Petrogenesis and geotectonic significance of magnesian andesite in the Nangunyuan area, northern Hainan Island, China

Abstract

The Magnesian andesite discovered in the Nangunyuan area of northern Hainan Island provides an important research object for constraining the tectonic evolution process of the Paleo-Tethys Ocean in Southeast Asia. The formation age of the Magnesian andesite in the Nangunyuan area of northern Hainan Island was determined to be 251.2 ± 4.5 Ma in the late Permian by LA-ICP-MS zircon U-Pb dating. The Magnesian andesite is characterized by relatively high contents of SiO₂, CaO, and MgO, and relatively low contents of Na₂O, K₂O, and FeO. It is enriched in large ion lithophile elements and relatively depleted in high field strength elements, with obvious negative anomalies of Ta, Nb, and Ti. It has geochemical characteristics similar to those of Sanukite and belongs to island arc volcanic rocks. The Magnesian andesite may be formed by the equilibrium reaction between the mantle peridotite and the Si-rich melt from the partial melting of the subducting oceanic crust slab or sediment. It is the product of the wedge mantle source region of the Changjiang-Qionghai tectonic belt affected by the metasomatism of the subduction component. Its formation age is close to the closure time of the Paleo-Tethys Ocean, which may mark the late stage of the subduction of the Paleo-Tethys Ocean. The discovery of the late Permian Magnesian andesite in northern Hainan Island reveals the late-stage dynamics of the subduction of the Paleo-Tethys Ocean. Its magma source mixing origin reflects the complex interactions between the crust and mantle in the subduction zone. This discovery is of great scientific value for constraining the closure time of the Paleo-Tethys Ocean, understanding the formation mechanism of the Paleo-Tethys orogenic belt, and regional metallogeny.

Introduction

Situated at the convergent junction of the Eurasian, Pacific, Indochina, and Philippine Sea plates, Hainan Island’s geological evolution has been jointly controlled by both Paleo-Pacific and Tethyan tectonic regimes. As a “geological bridgehead” extending from mainland China to the South China Sea, this region preserves critical evidence documenting multi-stage tectonic events including the closure of the Paleo-Asian Ocean, evolution of the Tethyan Ocean, and Pacific subduction, making it a key window for deciphering East Asian continental accretion and supercontinent cyclicity (Li et al., 2000a; Liu et al., 2021). Although previous studies established a fundamental “EW-zonation and NS-blocking” tectonic framework (Xu et al., 2001; Ding et al., 2005), significant controversies persist regarding core scientific issues such as its tectonic affinity, precise unit boundaries, spatial distribution of sutures, and final amalgamation timing (Li et al., 2002; Shen et al., 2018). Outstanding debates include whether Hainan constitutes Gondwana-derived fragments and preserves remnants of Paleo-Tethyan subduction zones, while Late Mesozoic paleomagnetic and biogeographic evidence further reveals complex rotational drift trajectories (Liu et al., 2022a; b; Wang et al., 2022; Lv et al., 2023; Wei et al., 2023; Sheir et al., 2024; Ashraf et al., 2024).

Magnesian andesites represent a distinctive magma type with diagnostic geochemical signatures and specific petrogenetic settings, serving as critical probes for deep crust-mantle interactions and plate dynamics (Dong and Santosh, 2016; Gao et al., 2022). High-Mg andesites (HMA) are typically defined by SiO₂ >52 wt%, elevated MgO (>5 wt%) with Mg^# >55, enriched Ni-Cr, and low FeO^T/MgO (<1), whereas evolved magnesian andesites (MA) may exhibit lower MgO (two to three wt%) while maintaining high Mg^# with reduced Ni-Cr contents. Deng et al. (2010) classified these rocks into HMA and MA based on SiO₂-MgO-FeO^T/MgO systematics: HMAs originate from hydrous melting of mantle wedges above subduction zones, while MAs form through interaction between slab-derived melts/fluids and overlying mantle under high thermal gradients in subduction-related environments.

