Recent tectonics of the Blanco Ridge, eastern blanco transform fault zone

@article{Dziak2000RecentTO,
  title={Recent tectonics of the Blanco Ridge, eastern blanco transform fault zone},
  author={R. Dziak and C. Fox and R. Embley and J. N{\'a}bělek and J. Braunmiller and R. Koski},
  journal={Marine Geophysical Researches},
  year={2000},
  volume={21},
  pages={423-450}
}
Bathymetric, hydro-acoustic, seismic, submersible, and gravity data are used to investigate the active tectonics of the eastern Blanco Transform Fault Zone (BTFZ). The eastern BTFZ is dominated by the ∼150 km long transform-parallel Blanco Ridge (BR) which is a right-lateral strike-slip fault bordered to the east and west by the Gorda and Cascadia Depressions. Acoustic locations, fault-parameter information, and slip vector estimates of 43 earthquakes (Mw≥3.8) that occurred along the eastern… Expand
Defining static correction for jointly relocated earthquakes along the Blanco Transform Fault Zone based on SOSUS hydrophone data
  • V. Cronin, K. A. Sverdrup
  • Geology
  • Oceans 2003. Celebrating the Past ... Teaming Toward the Future (IEEE Cat. No.03CH37492)
  • 2003
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