He-Ar isotopic signatures of the Mesozoic granitoids in South Korea: implications for genesis of the granitic magma and crustal evolution in NE continental margin of the Eurasian plate

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Geosciences Journal Pub Date : 2024-09-07 DOI:10.1007/s12303-024-0038-9
Kyu Han Kim, Keisuke Nagao, Hirochika Sumino, Jong Ik Lee, Jisun Park
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Abstract

In order to constrain the granitic magma source at the northeastern continental margin of the Eurasian plate, noble gas isotopic ratios such as helium (3He/4He), argon (40Ar/36Ar) and neon (20Ne/22Ne, 21Ne/22Ne) were determined for Mesozoic quartz and biotite minerals from granitic rocks in the Korean peninsula. 3He/4He ratios in fluid inclusions of quartz samples have a wide range from 0.005 to 0.522 RA (av. 0.095 RA) and 0.013 to 1.27 RA (av. 0.37 RA) (RA =1.40 × 10−6, atmospheric value) for Jurassic (Daebo) and Cretaceous (Bulguksa) granites, respectively. The 3He/4He ratios clearly show a contribution of mantle-derived He to the granitic rock at the formation, then the helium has been deeply affected by accumulation of in situ produced radiogenic 4He and/or crustal helium. Although these ratios are lower than those of the subcontinental lithospheric mantle (SCLM) (6.1 ± 0.9 RA), mantle helium has been traced in these Mesozoic I-type granites from South Korea. The observations imply that the helium of SCLM source predominates over all of the Jurassic granites in South Korea and the Cretaceous granites in the Ogcheon belt (OB), and suggests that the granitic magma was derived from the partial melting product of SCLM materials with appreciable amounts of radiogenic helium. Meanwhile, Cretaceous granites were originated from igneous mantle source materials beneath the Gyeongsang basin, south-eastern area of the Korean peninsula. A presence of mantle components (20Ne/22Ne ≈ 10.13) and/or nucleogenic Ne were identified in some quartz and most biotite samples of granitoids in Jurassic age. Argon isotopic ratios (av. 40Ar/36Ar = 2370) of fluid inclusions in quartz for Jurassic granites are considerably higher than those in Cretaceous granites (av. 40Ar/36Ar = 414), indicating a clear aging effect. He-Ar isotopic signatures together with the characteristics of Nd, Sr, and O isotopes can lead to the conclusion that the generation of Jurassic granitic magma was responsible for the subduction of the Izanagi oceanic plate. Meanwhile, the subduction ridge (e.g., the Kula-Pacific Ridge) model is likely to be a suitable scenario for formation of the Cretaceous granitic magma in the Korean peninsula.

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韩国中生代花岗岩的He-Ar同位素特征:对欧亚板块东北大陆边缘花岗岩岩浆成因和地壳演化的影响
为了确定欧亚板块东北大陆边缘的花岗岩岩浆来源,测定了朝鲜半岛花岗岩中生代石英和生物岩矿物中的氦(3He/4He)、氩(40Ar/36Ar)和氖(20Ne/22Ne、21Ne/22Ne)等惰性气体同位素比值。侏罗纪(Daebo)和白垩纪(Bulguksa)花岗岩石英样品流体包裹体中的 3He/4He 比值范围很广,分别为 0.005 至 0.522 RA(平均 0.095 RA)和 0.013 至 1.27 RA(平均 0.37 RA)(RA =1.40 × 10-6,大气值)。3He/4He比率清楚地表明,花岗岩在形成时有来自地幔的氦,然后氦又受到原地产生的放射性4He和/或地壳氦的积累的深刻影响。虽然这些比率低于次大陆岩石圈地幔(SCLM)的比率(6.1 ± 0.9 RA),但在这些来自韩国的中生代 I 型花岗岩中还是追踪到了地幔氦。这些观测结果表明,在韩国所有的侏罗纪花岗岩和Ogcheon带(OB)的白垩纪花岗岩中,SCLM来源的氦占主导地位,并表明花岗岩岩浆是来自SCLM物质的部分熔融产物,其中含有相当数量的放射性氦。同时,白垩纪花岗岩源于朝鲜半岛东南部庆尚盆地下的火成岩幔源物质。在侏罗纪花岗岩的一些石英和大多数生物岩样品中发现了地幔成分(20Ne/22Ne ≈ 10.13)和/或核生氖。侏罗纪花岗岩石英中流体包裹体的氩同位素比值(平均 40Ar/36Ar = 2370)大大高于白垩纪花岗岩(平均 40Ar/36Ar = 414),显示出明显的老化效应。He-Ar同位素特征以及Nd、Sr和O同位素特征可以得出结论,侏罗纪花岗岩岩浆的生成是伊邪那岐大洋板块俯冲的原因。同时,俯冲海岭(如库拉-太平洋海岭)模式很可能是朝鲜半岛白垩纪花岗岩岩浆形成的合适情景。
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来源期刊
Geosciences Journal
Geosciences Journal 地学-地球科学综合
CiteScore
2.70
自引率
8.30%
发文量
33
审稿时长
6 months
期刊介绍: Geosciences Journal opens a new era for the publication of geoscientific research articles in English, covering geology, geophysics, geochemistry, paleontology, structural geology, mineralogy, petrology, stratigraphy, sedimentology, environmental geology, economic geology, petroleum geology, hydrogeology, remote sensing and planetary geology.
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