Late Paleozoic volcanic rocks remain poorly exposed in Hainan, with Permian volcanism particularly understudied. Existing research has primarily focused on limited Late Paleozoic volcanic units in southern and central-western Hainan (He et al., 2016; Gou et al., 2019), leaving critical gaps in understanding the island’s Permian tectonic evolution. Our recent discovery of Permian intermediate lavas in the Nangunyuan area (northern Hainan) provides new constraints through integrated LA-ICP-MS zircon U-Pb geochronology and petrochemical analyses. By characterizing these magnesian andesites’ geochemical fingerprints and comparing their age spectra with regional tectono-magmatic events, this study aims to: elucidate their petrogenesis, decipher tectonic implications and establish robust geological evidence for reconstructing Hainan’s Permian evolution. These findings hold significant implications for determining the closure timing of the eastern Paleo-Tethys Ocean, understanding Paleo-Tethyan orogenic mechanisms, and regional metallogeny.

Geological settings

Hainan Island is geographically separated from the South China Block by the Qiongzhou Strait and adjoins the Indochina Block through the Beibu Gulf, occupying a critical junction between the Paleo-Tethyan and Paleo-Pacific tectonic domains (Figure 1a). The island has undergone multiple tectonic episodes including the Jinningian, Caledonian, Hercynian, Indosinian, Yanshanian, and Himalayan orogenies, resulting in dominant EW- and NE-trending structural systems with subordinate NS-oriented structures (Figure 1b) (Chao et al., 2016; Liang et al., 2018). The EW-trending tectonic framework comprises four major belts from north to south: the Wangwu-Wenchang, Changjiang-Qionghai, Jianfeng-Diaoluo, and Jiusuo-Lingshu tectonic zones (Liang et al., 2018). NE-trending structures are principally represented by the Gezhen and Baisha faults.

FIGURE 1

Liu et al., 2016; Liang et al., 2023, with modifications)、Geological Map of Hainan Island (b) and Study Area (c).

The stratigraphic record spans from Proterozoic to Cenozoic, excluding Devonian and Jurassic systems, with the Mesoproterozoic Baoban Group constituting the crystalline basement (Long et al., 2023). Intense magmatic activity is manifested through widespread Hercynian-Indosinian granitoids, predominantly biotite monzogranites and granodiorites, followed by Late Yanshanian intrusives (Wang et al., 2019). Volcanic sequences exhibit multi-phase eruptive histories, dominated by Cenozoic volcanics in northern Hainan, with subordinate Cretaceous continental intermediate-acid volcanic rocks in Mesozoic basins, while Proterozoic and Paleozoic volcanic units occur sporadically (Liang et al., 2021; Lin et al., 2022).

The Nangunyuan magnesian andesites in northern Hainan are located south of the Wangwu-Wenjiao Fault and north of the Changjiang-Qionghai Fault, specifically within the Nanchu Village area of Renxing Town, Chengmai County (Figure 1c). This region exposes several-kilometer-thick Paleozoic sedimentary sequences comprising flyschoid formations intercalated with volcanic and siliceous rocks, the latter containing radiolarian fossils indicative of pelagic environments (Long et al., 2007). Our field investigations identified newly discovered magnesian andesites occurring as interlayered and lenticular bodies within Late Paleozoic mudstones, argillaceous siltstones, silty mudstones, quartz sandstones, and siltstones (Figure 2a). These volcanic units strike NE-SW, concordant with regional bedding attitudes. The adjacent area hosts numerous Late Permian to Early-Middle Triassic monzogranite intrusions.

FIGURE 2

The magnesian andesites have undergone greenschist-facies metamorphism, with primary mineral assemblages largely replaced by secondary phases dominated by quartz (Figures 2b,c), actinolite (Figures 2b,c), zoisite, and epidote (Figure 2d). Rare relict clinopyroxene, diopside, and plagioclase crystals are locally preserved. Resultant metamorphic lithologies include quartz-actinolite schist, zoisite-actinolite rock, actinolite-diopside rock, quartz-epidote rock, quartz-plagioclase-epidote rock, and quartz-diopside rock, reflecting complex metasomatic overprinting during tectonic evolution.

