东印度洋爪哇板块边缘俯冲结构及其对地质灾害的影响

doi:10.11978/2025117

热带海洋学报 ›› 2026, Vol. 45 ›› Issue (1): 35-43.doi: 10.11978/2025117CSTR: 32234.14.2025117

东印度洋爪哇板块边缘俯冲结构及其对地质灾害的影响

张翠梅¹^,²(), 张洁³, 孙珍⁴(), 丁巍伟³, 张江阳¹^,², 邱宁¹^,², 李付成⁴, 姜峰⁴, 赵阳慧³, 蔡佩思⁵

¹热带海洋环境与岛礁生态全国重点实验室(中国科学院南海海洋研究所), 广东广州 511458
²边缘海与大洋地质实验室(中国科学院南海海洋研究所), 广东广州 510301
³海底科学与划界全国重点实验室(自然资源部第二海洋研究所), 浙江杭州 310012
⁴广州海洋地质调查局, 广东广州 511458
⁵中国科学院大学, 北京 100049

收稿日期:2025-07-25 修回日期:2025-08-13 出版日期:2026-01-10 发布日期:2026-01-30
通讯作者: 孙珍。email: sun_zhen2024@126.com
作者简介:
张翠梅(1981—), 女, 副研究员, 博士, 主要从事海洋盆地构造分析与模拟研究。email: cmzhang@scsio.ac.cn
基金资助:
国家重点研发计划项目(2023YFF0803402); 国家重点研发计划项目(2024YFB3908104)

Subduction structure and its influence on geological hazards at the Java Plate margin in the eastern Indian Ocean

ZHANG Cuimei¹^,²(), ZHANG Jie³, SUN Zhen⁴(), DING Weiwei³, ZHANG Jiangyang¹^,², QIU Ning¹^,², LI Fucheng⁴, JIANG Feng⁴, ZHAO Yanghui³, CHUA Peisi⁵

¹State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 511458, China
²Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
³State Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
⁴Guangzhou Marine Geological Survey, Guangzhou 511458, China
⁵University of Chinese Academy of Sciences, Beijing 100049, China

Received:2025-07-25 Revised:2025-08-13 Online:2026-01-10 Published:2026-01-30
Contact: SUN Zhen. email: sun_zhen2024@126.com
Supported by:
National Key Research and Development Program of China(2023YFF0803402); National Key Research and Development Program of China(2024YFB3908104)

摘要/Abstract

摘要：

作为活跃的汇聚带, 巽他弧以强震、海啸和火山活动著称, 而目前对东巽他弧板块边缘的关注相对较少。该研究全面梳理了爪哇东至松巴哇岛板块边缘的俯冲洋壳、海沟及增生楔沿走向的变化, 探讨了俯冲板块地形地貌对上覆板块变形的控制, 并揭示了俯冲作用对浅部地质灾害的影响。结果表明研究区俯冲结构具有显著的分段性, 西部和东部分别受Roo隆起和阿尔戈深海平原俯冲所控制。俯冲板块的海底地貌和结构导致了海沟和弧前区变形不同: Roo隆起俯冲造成侵蚀作用, 形成范围较小的增生楔, 且倾斜坡度大; 深海平原俯冲对应发育宽缓增生楔。无论海山/隆起俯冲或俯冲板块挠曲产生的正断层都可能触发地质灾害的发生。相关结论为理解俯冲增生过程、地震和海啸灾害提供了理论依据。

关键词: 海山俯冲, 地质灾害, 爪哇海沟, 俯冲带, 板块边缘

Abstract:

As an active convergent margin, the Sunda Arc is renowned for its intense seismic activity, tsunamis, and volcanic eruptions, and yet relatively less attention has been paid to its eastern segment. This study describes the along-strike variations of the subducting oceanic crust, trench, and accretionary wedge from eastern Java to Sumbawa Island. It investigates the control of subducting plate topography on the deformation of the overriding plate and reveals the influence of subduction on shallow geological hazards. The results show significant segmentation of the subduction structure in the study area, with the western and eastern parts controlled by the subduction of the Roo Rise and the Argo Abyssal Plain, respectively. The seafloor topography and structures of the subducting plate lead to distinct variations of trench and forearc deformation: the subduction of the Roo Rise results in prominent erosion and the development of a narrow and steeply inclined accretionary wedge, while that of the abyssal plain results in a broad and gently sloping accretionary wedge. Both seamount/rise subduction and normal faulting generated by plate bending may trigger geological hazards. These findings provide a theoretical basis for understanding accretion processes of subduction zones, as well as earthquake and tsunami hazards.

