Formation and Evolution of the Late Triassic Granite Buried Hill in the Songnan Low Uplift, Qiongdongnan Basin
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摘要: 为了进一步研究松南低凸起花岗岩潜山演化过程，对Y8-A井基底二长花岗岩进行年代学、主微量、Sr-Nd-Pb-Hf同位素、磷灰石裂变径迹和锆石（U-Th）/He分析.LA-ICP-MS锆石U-Pb定年结果为235.6±4.8 Ma，基性岩脉40Ar/39Ar坪年龄为141.57±0.63 Ma.花岗岩主微量元素特征表明其为高钾钙碱性、过铝质S型花岗岩.花岗岩（87Sr/86Sr）i比值为0.707 93~0.709 44，εNd（t）值为-4.45~-6.39，εHf（t）值为-5.6~1.5.磷灰石裂变径迹年龄为66.3±5.6 Ma，锆石（U-Th）/He单颗粒年龄为（82.05±1.99）~（45.93±1.14）Ma.综合研究表明，二长花岗岩形成于印支与华南碰撞拼合后的后碰撞背景，热史反演结果表明花岗岩潜山的演化可分为侵位冷凝、缓慢冷却、较快冷却、近地表剥露和沉降埋藏5个阶段.Abstract: To further study the evolution process of the Songnan Low Uplift granite buried hill, the basement monzogranite in well Y8-A are analysed by chronology, major and trace, Sr-Nd-Pb-Hf isotopes, apatite fission track, and zircon (U-Th)/He methods. LA-ICP-MS zircon U-Pb dating is 235.6±4.8 Ma. The mafic dikes 40Ar/39Ar flateau age is 141.57±0.63 Ma. These granites belong to high potassium calc alkaline and peraluminous S-type granite. Their (87Sr/86Sr)i, εNd(t), and εHf(t) values are 0.707 93-0.709 44, -4.45 to -6.39, and --5.6 to 1.5, respectively. The apatite fission track age is 66.3±5.6 Ma, and the single zircon (U-Th) /He particle age ranges from (82.05±1.99) to (45.93±1.14) Ma. The comprehensive study shows that the monzogranite was formed in the post-collision background after the collision between Indochina and South China. The thermal history inversion results show that the evolution of granite buried hill can be divided into five stages: emplacement, slow cooling, fast cooling, near-surface denudation and sediments burial.
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Key words:
- Qiongdongnan basin /
- Songnan low uplift /
- granite buried hill /
- petrogenesis /
- tectonic evolution /
- petrology /
- geochronology
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图 1 琼东南盆地构造单元(a)及松南低凸起剖面图(b)
a.据钟佳和王岩泉（2022）；b.据杨计海等（2019）.潜山基岩年龄数据来源于徐长贵等（2024）
Fig. 1. Tectonic unit of the Qiongdongnan Basin (a), and profile of the Songnan low uplift (b)
图 2 松南低凸起Y8-A井基底花岗岩岩屑、基性岩脉岩屑照片和显微照片
a.肉红色中细粒碎裂二长花岗岩/二长花岗斑岩岩屑；b.二长花岗岩单偏光镜下照片；c.二长花岗岩正交偏光镜下照片；d.灰黑色辉绿岩岩屑；e.蚀变辉绿岩单偏光镜下照片；f.蚀变辉绿岩正交偏光镜下照片；Aug.普通辉石；Kfs.钾长石；Pl.斜长石；Qz.石英
Fig. 2. Photos and micrographs of basement granite cuttings and basic dike cuttings of the well Y8-A in the Songnan low uplift
图 3 松南低凸起Y8-A井中生代花岗岩锆石CL图
Fig. 3. CL images of zircons from the well Y8-A in the Songnan low uplift
图 4 松南低凸起Y8-A井花岗岩锆石U-Pb谐和图(a)和加权平均年龄图(b)
Fig. 4. LA-ICP-MS U-Pb concordia diagram (a) and weighted mean age diagram (b) for the zircons from well Y8-A granite in the Songnan low uplift
图 5 松南低凸起Y8-A井花岗岩TAS图解(a)、K2O-SiO2图解(b)和A/NK-A/CNK图解(c)
Fig. 5. Total alkalis (K2O+Na2O) vs. SiO2 (TAS) (a), K2O vs. SiO2 (b), and A/NK (molar ratio Al2O3/(Na2O+K2O)) vs. A/CNK (molar ratio Al2O3/(CaO+Na2O+K2O)) (c) diagrams for the well Y8-A granite in the Songnan low uplift