Methods

The zircon separation was completed in the laboratory of the Hebei Regional Geological and Mineral Survey Research Institute. Conventional gravity and magnetic separation methods were used to separate zircon monominerals, and then zircons were handpicked under a binocular microscope. The zircons were placed on epoxy resin and then ground and polished to expose the surface of the zircons. Cathodoluminescence (CL) microscopy was performed on the zircons to be dated. Zircon CL photography and LA-ICP-MS analysis were completed in the State Key Laboratory of Geological Processes and Mineral Resources at China University of Geosciences (Wuhan). CL photography was taken on a JEOL-JXA-8100 electron microprobe instrument. Zircon U-Pb isotope and trace element content analyses were carried out using the GeoLas 2005 excimer laser ablation system from MicroLas Company on an Agilent7500a type ICP-MS instrument from Agilent Company in the United States. Zircon ages were calibrated externally using standard zircon 91,500, and GJ-1 was used as the internal standard sample. Element contents were calibrated externally using SRM610, with ²⁹Si as the internal standard element. ICP-MS-DataCal 8.3 was used for offline processing of the measured isotope data. The U-Pb age concordia diagram and weighted average age calculations and plots were completed using Isoplot 3.0. The error for individual data points is 1σ, and the confidence level for the weighted average age of the sample is 2σ, with a confidence level of 95%.

The analysis of whole-rock major elements, trace elements, and rare earth elements was completed in the Hubei Geological Experiment Research Institute. For major element analysis, except for H₂O, which was determined by gravimetric method, and CO₂, which was analyzed by non-aqueous titration, the remaining oxides were determined by X-ray fluorescence spectroscopy with the a-coefficient method. The analytical precision (relative error) is 1% for all elements except H₂O. Trace elements and rare earth elements were analyzed using inductively coupled plasma atomic emission spectrometry (ICP-AES). The long-term (4 h) stability of this instrument is better than 1%, and the analytical precision is better than 1%. Spectral interferences were treated using a peak shaping function, i.e., Fitted background correction, to process the analyzed peak shapes.

Results

Zircon U-Pb age

The zircons in sample D0245-2 are mostly light rose or light brown in color, with a few being colorless and transparent. They are idiomorphic to subidiomorphic long columnar crystals, with lengths mostly ranging from 100 μm to 400 μm. The length-to-width ratios of the columnar crystals range from 2:1 to 4:1. CL images show distinct oscillatory zoning or platy zoning, which are typical characteristics of magmatic crystallization zircons (Figure 3). During LA-ICP-MS analysis, positions without inclusions and fractures were selected for measurement. Most of the selected positions are located at the edges of the zircons. The U and Pb test data of 20 points of zircons are shown in Table 1. The Th and U contents of the zircons range from 57 ppm to 1,695 ppm and 75 ppm–1970 ppm, respectively, with Th/U values between 0.25 and 1.04. The ²⁰⁶Pb/²³⁸U ages of the 20 measured points range from (244.5 ± 2.2) Ma to (2,375.8 ± 19.9) Ma. All the tested points are located on or near the concordia line. Among them, three points have 206 Pb/238U ages greater than 1800 Ma, and two points have ²⁰⁶Pb/²³⁸U ages of 862.6 ± 7.0 Ma and 537.8 ± 4.8 Ma, respectively. The remaining points are mainly distributed between 389–443 Ma and 244–256 Ma. Zircons at test points 7, 8, 9, 10, 11, and 17 exhibit broad platy zoning, which is a characteristic feature of zircons from typical neutral volcanic rocks. The weighted average ²⁰⁶Pb/²³⁸U age of these zircons is 251.2 ± 4.5 Ma (Figure 4). The obtained age of 251.2 ± 4.5 Ma can be interpreted as the eruption crystallization age of the volcanic rocks, while the other older ²⁰⁶Pb/²³⁸U ages may represent inherited zircon ages.

