日本地球惑星科学連合2024年大会

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[J] ポスター発表

セッション記号 S (固体地球科学) » S-GL 地質学

[S-GL18] 日本列島および東アジアの地質と構造発達史

2024年5月30日(木) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:羽地 俊樹(産業技術総合研究所 地質調査総合センター 地質情報研究部門)、大坪 誠(産業技術総合研究所 活断層・火山研究部門)

17:15 〜 18:45

[SGL18-P08] Is the Pre-Cenozoic basement of Taiwan strait an exotic terrane? : Constraints from detrital zircon and monazite U-Pb ages of Well TL-1 in Penghu Island

*Jian-wei Lin1 (1.Institute of Earth Sciences, Academia Sinica, Taiwan)

キーワード:Detrital zircon and monazite, U-Pb ages, pre-Cenozoic basement, exotic terrane, Taiwan Strait

The Pre-Cenozoic basement beneath the Taiwan Strait (TS) and East China Sea (ECS), considered an extension of the East Cathaysia Block (ECB), remains poorly understood with limited investigation into its crustal compositions. This study focuses on Well TL-1, a 900-meter-deep core on Penghu Island, employing coupled detrital zircon and monazite U-Pb ages of littoral-to-neritic facies sediments. The aim is to elucidate the crustal characteristics of the TS basement and its relationship with ECB. Below an unconformity at depth of 503 meters, five Early Cretaceous sand-siltstones exhibit a distinctive zircon age cluster of approximately 120 Ma with minor Early Jurassic (ca.190 Ma) inherited grains. These ages align with major magmatic episodes observed in the ECS basement. Positive eHf(t) features of these Jurassic-Cretaceous zircons suggest mantle-origin magmatism, contrasting with the Mesozoic crustal assimilation magmatic system in ECB. On the other hand, zircon age spectra from two Early Miocene sediments at depths of 403 and 500 meters reveal four groups, including ca.1.8 Ga, 800-700 Ma, 450-430 Ma, and 300-200 Ma, consistent with common deposits in ECS and the drainage systems of ECB. Notably, the presence of 1.8 Ga monazites (30-45 percent) in these samples, absent from neighboring continents, indicates an exotic provenance. The large grain sizes (larger than100 microns) and euhedral to subhedral morphology of these monazites further suggest a proximal source-sink relationship for the Miocene sediments. In summary, the features observed in Well TL-1 deposits suggest a potential disconnection between TS and ECB crusts, implying the concept of an allochthonous terrane. Additionally, the application of dual-mineral geochronology to sediments proves valuable in providing comprehensive information on source areas.