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深部俯冲板片三维构造重建及其几何学、运动学研究——以汤加—克马德克地区俯冲板片为例; Deep subducting slab reconstruction and its geometry, kinematics : a case study for the Tonga-Kermadec slab from tomography
鲁人齐 ; 何登发 ; 刘波 ; 陈于高
刊名地球物理学报
2013
关键词地震层析成像 俯冲板片 三维构造模型 几何学、运动学 汤加—克马德克地区 Seismic tomography Subducting slab 3-D Structural model Geometry and Kinematics Tonga-Kermadec
DOI10.6038/cjg20131125
英文摘要西南太平洋板块与澳大利亚板块之间的汤加—克马德克俯冲带,是研究地球动力学最重要的区域之一.本文研究根据MIT-P08地震数据,结合板块构造边界、地震活动分布、海岸地形数据等,基于GOCAD软件平台建立三维地震层析成像,对西南太平洋板块的汤加—克马德克俯冲板片进行三维解释.地震层析成像显示汤加—斐济地区地幔至少存在三个"高速"异常体.早期汤加—克马德克俯冲板片穿过地幔转换带,并进入下地幔,最大深度达1600km.三维构造模型揭示了汤加—克马德克板片在深度600~800km处存在断折形变,该俯冲板片去褶皱恢复后,测量其俯冲的最大位移达2600km.汤加—克马德克板片开始快速俯冲的时间至少在30Ma...; The Tonga-Kermadec subdction zone between the southwest Pacific Plate and the Australian Plate is one of the key regions to the Geodynamics research. In this paper, in order to map the 3-D geometries of subducting slabs, the MIT-P08 seismic tomography dataset have been add to the GOCAD software by integrating with tectonic boundaries, earthquakes and coastlines. The tomography shows there are three anomalously fast regions in the mantle beneath the Tonga-Fiji area. The Tonga-kermadec slab have subducted into the mantle transition zone and penetrated into the lower mantle. The maximum subducted depth is about 1600 km. 3-D structural model reveals the Tonga-kemadec slab is faulting and folding at 600 similar to 800 km depth. After the subducting slab is unfolding and restoration, measuring its maximum subducted displacement nearly 2600 km. The results indicate that the Tonga-kemadec slab subducted before 30Ma at least with the average rates of 68 similar to 104 mm/a. Reconstruction and recovery of the 3-D slab can reveal the detailed geometry and the kinematics of subducting slab, which is providing the constraints to the deep earthquakes, the deep earth processes and dynamic mechanism.; http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000327753000025&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 ; SCI(E); EI; 中文核心期刊要目总览(PKU); 中国科技核心期刊(ISTIC); 中国科学引文数据库(CSCD); 1; 11; 3837-3845; 56
语种中文
内容类型期刊论文
源URL[http://ir.pku.edu.cn/handle/20.500.11897/49173]  
专题地球与空间科学学院
推荐引用方式
GB/T 7714
鲁人齐,何登发,刘波,等. 深部俯冲板片三维构造重建及其几何学、运动学研究——以汤加—克马德克地区俯冲板片为例, Deep subducting slab reconstruction and its geometry, kinematics : a case study for the Tonga-Kermadec slab from tomography[J]. 地球物理学报,2013.
APA 鲁人齐,何登发,刘波,&陈于高.(2013).深部俯冲板片三维构造重建及其几何学、运动学研究——以汤加—克马德克地区俯冲板片为例.地球物理学报.
MLA 鲁人齐,et al."深部俯冲板片三维构造重建及其几何学、运动学研究——以汤加—克马德克地区俯冲板片为例".地球物理学报 (2013).
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