FIGURE 3

FIGURE 4

Major element

Due to the fact that the magnesian andesites in the Nangunyuan area of northern Hainan Island occur as interlayers and lens-shaped bodies within Late Paleozoic metamorphic rocks, with small outcrop areas and strong rock weathering, only five fresh rock chemical samples were collected in this study. The chemical analysis results and main parameters of the rocks are listed in Table 2. The Al₂O₃ content of the magnesian andesite in the Nangunyuan area of northern Hainan Island is relatively low. The aluminum saturation index A/CNK of most samples is less than 1, and the A/NK value is greater than 1, ranging from 1.93 to 3.22, indicating that they are metaluminous rocks. The Rittmann index σ ranges from 0.15 to 0.60, all less than 1. According to Rittmann’s classification, they belong to the extremely strong Pacific-type within the alkali-calcic rock series. Based on the SiO₂-Nb/Y diagram (Figure 5), they mainly fall into the rhyodacite/dacite series. Moreover, according to the Th-Co diagram (Figure 6), the samples all fall into the high-potassium calc-alkaline series and the olivine basalt series. The Magnesian-iron index (MF) value of the rocks is not large, ranging from 60.62 to 67.96, indicating that the degree of magmatic fractional crystallization is not high. The Mg^# value is moderate, ranging from 45.78 to 54.07, representing that the magma has undergone slight differentiation. The differentiation index (DI) is moderate, ranging from 41.15 to 59.70, close to the differentiation index (56) of the average chemical composition of Dacite, indicating that the degree of magmatic differentiation and evolution is moderate. However, the solidification index (SI) value is relatively small, ranging from 25.61 to 28.17, indicating that the basicity of the rocks is moderate.

FIGURE 5

Winchester and Floyd, 1977).

FIGURE 6

Hastie et al., 2007).

Rare earth element

The total rare earth element (REE) contents of the five rocks do not vary significantly, and they generally exhibit similar REE distribution patterns (Figure 7), all showing right-leaning curves enriched in light rare earth elements (LREEs). The ratios of light to heavy rare earth elements range from 3.90 to 7.13; the (La/Yb)_N values range from 5.92 to 8.63, and the (Ce/Yb)_N values range from 1.71 to 5.12, indicating moderate differentiation between light and heavy rare earth elements. The (La/Sm)_N values range from 2.83 to 3.74 (with an average of 3.23), suggesting a slightly stronger fractionation among light rare earth elements. The (Gd/Yb)_N values range from 1.39 to 1.78, indicating that the fractionation among heavy rare earth elements is not significant, and the degree of fractionation of light rare earth elements is slightly stronger than that of heavy rare earth elements. The Eu element shows a moderate negative anomaly, with δEu values ranging from 0.67 to 0.74. The δCe values range from 0.29 to 0.90. Except for the D0245-1 sample, which has a δCe value of 0.9, showing a weak negative anomaly of the Ce element, the other samples exhibit a strong negative anomaly of the Ce element.

FIGURE 7

Anders and Grevesse, 1989).

Trace element

The high field strength elements (HFS) Zr and Hf in the rocks have relatively high contents, while the contents of Nb and Ta are relatively low. The Nb/Ta ratios range from 8.4 to 13.46 (with an average of 11.5), all lower than those of chondrites, primitive mantle, mid-ocean ridge basalts (Nb/Ta = 17.39–17.66) (Anders and Grevesse, 1989; Sun and McDonough, 1989) and depleted mantle (Nb/Ta = 14.29) (McDonough, 1990), but close to that of the continental crust (Nb/Ta = 11.43) (Rudnick and Fountain, 1995). The large ion lithophile elements are significantly enriched. On the trace element spider diagram (Figure 8), the trace element spider distribution curves of the five rock samples are basically consistent. They are characterized by the strong incompatible elements such as Rb, Ba, Th, K being more enriched than the moderately incompatible elements such as Sr, Nb, P, Zr. Among them, Rb, Th, U, K, La, Pb, Pr, Nd, Sm, Gd show significant positive anomalies on the trace element ratio spider diagram, while Cs, Ba, Nb, Ce, P, Zr, Ti show obvious negative anomalies.

