| Zhang Jie,Chen Ling,Cheng Zihua,Tang Limei.Geological characteristics of the Nankai Trough subduction zone and their tectonic significances[J].Acta Oceanologica Sinica,2020,39(10):81-95 |
| 日本南海海槽俯冲带的地质特征及其构造意义 |
| Geological characteristics of the Nankai Trough subduction zone and their tectonic significances |
| 投稿时间：2020-01-06 |
| DOI：10.1007/s13131-020-1663-4 |
| 中文关键词: 南海海槽 俯冲带 速度结构 重力模拟 地球化学 岩石学 板片熔融 地质效应 |
| 英文关键词:Nankai Trough subduction zone velocity structure gravity modeling geochemistry petrology slab melting geological effect |
| 基金项目: |
| 作者 | 单位 | E-mail | | 张洁 | 自然资源部第二海洋研究所, 自然资源部海底科学重点实验室, 杭州, 310012
南方海洋科学与工程广东省实验室（珠海）, 珠海, 519080 | | | 陈灵 | 自然资源部第二海洋研究所, 自然资源部海底科学重点实验室, 杭州, 310012
自然资源部广州海洋地质调查局, 自然资源部海底矿产资源重点实验室, 广州, 510760 | chenling@sio.org.cn | | 程子华 | 中国科学院南海海洋研究所, 中国科学院边缘海与大洋地质重点实验室, 广州, 510301 | | | 唐立梅 | 自然资源部第二海洋研究所, 自然资源部海底科学重点实验室, 杭州, 310012 | |
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| 中文摘要: |
| 日本西南部的南海海槽是一个典型的俯冲系统，由菲律宾海板块向欧亚板块俯冲形成，其俯冲板片包含了九州-帕劳洋脊（KPR）、Kinan海山链、四国海盆和伊豆-小笠原岛弧（IBA）等多种地质单元。为了研究不同地质单元的板块俯冲效应，本文系统分析了南海海槽的地球物理和岩石地球化学特征。重力和热流特征显示南海海槽中部具有低的重力异常（-20–-40 mGal）和高的热流值（60–200 mW/m2），而东西两侧的热流值（20–80 mW/m2）较低。地震模拟结果显示俯冲板块的地壳厚度为5–20 km。地球化学结果表明俯冲板块的下覆地幔成分从西到东逐渐亏损。无震洋脊（如KPR、Kian海山链和Zenisu洋脊）的俯冲是控制南海海槽俯冲效应的主要因素。首先，无震洋脊的俯冲可能使上覆板块发生变形，沿着增生楔前缘出现不规则的地形凹陷。其次，无震洋脊的俯冲是大型逆冲地震的止裂体，阻碍了南海海槽1944年Mw 8.1和1946年Mw 8.3地震破裂的传播。此外，KPR和热的、年轻的四国海盆的俯冲会导致俯冲板片熔融，在日本岛弧上出现埃达克质岩浆活动，并为斑岩铜金矿床提供成矿物质。地球物理和地球化学特征的差异表明尽管IBA已经和日本岛弧发生碰撞，但作为IBA的残留弧，KPR仍然处于俯冲阶段，与日本岛弧之间有明显的地形分界，呈现单向收敛的状态。 |
| 英文摘要: |
| The Nankai Trough subduction zone is a typical subduction system characterized by subduction of multiple geological units of the Philippine Sea Plate (the Kyushu-Palau Ridge, the Shikoku Basin, the Kinan Seamount Chain, and the Izu-Bonin Arc) beneath the Eurasian Plate in the southwest of Japan. This study presents a geophysical and geochemical analysis of the Nankai Trough subduction zone in order to determine the features and subduction effects of each geological unit. The results show that the Nankai Trough is characterized by low-gravity anomalies (–20 mGal to –40 mGal) and high heat flow (60–200 mW/m2) in the middle part and low heat flow (20–80 mW/m2) in the western and eastern parts. The crust of the subducting plate is 5–20 km thick. The mantle composition of the subducting plate is progressively depleted from west to east. Subduction of aseismic ridges (e.g., the Kyushu-Palau Ridge, the Kinan Seamount Chain, and the Zenisu Ridge) is a common process that leads to a series of subduction effects at the Nankai Trough. Firstly, aseismic ridge or seamount chain subduction may deform the overriding plate, resulting in irregular concave topography along the front edge of the accretionary wedge. Secondly, it may have served as a seismic barrier inhibiting rupture propagation in the 1944 Mw 8.1 and 1946 Mw 8.3 earthquakes. In addition, subduction of the Kyushu-Palau Ridge and hot and young Shikoku Basin lithosphere may induce slab melting, resulting in adakitic magmatism and the provision of ore-forming metals for the formation of porphyry copper and gold deposits in the overriding Japan Arc. Based on comparisons of their geophysical and geochemical characteristics, we suggest that, although the Izu-Bonin Arc has already collided with the Japan Arc, the Kyushu-Palau Ridge, which represents a remnant arc of the Izu-Bonin Arc, is still at the subduction stage characterized by a single-vergence system and a topographic boundary with the Japan Arc. |
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