西太平洋雅浦海沟地幔演化与岩浆作用研究进展

田原; 陈灵; 唐立梅; 高鹏; 方银霞

doi:10.3799/dqkx.2021.003

Volume 46 Issue 3

Mar. 2021

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Tian Yuan, Chen Ling, Tang Limei, Gao Peng, Fang Yinxia, 2021. Research Progress on Mantle Evolution and Magmatism in the Yap Trench, Western Pacific. Earth Science, 46(3): 840-852. doi: 10.3799/dqkx.2021.003

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Tian Yuan, Chen Ling, Tang Limei, Gao Peng, Fang Yinxia, 2021. Research Progress on Mantle Evolution and Magmatism in the Yap Trench, Western Pacific. Earth Science, 46(3): 840-852. doi: 10.3799/dqkx.2021.003

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Research Progress on Mantle Evolution and Magmatism in the Yap Trench, Western Pacific

doi: 10.3799/dqkx.2021.003

Tian Yuan^{1, 2
,
,},
Chen Ling¹,
Tang Limei^{1
,
,},
Gao Peng¹,
Fang Yinxia¹

1.
Key Laboratory of Submarine Geosciences & Second Institute of Oceanography, MNR, Hangzhou 310012, China
2.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2020-10-30
Publish Date: 2021-03-01

Abstract

Abstract

Mantle evolution and magmatism in subduction zone are important geological processes in which circulation of materials and energy takes place among the solid layers of the earth. the Yap trench in the western Pacific ocean is an ideal place to study the evolution of subduction zone under complex conditions because of its unique geological structural characteristics such as extremely short trench-arc distance and ocean ridge-trench collision. In order to explore the mantle evolution and magmatism of the Yap trench, this paper analyzes the genesis of the igneous rocks of the Yap trench by integrating the previous research data on the igneous rocks of the Yap trench. According to the formation conditions of the igneous rocks, the mantle evolution and magmatism during the subduction of the Caroline Plate to the Philippine Sea Plate are discussed. The results show that igneous rocks of the Yap trench have the typical characteristics of subduction-related igneous rocks. The geochemical characteristics of peridotite indicate that the melting degree of mantle in Yap trench is 20%-25%, and the mantle is subjected to metasomatism of fluid and melt during the process of partial melting.The Re-Os isotope characteristics indicate that there is an ancient residual mantle with a Re depleted age of 1.16 Ga in the mantle of the Yap trench, indicating that the mantle may have experienced multi-stage melting events, resulting in a ultra-depleted mantle in the Yap trench. The origin of the Yap arc is still controversial up to now, mainly including: (1) The Yap arc is a part of the ocean crust of the Parece Vela basin, which was thrusting above the original Yap Arc in the Miocene due to the collision of the Caroline ridge. (2) Yap Arc experienced several stages of island arc magmatism in different tectonic periods, including forearc basalts at the initial stage of subduction (~52 Ma), island arc basalts after subduction (~25 Ma), and island arc basalts (7-11 Ma) after collision with the Caroline ridge (21 Ma). The 7-11 Ma island arc basalts indicate that the island arc magmatism in the Yap trench has not completely stopped due to the collision of the Caroline ridge and is likely rejuvenated in the Late Miocene.
- Yap trench,
- subduction zone,
- igneous rocks,
- mantle evolution,
- magmatism,
- marine geology

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References(52)

References

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Research Progress on Mantle Evolution and Magmatism in the Yap Trench, Western Pacific

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