俯冲带深海-岩石圈流体交换及其效应

doi:10.13745/j.esf.sf.2021.9.16

地学前缘 ›› 2022, Vol. 29 ›› Issue (5): 246-254.DOI: 10.13745/j.esf.sf.2021.9.16

俯冲带深海-岩石圈流体交换及其效应

邢会林¹^,²^,³(), 王建超¹^,³^,^*(), 逄硕¹^,²^,³, 王瑞泽¹^,³, 刘冬豫¹^,³, 马子涵¹^,³, 张愉玲¹^,³, 谭玉阳¹^,²^,³

1.中国海洋大学深海圈层与地球系统前沿科学中心/海底科学与探测技术教育部重点实验室/海洋地球科学学院, 山东青岛 266100
2.青岛海洋科学与技术试点国家实验室深海多学科交叉研究中心, 山东青岛, 266100
3.中国海洋大学海底科学与工程计算国际中心, 山东青岛 266100

收稿日期:2021-05-11 修回日期:2021-08-21 出版日期:2022-09-25 发布日期:2022-08-24
通信作者: 王建超
作者简介:邢会林(1965—),男,教授,博士生导师,主要从事超级计算地球科学理论、软件研发及其应用等研究工作。E-mail: h.xing@ouc.edu.cn
基金资助:
国家自然科学基金项目(92058211);国家自然科学基金项目(52074251);中央高校基本科研业务经费项目(842012003);高等学校学科创新引智计划项目(B20048)

Deep sea-lithosphere fluid exchange in subduction zones and its effects: A critical review

XING Huilin¹^,²^,³(), WANG Jianchao¹^,³^,^*(), PANG Shuo¹^,²^,³, WANG Ruize¹^,³, LIU Dongyu¹^,³, MA Zihan¹^,³, ZHANG Yuling¹^,³, TAN Yuyang¹^,²^,³

1. Frontiers Science Center for Deep Ocean Multispheres and Earth System/MOE Key Lab of Submarine Geosciences and Prospecting Techniques/College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2. Deep-Sea Multidisciplinary Research Center, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266100, China
3. International Center for Submarine Geosciences and Geoengineering Computing (iGeoComp), Ocean University of China, Qingdao 266100, China

Received:2021-05-11 Revised:2021-08-21 Online:2022-09-25 Published:2022-08-24
Contact: WANG Jianchao

摘要/Abstract

摘要：

俯冲带是地球上构造活动最复杂、最强烈的区域,也是地球物质循环系统的重要组成部分,对俯冲带的深入研究有助于加深我们对地球系统科学的认识。通过系统地梳理分析国内外相关文献,大洋岩石圈通过在汇聚板块边界的俯冲将大量水带入到地幔中,并对俯冲带地震的发生、地幔的熔融、岩浆的产生、陆壳的形成乃至矿产资源富集都起到了重要的控制作用。弧前隆起区的岩石圈地幔在顺断层渗透的深海水作用下发生强烈水化作用并形成水化地幔,是水富集在岩石圈的主要方式之一。随着俯冲板片深度的增加,在一定的温压条件下,水化地幔(蛇纹岩)发生脱水相变,引发俯冲带中源地震。脱出的水则由于运移的差异,既可以产生板内的水压致裂,也会影响俯冲界面的耦合,进而导致慢滑移地震区的形成。由此可见,俯冲带地区深海-岩石圈流体交换及其在深部的效应是一个包含化学反应-温度-流体流动-应力变形/破坏的多物理场耦合的复杂动力学系统。然而,目前的相关研究工作主要侧重于对其中某个因素、现象或者某个特定条件下具体过程的探索性观测分析研究。因此,我们需要从地球系统科学的角度出发,将流体运移、化学反应与传统的固体地球研究相结合,着眼于多学科交叉的多场耦合动力学综合研究,对俯冲带地区深海-岩石圈流体交换及其效应进行多时空尺度定量化表征和分析。

