气候变化领域集成服务门户(CCPortal): Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging

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DOI	10.1016/j.tecto.2021.229005
	Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging
	Leydier T.; Goncalves P.; Albaric J.; Leclère H.; Mahan K.H.; Faulkner D.
发表日期	2021
ISSN	00401951
卷号	816
英文摘要	Detecting the presence and geometry of crustal shear zones by geophysical methods relies on our understanding of the intrinsic parameters controlling the seismic properties of these deformed rocks, over the range of pressure-temperature conditions expected in the Earth's crust. To this end, we aimed to track changes in P-wave propagation velocity (VP), anisotropy (AVP) and S-wave splitting (AVS) across a natural shear zone using experimental and electron backscatter diffraction methods. Five samples were collected across a meter-scale shear zone developed under amphibolite- to greenschist-facies in the Neves metagranodiorite (Tauern Window, Eastern Alps). With increasing strain, seismic properties show a non-linear evolution resulting from interactions among structural, textural and mineralogical changes. Geometry and magnitude of seismic anisotropy are controlled by the interference of strongly anisotropic phyllosilicates with less anisotropic but more abundant quartz and plagioclase. The amphibolite-facies shear zone margin (> 500 °C) is free of major mineral transformations, and rather characterized by the development of S-C structure, inducing an orthorhombic symmetry to the VP distribution and up to 12 % AVP, with the fast axis parallel to lineation. AVS is maximized (6 %) in the two directions parallel to the C-planes. Further deformation under greenschist-facies (450–500 °C) induces significant crystallization of muscovite, chlorite, and albite. A dominant hexagonal symmetry develops, with a fast VP plane and a fast S-wave polarization plane along the C-planes. AVP and AVS exceed 10 %. The computed elastic tensor of the whole shear zone emphasizes the importance of the strain gradient on the seismic signature of the overall structure. In our model, the bulk seismic properties are dominated by the orthorhombic symmetry of the protomylonitic zone rather than by the ultramylonite core with hexagonal symmetry (C-plane), which may explain why seismic studies of shear zones commonly involve a fast velocity plane oblique to the layer boundaries. © 2021
关键词	EBSD Seismic anisotropy Shear zone Ultrasonic measurements
英文关键词	Anisotropy; Feldspar; Mica; Seismic prospecting; Seismic waves; Seismology; Shear waves; Silicates; Structural geology; Wave propagation; Electron backscatter diffraction methods; Further deformations; Intrinsic parameters; Mineral transformations; Mineralogical changes; Nonlinear evolutions; Orthorhombic symmetry; Pressure-temperature conditions; Shear flow; amphibolite facies; greenschist facies; P-wave; S-wave; seismic anisotropy; seismic property; seismic velocity; shear zone; strain analysis; wave propagation; wave splitting; Alps; Eastern Alps; Italy
语种	英语
来源期刊	Tectonophysics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/208003
作者单位	Université de Bourgogne Franche-Comté, UMR-CNRS 6249 Laboratoire Chrono-Environnement, 16 route de Gray, Besancon, 25000, France; Department of Geological Sciences, University of Colorado Boulder, 2200 Colorado Ave, Boulder, CO 80309, United States; Department of Earth and Ocean Sciences, University of Liverpool, 4 Brownlow Street, Liverpool, L69 3GP, United Kingdom
推荐引用方式 GB/T 7714	Leydier T.,Goncalves P.,Albaric J.,et al. Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging[J],2021,816.
APA	Leydier T.,Goncalves P.,Albaric J.,Leclère H.,Mahan K.H.,&Faulkner D..(2021).Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging.Tectonophysics,816.
MLA	Leydier T.,et al."Seismic properties across an amphibolite- to greenschist-facies strain gradient (Neves area, eastern Alps, Italy): New considerations for shear zone imaging".Tectonophysics 816(2021).