Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite
It is thought that Atlantic style passive margins have experienced episodes of uplift and volcanism in response to changes in mantle circulation. The authors here employ U-Pb dating of calcite in faults and fractures along the eastern North American margin and find a 40 Myr long period of fracturing...
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Nature Portfolio
2022-04-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-022-29680-z |
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author | William H. Amidon Andrew R. C. Kylander-Clark Matthew N. Barr Samuel F. I. Graf David P. West |
author_facet | William H. Amidon Andrew R. C. Kylander-Clark Matthew N. Barr Samuel F. I. Graf David P. West |
author_sort | William H. Amidon |
collection | DOAJ |
description | It is thought that Atlantic style passive margins have experienced episodes of uplift and volcanism in response to changes in mantle circulation. The authors here employ U-Pb dating of calcite in faults and fractures along the eastern North American margin and find a 40 Myr long period of fracturing and faulting from 115 to 75 Ma. |
first_indexed | 2024-04-14T01:03:07Z |
format | Article |
id | doaj.art-2540ff1c164b4619a4e7537e0421740b |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-04-14T01:03:07Z |
publishDate | 2022-04-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
spelling | doaj.art-2540ff1c164b4619a4e7537e0421740b2022-12-22T02:21:19ZengNature PortfolioNature Communications2041-17232022-04-011311710.1038/s41467-022-29680-zPace of passive margin tectonism revealed by U-Pb dating of fracture-filling calciteWilliam H. Amidon0Andrew R. C. Kylander-Clark1Matthew N. Barr2Samuel F. I. Graf3David P. West4Geology Department, Middlebury CollegeEarth Science Department, UC Santa BarbaraGeology Department, Middlebury CollegeGeology Department, Middlebury CollegeGeology Department, Middlebury CollegeIt is thought that Atlantic style passive margins have experienced episodes of uplift and volcanism in response to changes in mantle circulation. The authors here employ U-Pb dating of calcite in faults and fractures along the eastern North American margin and find a 40 Myr long period of fracturing and faulting from 115 to 75 Ma.https://doi.org/10.1038/s41467-022-29680-z |
spellingShingle | William H. Amidon Andrew R. C. Kylander-Clark Matthew N. Barr Samuel F. I. Graf David P. West Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite Nature Communications |
title | Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite |
title_full | Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite |
title_fullStr | Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite |
title_full_unstemmed | Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite |
title_short | Pace of passive margin tectonism revealed by U-Pb dating of fracture-filling calcite |
title_sort | pace of passive margin tectonism revealed by u pb dating of fracture filling calcite |
url | https://doi.org/10.1038/s41467-022-29680-z |
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