xia et al., 2010)