Strain Signatures of Fjord Sediment Sliding: Micro-Scale Examples from Yakutat Bay and Glacier Bay, Alaska, U.S.A.

John F. Hiemstra; Kamil Zaniewski; Ross D. Powell; Ellen A. Cowan

doi:10.1306/040504740760

Strain Signatures of Fjord Sediment Sliding: Micro-Scale Examples from Yakutat Bay and Glacier Bay, Alaska, U.S.A.

John F. Hiemstra
, Kamil Zaniewski
, Ross D. Powell
, Ellen A. Cowan

Appalachian State University

Research output: Contribution to journal › Article › peer-review

Original language	American English
Journal	Journal of Sedimentary Research
Volume	74
DOIs	https://doi.org/10.1306/040504740760
State	Published - Nov 1 2004

Disciplines

Geology
Geomorphology

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10.1306/040504740760License: Unspecified

Cite this

@article{353ac3ffec11421391e4bf1a3d670a6e,

title = "Strain Signatures of Fjord Sediment Sliding: Micro-Scale Examples from Yakutat Bay and Glacier Bay, Alaska, U.S.A.",

author = "Hiemstra, \{John F.\} and Kamil Zaniewski and Powell, \{Ross D.\} and Cowan, \{Ellen A.\}",

note = "Narrow zones in many of the fine-grained core intervals show subtle patterns of preferred clay-mineral orientations (plasmic fabrics). We interpret these intervals as being low-strain simple shear zones. They all show a consistent and regular internal configuration that is formed by sets of conjugate shear planes.",

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AU - Hiemstra, John F.

AU - Zaniewski, Kamil

AU - Powell, Ross D.

AU - Cowan, Ellen A.

N1 - Narrow zones in many of the fine-grained core intervals show subtle patterns of preferred clay-mineral orientations (plasmic fabrics). We interpret these intervals as being low-strain simple shear zones. They all show a consistent and regular internal configuration that is formed by sets of conjugate shear planes.

PY - 2004/11/1

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