Lithospheric mantle anisotropy from local events beneath the Sunda–Banda arc transition and its geodynamic implications

Acta Geophysica

article

Syuhada, Syuhada¹  Hananto, Nugroho D.²  Abdullah, Chalid I.³  Puspito, Nanang T.⁴  Anggono, Titi¹  Febriani, Febty¹  Soedjatmiko, Bogie¹ 

[1] Research Centre for Physics, Indonesian Institute of Sciences (LIPI);Research Centre for Deep Sea-LIPI;Faculty of Earth Sciences and Technology, Bandung Institute of Technology;Faculty of Mining and Petroleum Engineering, Bandung Institute of Technology

关键词: Shear wave splitting;    Seismic anisotropy;    Mantle flow;    Sunda–Banda arc transition zone;   

DOI  :  10.1007/s11600-020-00486-1

学科分类：地球科学(综合)

来源: Polska Akademia Nauk * Instytut Geofizyki

【 摘 要 】

Shear wave splitting analysis to characterise lithospheric mantle anisotropy has been performed to provide better knowledge about lithospheric deformation and mantle flow beneath the Sunda–Banda arc transition, Indonesia. The tectonic setting of the study area is very complex characterised by the transition from subduction along Sunda arc to collision in Banda arc. The splitting measurements show lateral and vertical variation in the fast directions of the S-waves in this region. When the splitting results are analysed through 2D delay-time tomography and spatial averaging, systematic patterns in delay times and fast polarisation become more visible. In the subduction domain, the spatial averages of fast directions are dominated by two distinct fast polarisations: perpendicular and parallel to the plate motion for shallow and deep events, respectively. The results suggest that anisotropy in this area is not only controlled by anisotropic source related to the simple mantle flow model, but also by anisotropic fabric in the mantle deformed under influence of high stresses, high water contents and low temperatures. In addition, there might also be contribution from the anisotropic body in the upper layer. In the collision domain, spatially averaged fast directions show mostly perpendicular to the plate motion for all deep levels. For shallow level in this region, this trend is mainly governed by the lithospheric deformation process due to the continent-arc collision as also shown by delay time tomographic inversion. For deeper part of the region, the result of tomographic inversion and spatial averaging reveals a high anisotropy followed by rotational pattern of fast directions in the north of Timor. We suggest that this pattern might be related to the induced mantle flow due to lateral tearing of the slab.

【 授权许可】

Unknown