The Ulakhan fault surface rupture and the seismicity of the Okhotsk–North America plate boundary
<p>New field work, combined with analysis of high-resolution aerial photographs, digital elevation models, and satellite imagery, has identified an active fault that is traceable for <span class="inline-formula">∼90</span> km across the Seymchan Basin and is pa...
Main Authors: | D. Hindle, B. Sedov, S. Lindauer, K. Mackey |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2019-04-01
|
Series: | Solid Earth |
Online Access: | https://www.solid-earth.net/10/561/2019/se-10-561-2019.pdf |
Similar Items
-
Rock glaciers in the Ulakhan-Chistay ridge (axial part of the Chersky mountain range)
by: V. M. Lytkin, et al.
Published: (2019-12-01) -
Deformation mechanisms along active strike-slip faults : SeaMARC II and seismic data from the North America-Caribbean plate boundary
by: Tyburski, Stacey Ann
Published: (2015) -
Tidally modified western boundary current drives interbasin exchange between the Sea of Okhotsk and the North Pacific
by: Hung-Wei Shu, et al.
Published: (2021-06-01) -
Measuring Low Fault Strain Rate with Synthetic Aperture Radar: Application to the Pacific-North America Plate Boundary
by: Gourmelen, Noel
Published: (2009) -
NEOTECTONICS OF THE SEA OF OKHOTSK
by: V. P. Semakin, et al.
Published: (2016-06-01)