FIGURE 8

Anders and Grevesse, 1989).

Discussion

Petrogenesis of magnesian andesite

Current petrogenetic models for magnesian andesites primarily include: (1) assimilation-fractional crystallization (AFC) of mantle-derived basaltic magmas (Macpherson et al., 2006); (2) partial melting of hydrous mantle peridotite (Straub et al., 2011); (3) reaction between delaminated lower crust and mantle peridotite (Xu et al., 2002); (4) mixing of crustal felsic and mantle-derived basaltic magmas (Streck et al., 2007); and (5) metasomatic interactions between subducted slab melts/sediment melts/slab-derived fluids and overlying mantle wedge (Dong and Santosh, 2016).

The Nangunyuan magnesian andesites in northern Hainan Island exhibit elevated SiO₂ (53.12–58.34 wt%), CaO (6.23–8.15 wt%), and MgO (5.67–7.89 wt%) contents, coupled with relatively low Na₂O (2.12–3.45 wt%), K₂O (0.78–1.56 wt%), and Fe₂O₃ (6.34–7.89 wt%) concentrations. Their position within the LF-CA field on the SiO₂-FeO*/MgO diagram (Figure 9) confirms their classification as magnesian andesites, precluding their origin from partial melting of basaltic rocks. Delamination models typically operate under crustal thickening conditions with garnet as the dominant residual phase. Given the strong compatibility of heavy rare earth elements (HREEs) and Y in garnet, significant HREE and Y depletion serves as a diagnostic indicator of garnet residue (Xu et al., 2002). However, the studied samples display low (Dy/Yb)N ratios (1.16–1.41), coupled with elevated Yb (2.69–6.36 ppm) and Y (23.67–79.23 ppm) concentrations, demonstrating the absence of substantial garnet residues in their source. Furthermore, delaminated lower crust melting typically generates high Sr/Y adakites with Mg^# <45 (Huang et al., 2007), whereas the Mg^# values of these andesites range from 45.78 to 54.07, systematically exceeding the threshold. These geochemical contradictions effectively exclude the delamination-peridotite reaction model as a viable mechanism for the Nangunyuan magnesian andesites.

FIGURE 9

The magnesian andesites from the Nangunyuan area in northern Hainan Island exhibit diagnostic arc volcanic signatures, as evidenced by their elevated Zr/Nb ratios (13.76–20.06), low Nb/La (0.091–0.342), and Nb/Th ratios (0.858–1.252) – geochemical parameters characteristic of typical island arc systems. These rocks display marked enrichment in large-ion lithophile elements (LILEs) coupled with relative depletion of high-field-strength elements (HFSEs), accompanied by pronounced negative anomalies in Ta, Nb, and Ti, features consistent with active continental margin or arc volcanic settings. The HFSEs (Zr, Hf, Nb, Ta), being relatively immobile during alteration and metamorphic processes, serve as robust tracers for source characterization. Ratios between these elements (Nb/Ta, Zr/Nb) provide critical petrogenetic constraints, particularly given the limited fractionation of Nb/Ta ratios during mantle partial melting or magmatic differentiation. The studied andesites show Nb/Ta ratios (average 11.5) comparable to continental crust values (11–13), while their Zr/Nb ratios align with primitive mantle compositions. This dual signature implies significant crustal contamination during magma evolution. Further confirmation comes from immobile element discrimination diagrams: The Nb/Th versus Nb plot (Figure 10) and Ce/Pb versus Ce systematics (Figure 11) consistently classify these rocks within the arc volcanic field. The integrated geochemical evidence demonstrates that crustal material incorporation played a pivotal role in modifying mantle-derived magmas, likely through subduction-related processes involving slab-derived fluids or sediment melts.