Key words: seamount subduction, geological hazards, Java trench, subduction zone, plate margin

中图分类号:

P542

张翠梅, 张洁, 孙珍, 丁巍伟, 张江阳, 邱宁, 李付成, 姜峰, 赵阳慧, 蔡佩思. 东印度洋爪哇板块边缘俯冲结构及其对地质灾害的影响[J]. 热带海洋学报, 2026, 45(1): 35-43.

ZHANG Cuimei, ZHANG Jie, SUN Zhen, DING Weiwei, ZHANG Jiangyang, QIU Ning, LI Fucheng, JIANG Feng, ZHAO Yanghui, CHUA Peisi. Subduction structure and its influence on geological hazards at the Java Plate margin in the eastern Indian Ocean[J]. Journal of Tropical Oceanography, 2026, 45(1): 35-43.

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参考文献 32

[1]	丁巍伟, 朱日祥, 万博, 等, 2023. 新特提斯洋东南段动力过程及东南亚环形俯冲体系形成机制[J]. 中国科学: 地球科学, 53(4): 687-701.
	DING WEIWEI, ZHU RIXIANG, WAN BO, et al, 2023. Geodynamic processes of the southeastern Neo-Tethys Ocean and the formation mechanism of the curved subduction system in Southeast Asia[J]. Science China Earth Sciences, 66(4): 703-717. doi: 10.1007/s11430-022-1071-4
[2]	李付成, 孙珍, 张江阳, 2016. 海山俯冲过程中的变形特征——物理模拟和数值模拟证据[J]. 热带海洋学报, 35(1): 31-37. doi: 10.11978/2015002
	LI FUCHENG, SUN ZHEN, ZHANG JIANGYANG, 2016. Deformation of seamount during subduction: Insights from sandbox experiment and numerical simulation[J]. Journal of Tropical Oceanography, 35(1): 31-37 (in Chinese with English abstract). doi: 10.11978/2015002
[3]	李付成, 孙珍, 张云帆, 等, 2012. 海山的倾斜俯冲对上覆板块变形的影响[J]. 地球物理学进展, 27(4): 1406-1415.
	LI FUCHENG, SUN ZHEN, ZHANG YUNFAN, et al, 2012. Influence of oblique seamount subduction on the deformation of upper plate[J]. Progress in Geophysics, 27(4): 1406-1415 (in Chinese with English abstract).
[4]	冉伟民, 鲁银涛, 魏新元, 等, 2022. 东印度洋Roo海隆区域属性及其俯冲区域响应特征[J]. 地球物理学报, 65(8): 3025-3039.
	RAN WEIMIN, LU YINTAO, WEI XINYUAN, et al, 2022. The nature and the response characteristics of the Roo Rise to subduction zone in the eastern Indian Ocean[J]. Chinese Journal of Geophysics, 65(8): 3025-3039 (in Chinese with English abstract).
[5]	ABERCROMBIE R E, ANTOLIK M, FELZER K, et al, 2001. The 1994 Java tsunami earthquake: Slip over a subducting seamount[J]. Journal of Geophysical Research: Solid Earth, 106(B4): 6595-6607.
[33]	SANDWELL D T, MÜLLER R D, SMITH W H F, et al, 2014. New global marine gravity model from CryoSat-2 and Jason-1 reveals buried tectonic structure[J]. Science, 346(6205): 65-67. doi: 10.1126/science.1258213
[34]	SATAKE K, TANIOKA Y, 1999. Sources of tsunami and tsunamigenic earthquakes in subduction zones[J]. Pure and Applied Geophysics, 154: 467-483. doi: 10.1007/s000240050240
[35]	SHULGIN A, KOPP H, MUELLER C, et al, 2011. Structural architecture of oceanic plateau subduction offshore Eastern Java and the potential implications for geohazards[J]. Geophysical Journal International, 184(1): 12-28. doi: 10.1111/gji.2010.184.issue-1
[36]	SPENCE W, 1986. The 1977 Sumba earthquake series: Evidence for Slab pull force acting at a subduction zone[J]. Journal of Geophysical Research: Solid Earth, 91(B7): 7225-7239.
[37]	VAN DER WERFF W, 1996. Variation in forearc basin development along the Sunda Arc, Indonesia[J]. Journal of Southeast Asian Earth Sciences, 14: 331-349. doi: 10.1016/S0743-9547(96)00068-2
[38]	VAN HUNEN J, VAN DEN BERG A P, VLAAR N J, 2002. On the role of subducting oceanic plateaus in the development of shallow flat subduction[J]. Tectonophysics, 352(3-4): 317-333. doi: 10.1016/S0040-1951(02)00263-9
