Crustal structure and variation along the southern part of the Kyushu-Palau Ridge  

作　　者：Xiaodong Wei Weiwei Ding Aiguo Ruan Jie Zhang Xiongwei Niu Jiabiao Li Yong Tang 

机构地区：[1]Key Laboratory of Submarine Geosciences,Ministry of Natural Resources/Second Institute of Oceanography,Ministry of Natural Resources,Hangzhou 310012,China [2]Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai),Zhuhai 519080,China [3]School of Oceanography,Shanghai Jiao Tong University,Shanghai 200240,China

出　　处：《Acta Oceanologica Sinica》2022年第1期50-57,共8页海洋学报（英文版）

基　　金：The Scientific Research Fund of the Second Institute of Oceanography;MNR under contract No.QNYC1801;the National Natural Science Foundation of China under contract Nos 91858214,41776053,42025601,42076047,41890811 and 42006072;the National Program on Global Change and Air-Sea Interaction;Ministry of Natural Resources under contract No.GASI-02-PACDWZP02;the Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai)under contract No.311020018。

摘　　要：As an interoceanic arc,the Kyushu-Palau Ridge(KPR)is an exceptional place to study the subduction process and related magmatism through its interior velocity structure.However,the crustal structure and its nature of the KPR,especially the southern part with limited seismic data,are still in mystery.In order to unveil the crustal structure of the southern part of the KPR,this study uses deep reflection/refraction seismic data recorded by 24 ocean bottom seismometers to reconstruct a detailed P-wave velocity model along the ridge.Results show strong alongridge variations either on the crustal velocity or the thickness of the KPR.P-wave velocity model is featured with(1)a crustal thickness between 6–12 km,with velocity increases from 4.0 km/s to 7.0 km/s from top to bottom;(2)high gradient(~1 s^(-1))in the upper crust but low one(<0.2 s^(-1))in the lower crust;(3)a slow mantle velocity between 7.2 km/s and 7.6 km/s in the uppermost mantle;and(4)inhomogenous velocity anomalies in the lower crust beneath seamounts.By comparing with the mature arc in the Izu-Bonin-Mariana arc in the east,this study suggests the southern part of KPR is a thicken oceanic crust rather than a typical arc crust.The origin of low velocities in the lower crust and upper mantle may be related with crustal differentiation,which implies advanced crustal evolution from normal oceanic crust to partly thicken oceanic crust.High velocities in the lower crust are related to the difference in magmatism.

关 键 词：P-WAVE velocity structure ocean bottom SEISMOMETER Kyushu-Palau RIDGE MAGMATISM thicken oceanic crust 

分 类 号：P736.1[天文地球—海洋地质]