FIGURE 10

Li et al., 2015) MORB: mid-ocean-ridge basalt; OIB: ocean-island basalts.

FIGURE 11

Foley et al., 2002) MORB: mid-ocean-ridge basalt; OIB: ocean-island basalts.

The Sanukite from the Setouchi region of Japan represents a typical island arc volcanic rock, characterized by high silica content and elevated Mg, Cr, and Ni concentrations (Tatsumi, 2008). Although the magnesian andesites from Nangunyuan area in northern Hainan Island plot within the sanukite field on the Y-Sr/Y diagram (Figure 12) and share similar geochemical signatures with sanukite, they exhibit notably lower MgO (Mg#), Ni, and Cr contents compared to the Japanese Sanukite. The Nb/Ta ratios of these Hainan samples range from 8.4 to 13.46 (average 11.5), consistently lower than those of chondrites (17.5), primitive mantle (17.5), mid-ocean ridge basalts (15-16), and depleted mantle, but comparable to continental crust values (11-13). In the Zr-(Nb/Zr)N classification diagram (Figure 13), the Hainan magnesian andesites predominantly fall within the subduction-related rock field.

FIGURE 12

Kamei et al., 2004).

FIGURE 13

Thieblemont and Tegyey, 1994).

The Th/Nb-Ce/Nb systematics (Figure 14) further indicate that these rocks plot near arc volcanic magma fields, suggesting their magmatic formation might be associated with arc-related processes. This implies potential incorporation of deep-sea sediments or crustal materials into their source region. Petrogenetic modeling supports a source region formed through metasomatic reactions between mantle peridotite and Si-rich melts derived from partial melting of subducted oceanic crust or sediments (Figure 15). In contrast, the Setouchi sanukite originates from mantle wedge environments in subduction zones, representing typical products of crust-mantle interaction (Tatsumi, 2008).

FIGURE 14

Song et al., 2004) N-MORB: Normal Mid-Ocean Ridge Basalt; E-MORB: Enriched Mid-Ocean Ridge Basalt; OIB: ocean-island basalts; CFB: Continental Flood Basalt; UCC: Upper Continental Crust; PM: Primitive Mantle.

FIGURE 15

While the Hainan magnesian andesites share genetic similarities with typical arc-related rocks from Setouchi in terms of geochemical characteristics and formation mechanisms, their distinct compositional differences reflect unique tectonic-magmatic evolutionary processes in different regional settings. Comparatively, these Hainan rocks exhibit analogous petrogenetic patterns to magnesian andesites from the northeastern margin of the North China Craton (Guo et al., 2022) and the Qinling orogen (Li et al., 2020), all originating from hybrid sources involving interactions between subducted slab-derived melts (or sediments) and mantle peridotite.

