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Volumn 319, Issue 5861, 2008, Pages 315-318

The subduction zone flow field from seismic anisotropy: A global view

Author keywords

[No Author keywords available]

Indexed keywords

CONVERGENCE; FLOW FIELD; GEOMORPHOLOGY; MANTLE; S-WAVE; SEISMIC ANISOTROPY; SLAB; SUBDUCTION ZONE; VELOCITY;

EID: 38349153612     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1150809     Document Type: Article
Times cited : (330)

References (30)
  • 12
    • 0035957686 scopus 로고    scopus 로고
    • G. P. Smith et al., Science 292, 713 (2001).
    • (2001) Science , vol.292 , pp. 713
    • Smith, G.P.1
  • 25
    • 38349138026 scopus 로고    scopus 로고
    • Although the transition described here is more common, trench-perpendicular to trench-parallel transitions in φ have also been observed, for example, in Kamchatka and Alaska. These backward transitions are not easily explained by our model; however, because both Kamchatka and Alaska are located near slab edges, local processes may affect these regions
    • Although the transition described here is more common, trench-perpendicular to trench-parallel transitions in φ have also been observed, for example, in Kamchatka and Alaska. These backward transitions are not easily explained by our model; however, because both Kamchatka and Alaska are located near slab edges, local processes may affect these regions.
  • 30
    • 38349096791 scopus 로고    scopus 로고
    • We thank the Alaska Regional Network, Alaska Tsunami Warning Seismic System, the Pacific Orient Seismic Digital Observation Network POSEIDON, and the Incorporated Research Institutions for Seismology/United States Geological Survey for providing data used in this study. We thank M. Behn and S. Pozgay for useful discussions and L. Wagner for assistance with figures
    • We thank the Alaska Regional Network, Alaska Tsunami Warning Seismic System, the Pacific Orient Seismic Digital Observation Network (POSEIDON), and the Incorporated Research Institutions for Seismology/United States Geological Survey for providing data used in this study. We thank M. Behn and S. Pozgay for useful discussions and L. Wagner for assistance with figures.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.