[39]	WESSEL P, SMITH W H F, 1991. Free software helps map and display data[J]. Eos, Transactions American Geophysical Union, 72(41): 441-446.
[40]	XIA YUEYANG, KOPP H, KLAESCHEN D, et al, 2023. Seamount and ridge subduction at the Java margin, Indonesia: effects on structural geology and seismogenesis[J]. Journal of Geophysical Research: Solid Earth, 128(9): e2022JB026272.
[41]	XIA YUEYANG, GEERSEN J, KLAESCHEN D, et al, 2021. Marine forearc structure of eastern Java and its role in the 1994 Java tsunami earthquake[J]. Solid Earth, 12(11): 2467-2477. doi: 10.5194/se-12-2467-2021
[6]	BILEK S L, ENGDAHL E R, 2007. Rupture characterization and aftershock relocations for the 1994 and 2006 tsunami earthquakes in the Java subduction zone[J]. Geophysical Research Letters, 34(20): L20311.
[7]	DEMETS C, GORDON R G, ARGUS D F, 2010. Geologically current plate motions[J]. Geophysical Journal International, 181(1): 1-80. doi: 10.1111/gji.2010.181.issue-1
[8]	DICKINSON W R, 1977. Tectono-stratigraphic evolution of subduction-controlled sedimentary assemblages[M]//TALWANI M, PITMANN Ⅲ W C, Eds, Island Arcs, Deep Sea Trenches and Back-Arc Basins. Maurice Ewing Series 1. Washington, D. C.: American Geophysical Union:land Arcs, Deep Sea Trenches and Back-Arc Basins. Maurice Ewing Series 1. Washington, D. C.: American Geophysical Union: 33-40.
[9]	FONT Y, LALLEMAND S, 2009. Subducting oceanic high causes compressional faulting in southernmost Ryukyu forearc as revealed by hypocentral determinations of earthquakes and reflection/refraction seismic data[J]. Tectonophysics, 466(3-4): 255-267. doi: 10.1016/j.tecto.2007.11.018
[10]	HALL R, 2002. Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations[J]. Journal of Asian Earth Sciences, 20(4): 353-431. doi: 10.1016/S1367-9120(01)00069-4
[11]	HALL R, SMYTH H R, 2008. Cenozoic arc processes in Indonesia: identification of the key influences on the stratigraphic record in active volcanic arcs[M]//DRAUT A E, CLIFT P D, SCHOLL D W. Formation and applications of the sedimentary record in Arc Collision Zones. Boulder: Geological Society of America.
[12]	HAMILTON W B, 1979. Tectonics of the Indonesian Region[R]. Washington, D. C. : U. S. Government Publishing Office: 1078.
[13]	HAMILTON W B, 1988. Plate tectonics and island arcs[J]. GAS Bulletin, 100(10): 1503-1527.
[14]	HEINE C, MÜLLER R D, GAINA C, 2004. Reconstructing the lost eastern Tethys Ocean Basin: Convergence history of the SE Asian margin and marine gateways[M]//CLIFT P, KUHNT W, WANG P, et al. Continent-ocean interactions within East Asian marginal seas. Washington, D. C. : American Geophysical Union: 37-54.
[15]	HOERNLE K, HAUFF F, WERNER R, et al, 2011. Origin of Indian Ocean Seamount Province by shallow recycling of continental lithosphere[J]. Nature Geoscience, 4(12): 883-887. doi: 10.1038/ngeo1331
[16]	KODAIRA S, TAKAHASHI N, NAKANISHI A, et al, 2000. Subducted seamount imaged in the rupture zone of the 1946 Nankaido earthquake[J]. Science, 289(5476): 104-106. pmid: 10884221
[17]	KOPP H, 2011. The Java convergent margin: structure, seismogenesis and subduction processes[M]//HALL R, COTTAM M A; WILSON M E J. The SE Asian Gateway: history and tectonics of the Australia-Asia collision. London: Geological Society.
[18]	KOPP H, 2013. Invited review paper: The control of subduction zone structural complexity and geometry on margin segmentation and seismicity[J]. Tectonophysics, 589: 1-16. doi: 10.1016/j.tecto.2012.12.037
