An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys

An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys

In ultraslow-spreading ridges intermittent detachment faulting could contribute to discontinuous magmatic accretion supporting the development of massive sulfide deposits. Here the authors using a multi-scale magnetic survey of the Southwest Indian Ridge constrain that an episode of detachment fault...

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Autores principales: Tao Wu, Maurice A. Tivey, Chunhui Tao, Jinhui Zhang, Fei Zhou, Yunlong Liu
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/35b1f94ad43841ee8a6ed0715db91146
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spelling oai:doaj.org-article:35b1f94ad43841ee8a6ed0715db911462021-12-02T15:15:05ZAn intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys10.1038/s41467-021-25880-12041-1723https://doaj.org/article/35b1f94ad43841ee8a6ed0715db911462021-09-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-25880-1https://doaj.org/toc/2041-1723In ultraslow-spreading ridges intermittent detachment faulting could contribute to discontinuous magmatic accretion supporting the development of massive sulfide deposits. Here the authors using a multi-scale magnetic survey of the Southwest Indian Ridge constrain that an episode of detachment faulting took place 0.7-1.48 Ma, with the present fault active since 0.33 Ma.Tao WuMaurice A. TiveyChunhui TaoJinhui ZhangFei ZhouYunlong LiuNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-10 (2021)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Tao Wu
Maurice A. Tivey
Chunhui Tao
Jinhui Zhang
Fei Zhou
Yunlong Liu
An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
description In ultraslow-spreading ridges intermittent detachment faulting could contribute to discontinuous magmatic accretion supporting the development of massive sulfide deposits. Here the authors using a multi-scale magnetic survey of the Southwest Indian Ridge constrain that an episode of detachment faulting took place 0.7-1.48 Ma, with the present fault active since 0.33 Ma.
format article
author Tao Wu
Maurice A. Tivey
Chunhui Tao
Jinhui Zhang
Fei Zhou
Yunlong Liu
author_facet Tao Wu
Maurice A. Tivey
Chunhui Tao
Jinhui Zhang
Fei Zhou
Yunlong Liu
author_sort Tao Wu
title An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
title_short An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
title_full An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
title_fullStr An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
title_full_unstemmed An intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
title_sort intermittent detachment faulting system with a large sulfide deposit revealed by multi-scale magnetic surveys
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/35b1f94ad43841ee8a6ed0715db91146
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