图 6 松南低凸起Y8-A井中生代花岗岩哈克图解
Fig. 6. Harker diagram of the well Y8-A granite in the Songnan low uplift
图 7 松南低凸起Y8-A井中生代花岗岩球粒陨石标准化稀土元素配分模式图(a)和原始地幔标准化微量元素蛛网图(b)(标准化值据Sun and McDonough，1989)
Fig. 7. Chondrite-normalized REE (a) patterns and primitive mantle-normalized trace element spider (b) diagrams for the well Y8-A granite in the Songnan low uplift (the Chondrite and primitive mantle values are from Sun and McDonough, 1989)
图 8 松南低凸起Y8-A井花岗岩判别图解
a.εNd（t）-（86Sr/87Sr）i判别图解；b.εNd（t）-（86Sr/87Sr）i判别图解；c.（207Pb/204Pb）i-（2206Pb/204Pb）i判别图解；d.（2208Pb/204Pb）i-（2206Pb/204Pb）i判别图解. a~d.底图及参数详见Yan et al.（2017）；海南岛数据来源于葛小月等（2003），余金杰等（2012），Yan et al.（2017），芶琪钰等（2019），Cao et al.（2022）；南海NK-1井数据来源于Miao et al.（2021）
Fig. 8. Diagrams for the well Y8-A granite in the Songnan Low Uplift
图 9 松南低凸起Y8-A基底花岗岩锆石εHf(t)-t图解
海南岛数据来源于温淑女等（2013），Shen et al.（2018），赵国锋等（2018），Cao et al.（2022），吕方等（2023），齐重向等（2023）；琼东南盆地数据来源于Mi et al.（2023），徐长贵等（2024），周虎等（2024）；越南数据来源于Chen et al.（2014），Thanh et al.（2019），李慧玲等（2023）；哀牢山-金沙江数据来源于李龚健等（2013），巩小栋等（2020）；粤西数据来源于周岱等（2021）
Fig. 9. εHf(t)-t diagram for the well Y8-A granite in the Songnan low uplift
图 10 松南低凸起Y8-A井基性岩脉40Ar/39Ar年龄谱(a)、等时线(b)和反等时线(c)
Fig. 10. Age spectrum (a), isochron (b) and inverse isochron (c) of 40Ar-39Ar basic dike in well Y8-A, Songnan low uplift
图 11 松南低凸起Y8-A井花岗岩Nb-10 000 Ga/Al (a)、Th-Rb (b)、Y-Rb (c)、La/Sm-La (d)、La/Yb-La (e)、Th/Nd-Th (f)判别图解
Fig. 11. Nb-10 000 Ga/Al (a), Th-Rb (b), Y-Rb (c), La/Sm-La (d), La/Yb-La (e), Th/Nd-Th (f) discrimination diagrams for the well Y8-A granite in the Songnan low uplift
图 12 松南低凸起Y8-A基底花岗岩207Pb/204Pb-206Pb/204Pb(a，b)、208Pb/204Pb-206Pb/204Pb(c)、Δγ-Δβ(d)图解
Fig. 12. 207Pb/204Pb-206Pb/204Pb (a, b), 208Pb/204Pb-206Pb/204Pb (c), and Δγ-Δβ (d) discrimination diagrams for the well Y8-A granite in the Songnan Low Uplift
图 13 早三叠世(a)和中三叠世(b)南海及邻区板块构造演化重建及Y8-A井花岗岩岩浆成因示意图(c)
据Hennig et al.（2017）；Zheng et al.（2019）；Tian et al.（2021）
Fig. 13. Early Triassic (a) and Middle Triassic (b) reconstruction of plate tectonic evolution in the South China Sea and adjacent areas, and well Y8-A granite magma genesis schematic diagram(c)
图 14 松南低凸起Y8-A井基底花岗岩Nb-Y(a)、Rb-Y+Nb(b)、Rb/30-Hf-3×Ta(c)和R2-R1(d)判别图解
R1=4Si-11（Na+K）-2（Fe+Ti），R2=6Ca+2Mg.海南岛数据来源于葛小月（2003），谢才富等（2006），余金杰等（2012），Yan et al.（2017），Shen et al.（2018），赵国锋等（2018），芶琪钰等（2019），吕昭英等（2019），Cao et al.（2022），吕方等（2023），齐重向等（2023）；琼东南盆地数据来源于钟佳和王岩泉（2022），Mi et al.（2023），徐长贵等（2024）；越南数据来源于Chen et al.（2014），李慧玲等（2023），Thanh et al.（2019）；哀牢山-金沙江数据来源于李龚健等（2013），巩小栋等（2020）；川西数据来源于罗伟等（2023）；粤西数据来源于周岱等（2021）
Fig. 14. Nb-Y (a), Rb-Y+Nb (b), Rb/30-Hf-3×Ta (c) and R2-R1 (d) diagrams for the well Y8-A granite in the Songnan low uplift
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