关键词: 俯冲带, 流体交换, 相变反应, 流体运移, 多场耦合动力学

Abstract:

The subduction zone has the most complex and intense tectonic activities on Earth and is also an important part of the Earth's material circulation system. In-depth study of subduction zones will help deepen our understanding of the earth system. According to published results, it is believed that the oceanic lithosphere brings large amounts of water into the mantle through subduction at the boundary of the convergent plate, and this phenomenon is responsible for the control of subduction earthquakes, mantle melting, magma production, continental crust formation, and even mineral enrichment. The lithospheric mantle of the fore-arc uplift area is intensively hydrated by deep seawater infiltration along faults, and mantle hydration is one of the main ways of water accumulation in the lithosphere. With the increase of subduction depth, the hydrous serpentinized mantle dehydrates under certain temperature and pressure conditions, leading to intermediate earthquakes in the subduction zone. Moreover, due to differences in water migration, the separated water not only can cause hydrofracturing in the plate, but also can affect subduction interface coupling to form slow slip zones. Hence, fluid exchange between the deep sea and lithosphere in the subduction zone and its effect in the deep earth are complex dynamic processes with multiphysics couplings between chemical reaction, temperature, fluid migration and stress deformation. However, current researches mainly focus on exploratory observation and analysis of specific factors, phenomena or processes under certain conditions. Future research, therefore, needs to focus on the comprehensive, multidisciplinary study of multiphysics coupling dynamics from the perspective of earth system science, integrating fluid migration and chemical reaction into conventional solid earth research to quantitatively characterize/analyze the deep sea-lithosphere fluid exchange and its effects on the subduction dynamics at multiple spatiotemporal scales.

Key words: subduction zone, fluid exchange, phase changes, fluid migration, multi-physics coupling dynamics

中图分类号:

P313

邢会林, 王建超, 逄硕, 王瑞泽, 刘冬豫, 马子涵, 张愉玲, 谭玉阳. 俯冲带深海-岩石圈流体交换及其效应[J]. 地学前缘, 2022, 29(5): 246-254.

XING Huilin, WANG Jianchao, PANG Shuo, WANG Ruize, LIU Dongyu, MA Zihan, ZHANG Yuling, TAN Yuyang. Deep sea-lithosphere fluid exchange in subduction zones and its effects: A critical review[J]. Earth Science Frontiers, 2022, 29(5): 246-254.

图/表 5

图1 多种地球物理手段探测的海沟前缘隆起区水化断层通道(a,b,d据文献[41]修改;c据文献[33]修改;e据文献[47]修改) a—海底多波束探测;b—多道地震反射剖面;c—叠后有限差分时间偏移剖面;d—P波速度结构;e—主动源电磁探测。

Fig.1 Hydration fault channels in the uplift area at the trench front detected by various geophysical methods. a,b,d modified after [41]; c modified after [33]; e modified after [47].

图2 大洋岩石圈地幔蛇纹岩脱水反应矿物相变示意图(据文献[55-56]修改)

Fig.2 Dehydration induced phase transition in serpentinized oceanic lithospheric mantle. Modified after [55-56].

图3 按p-T条件分列的蛇纹石流变行为概要(据文献[52]修改)

Fig.3 Summary of serpentine rheological behavior according to p-T conditions. Modified after [52].

图4 微观结构下流体沿板块内部裂隙与离散断层运移示意图(据文献[70-71]修改)

Fig.4 Schematic of microscopic intraplate fluid migrations along fractures and discrete faults. Modified after [70-71].

图5 板内断层水化模式及应力传播示意图(据文献[75]修改)

Fig.5 Schematics of fault-mediated plate hydration (left) and stress propagation along faults (right). Modified after [74].

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俯冲带深海-岩石圈流体交换及其效应

Deep sea-lithosphere fluid exchange in subduction zones and its effects: A critical review

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