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Seismic properties of lawsonite eclogites from the southern Motagua fault zone, Guatemala

Cited 6 time in wos
Cited 8 time in scopus
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Seismic properties of lawsonite eclogites from the southern Motagua fault zone, Guatemala
Other Titles
과테말라 남 모타구아 전단대에서 채취한 로소나이트 에클로자이트의 지진파 특성
Kim, Daeyeong
Jin-Han Ree
Shunsuke Endo
Simonn Wallis
Crystal preferred orientation (CPO); Eclogite; Electron backscatter diffraction (EBSD); Lawsonite; Seismic anisotropy; Subducting oceanic crust
Issue Date
Kim, Daeyeong, et al. 2016. "Seismic properties of lawsonite eclogites from the southern Motagua fault zone, Guatemala". TECTONOPHYSICS, 677-678(677-678): 88-98.
We present new data on the crystal preferred orientation (CPO) and seismic properties of omphacite and lawsonite in extremely fresh eclogite from the southern Motagua fault zone, Guatemala, to discuss the seismic anisotropy of subducting oceanic crust. The CPO of omphacite is characterized by (010)[001], and it shows P-wave seismic anisotropies (AVP) of 1.4%?3.2% and S-wave seismic anisotropies (AVS) of 1.4%?2.7%. Lawsonite exhibits (001) planes parallel to the foliation and [010] axes parallel to the lineation, and seismic anisotropies of 1.7%?6.6% AVP and 3.4%?14.7% AVS. The seismic anisotropy of a rock mass consisting solely of omphacite and lawsonite is 1.2%?4.1% AVP and 1.8%?6.8% AVS. For events that propagate more or less parallel to the maximum extension direction, X, the fast S-wave velocity (VS) polarization is parallel to the Z in the Y?Z section (rotated from the X?Z section), causing trench-normal seismic anisotropy for orthogonal subduction. Based on the high modal abundance and strong fabric of lawsonite, the AVS of eclogites is estimated as ~ 11.7% in the case that lawsonite makes up ~ 75% of the rock mass. On this basis, we suggest that lawsonite in both blueschist and eclogite may play important roles in the formation of complex pattern of seismic anisotropy observed in NE Japan: weak trench-parallel anisotropy in the forearc basin domains and trench-normal anisotropy in the backarc region.
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