Geotectonic significance

The EW-trending Changjiang-Qionghai Fault in Hainan Island was initially inferred from contrasting geological and geophysical characteristics across its northern and southern sectors. However, its tectonic nature and final amalgamation age remain contentious. Along the fault’s northern flank (Junying, Bangxi, Bayi Farm, Nanfeng, Chenxing Farm, Zhongrui Farm), discontinuous meta-volcanic rocks ranging from acidic to ultramafic compositions have been identified, predominantly mafic lithologies occurring as stratiform, lenticular, or irregular bodies within Paleozoic deep-to shallow-marine metasedimentary sequences. Over the past 2 decades, multidisciplinary studies have proposed three principal genetic models: 1. Late Paleozoic bimodal volcanic suites representing intracontinental rifting (Xia and Shi, 1991) or coeval Paleo-Tethyan oceanic basin development (Tang, 1999); 2. Mesoproterozoic komatiitic basalts indicative of Paleoproterozoic subduction and Meso-Neoproterozoic crustal breakup (Zhang et al., 1998; Liang et al., 2000; Xu et al., 2001); 3. Mid-ocean ridge basalt (MORB) or ocean island basalt (OIB) assemblages interpreted as remnants of the eastern Paleo-Tethyan oceanic crust (Li et al., 2000b) or coeval Paleo-Tethyan basins (Wang et al., 2013; Metcalfe, 2021). These conflicting interpretations, largely based on localized lithological observations, fail to reconcile regional tectonic coherence. Xu et al. (2006) proposed a temporal-spatial framework: Mafic lavas at Chenxing Farm (Tunchang County) may record ∼450 Ma Early Paleozoic oceanic crust, while Junying-Bangxi mafic rocks potentially reflect ∼270 Ma back-arc spreading during Late Paleozoic subduction of the eastern Paleo-Tethyan Ocean beneath the South China margin. Peak subduction of the eastern Paleo-Tethyan Ocean occurred during the Carboniferous-Permian, with its closure constrained to ∼237–247 Ma (Xu et al., 2019; Yu et al., 2022). The Nangunyuan magnesian andesites in northern Hainan, dated to this interval, likely represent terminal-stage subduction processes. Supporting evidence includes N-MORB-type amphibolite-facies metabasites along the Changjiang-Qionghai Fault (Li et al., 2000a), geochemically correlative with the Jinshajiang-Song Ma ophiolites, suggesting Hainan’s Late Paleozoic basin constituted the easternmost Paleo-Tethyan extension. Petrogenetic models posit that hydrous slab-derived fluids metasomatized the mantle wedge, generating Mg-rich melts that mixed with peridotite to form magnesian andesites–a process confirming active Paleo-Tethyan subduction persisting into the Late Permian (Figure 15).

Conclusion

The Mg andesite in the Nangunyuan area of northern Hainan Island occurs as interbeds and lenses in late Paleozoic strata. It belongs to the neutral to acidic rock association of the high-potassium calc-alkaline series - olivine basalt series. The rocks are characterized by relatively high contents of SiO₂, CaO, and MgO, and relatively low contents of Na₂O, K₂O, and Fe₂O₃. Moreover, the Mg^# values range from 45.78 to 54.07. The petrogeochemical characteristics of the rocks indicate features of magnesian andesite. Geochemical discrimination diagrams suggest that the rocks possess typical island-arc volcanic features and belong to island-arc volcanic rocks.

These rocks exhibit geochemical affinities comparable to sanukite-type magmas, yet display distinctively lower MgO, Ni, and Cr concentrations relative to typical sanukites. Their Nb/Ta ratios (8.4–13.46) align with continental crustal values, suggesting source contamination through incorporation of deep-sea sediments or crustal materials. Petrogenetic modeling supports formation via metasomatic reactions between mantle peridotite and Si-rich melts derived from partial melting of subducted oceanic slabs/sediments. This geochemical fingerprint implies the operation of arc-active continental margin subduction systems during the Late Paleozoic. In future research, Sr-Nd-Hf isotope analysis and zircon U-Pb isotopic dating will be supplemented to enhance the argumentation basis and render the results more reliable.

(3) LA-ICP-MS zircon U-Pb dating constrains the magnesian andesites’ emplacement age to 251.2 ± 4.5 Ma (Late Permian), temporally coincident with the terminal closure of the eastern Paleo-Tethys Ocean (∼237–247 Ma). This chronological correlation positions their formation within the waning stages of Paleo-Tethyan subduction. Our findings provide critical constraints for refining the closure timeline of the eastern Paleo-Tethyan Ocean, deciphering the geodynamic mechanisms of Paleo-Tethyan orogenesis and elucidating metallogenic processes in convergent margin settings, thereby enhancing our understanding of East Asian tectonic evolution.

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