The Mackenzie Mountains Transect: Active Deformation from Margin to Craton

The Mackenzie Mountains Experiment aims to understand the reason mountains are forming 500 miles inland from the nearest plate boundary, while little deformation occurs closer to the boundary. This experiment will extend nearly from the plate boundary to the stable Canadian craton in a transect that...

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Bibliographic Details
Main Authors: Derek Schutt, Rick Aster
Format: Article in Journal/Newspaper
Language:unknown
Published: International Federation of Digital Seismograph Networks 2015
Subjects:
Canada
Mackenzie mountains
Online Access:https://dx.doi.org/10.7914/sn/7c_2015
https://www.fdsn.org/networks/detail/7C_2015/
id ftdatacite:10.7914/sn/7c_2015
record_format openpolar
spelling ftdatacite:10.7914/sn/7c_2015 2023-05-15T17:09:31+02:00 The Mackenzie Mountains Transect: Active Deformation from Margin to Craton Derek Schutt Rick Aster 2015 SEED data https://dx.doi.org/10.7914/sn/7c_2015 https://www.fdsn.org/networks/detail/7C_2015/ unknown International Federation of Digital Seismograph Networks Other CreativeWork article Seismic Network 2015 ftdatacite https://doi.org/10.7914/sn/7c_2015 2021-11-05T12:55:41Z The Mackenzie Mountains Experiment aims to understand the reason mountains are forming 500 miles inland from the nearest plate boundary, while little deformation occurs closer to the boundary. This experiment will extend nearly from the plate boundary to the stable Canadian craton in a transect that extends 500 miles through Northwest Canada Article in Journal/Newspaper Mackenzie mountains DataCite Metadata Store (German National Library of Science and Technology) Canada
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description The Mackenzie Mountains Experiment aims to understand the reason mountains are forming 500 miles inland from the nearest plate boundary, while little deformation occurs closer to the boundary. This experiment will extend nearly from the plate boundary to the stable Canadian craton in a transect that extends 500 miles through Northwest Canada
format Article in Journal/Newspaper
author Derek Schutt
Rick Aster
spellingShingle Derek Schutt
Rick Aster
The Mackenzie Mountains Transect: Active Deformation from Margin to Craton
author_facet Derek Schutt
Rick Aster
author_sort Derek Schutt
title The Mackenzie Mountains Transect: Active Deformation from Margin to Craton
title_short The Mackenzie Mountains Transect: Active Deformation from Margin to Craton
title_full The Mackenzie Mountains Transect: Active Deformation from Margin to Craton
title_fullStr The Mackenzie Mountains Transect: Active Deformation from Margin to Craton
title_full_unstemmed The Mackenzie Mountains Transect: Active Deformation from Margin to Craton
title_sort mackenzie mountains transect: active deformation from margin to craton
publisher International Federation of Digital Seismograph Networks
publishDate 2015
url https://dx.doi.org/10.7914/sn/7c_2015
https://www.fdsn.org/networks/detail/7C_2015/
geographic Canada
geographic_facet Canada
genre Mackenzie mountains
genre_facet Mackenzie mountains
op_doi https://doi.org/10.7914/sn/7c_2015
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