[19]	KOPP H, FLUEH E R, KLAESCHEN D, et al, 2001. Crustal structure of the central Sunda margin at the onset of oblique subduction[J]. Geophysical Journal International, 147(2): 449-474. doi: 10.1046/j.0956-540x.2001.01547.x
[20]	KOPP H, FLUEH E R, PETERSEN C J, et al, 2006. The Java margin revisited: Evidence for subduction erosion off Java[J]. Earth and Planetary Science Letters, 242(1-2): 130-142. doi: 10.1016/j.epsl.2005.11.036
[21]	KOPP H, HINDLE D, KLAESCHEN D, et al, 2009. Anatomy of the western Java plate interface from depth-migrated seismic images[J]. Earth and Planetary Science Letters, 288(3-4): 399-407. doi: 10.1016/j.epsl.2009.09.043
[22]	KOPP H, KUKOWSKI N, 2003. Backstop geometry and accretionary mechanics of the Sunda margin[J]. Tectonics, 22(6): 1072.
[23]	LÜSCHEN E, MÜLLER C, KOPP H, et al, 2011. Structure, evolution and tectonic activity of the eastern Sunda forearc, Indonesia, from marine seismic investigations[J]. Tectonophysics, 508(1-4): 6-21. doi: 10.1016/j.tecto.2010.06.008
[24]	MALOD J A, KARTA K, BESLIER M O, et al, 1995. From normal to oblique subduction: Tectonic relationships between Java and Sumatra[J]. Journal of Southeast Asian Earth Sciences, 12(1-2): 85-93. doi: 10.1016/0743-9547(95)00023-2
[25]	MARTÍNEZ-LORIENTE S, SALLARÈS V, RANERO C S, et al, 2019. Influence of incoming plate relief on overriding plate deformation and earthquake nucleation: Cocos ridge subduction (Costa Rica)[J]. Tectonics, 38(12): 4360-4377. doi: 10.1029/2019TC005586
[26]	MASSON D G, PARSON L M, MILSOM J, et al, 1990. Subduction of seamounts at the Java Trench: a view with long-range sidescan sonar[J]. Tectonophysics, 185(1-2): 51-65. doi: 10.1016/0040-1951(90)90404-V
[27]	MCNEILL L C, HENSTOCK T J, 2014. Forearc structure and morphology along the Sumatra-Andaman subduction zone[J]. Tectonics, 33(2): 112-134. doi: 10.1002/tect.v33.2
[28]	MOCHIZUKI K, YAMADA T, SHINOHARA M, et al, 2008. Weak interplate coupling by seamounts and repeating M - 7 earthquakes[J]. Science, 321(5893): 1194-1197. doi: 10.1126/science.1160250
[29]	MOORE G F, CURRAY J R, MOORE D G, et al, 1980. Variations in geologic structure along the Sunda fore Arc, Northeastern Indian Ocean[M]//HAYES D E. The tectonic and geologic evolution of Southeast Asian seas and islands. Washington, D. C. : American Geophysical Union, 23: 145-160.
[30]	MÜLLER C, BARCKHAUSEN U, EHRHARDT A, et al, 2008. From subduction to collision: the Sunda-Banda Arc transition[J]. Eos, Transactions American Geophysical Union, 89(6): 49-50. doi: 10.1029/2008EO060001
[31]	PLANERT L, KOPP H, LUESCHEN E, et al, 2010. Lower plate structure and upper plate deformational segmentation at the Sunda-Banda Arc transition, Indonesia[J]. Journal of Geophysical Research: Solid Earth, 115(B8): B08107.
[32]	RUH J B, SALLARÈS V, RANERO C R, et al, 2016. Crustal deformation dynamics and stress evolution during seamount subduction: High-resolution 3-D numerical modeling[J]. Journal of Geophysical Research: Solid Earth, 121(9): 6880-6902. doi: 10.1002/jgrb.v121.9

东印度洋爪哇板块边缘俯冲结构及其对地质灾害的影响

Subduction structure and its influence on geological hazards at the Java Plate margin in the eastern Indian Ocean

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