Heat flow measurements in the Northern Mozambique Channel

Heat flow in the Northern Mozambique Channel is poorly constrained, with only a few old measurements indicating relatively low values of 55–$62~\text{mW/m}^2$. During the SISMAORE cruise to the Northern Mozambique Channel, we obtained new heat flow measurements at four sites, using sediment corers e...

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Main Authors: Rolandone, Frédérique, Poort, Jeffrey, Masquelet, Charles, Leroy, Sylvie, Thinon, Isabelle, Lemoine, Anne, Paquet, Fabien
Format: Article
Language:English
Published: Académie des sciences 2022-12-01
Series:Comptes Rendus. Géoscience
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Online Access:https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.130/
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author Rolandone, Frédérique
Poort, Jeffrey
Masquelet, Charles
Leroy, Sylvie
Thinon, Isabelle
Lemoine, Anne
Paquet, Fabien
author_facet Rolandone, Frédérique
Poort, Jeffrey
Masquelet, Charles
Leroy, Sylvie
Thinon, Isabelle
Lemoine, Anne
Paquet, Fabien
author_sort Rolandone, Frédérique
collection DOAJ
description Heat flow in the Northern Mozambique Channel is poorly constrained, with only a few old measurements indicating relatively low values of 55–$62~\text{mW/m}^2$. During the SISMAORE cruise to the Northern Mozambique Channel, we obtained new heat flow measurements at four sites, using sediment corers equipped with thermal probes. Three of the sites yield values of 42–47 $\text{mW/m}^2$, confirming low regional heat flow in this area. Our values are consistent with a Jurassic oceanic lithosphere around Mayotte, although the presence of very thin continental crust or continental fragments could also explain the observed heat flow. Our values do not support a regional thermal anomaly and so do not favor a hotspot model for Mayotte. However, at a fourth site located 30 km east of the submarine volcano that appeared in 2018 east of Mayotte, we measured a very high heat flow value of $235~\text{mW/m}^2$, which we relate to the circulation of hot fluids linked to recent magmatic activity.
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issn 1778-7025
language English
publishDate 2022-12-01
publisher Académie des sciences
record_format Article
series Comptes Rendus. Géoscience
spelling doaj-art-bc9dfebec12f47a58897d74a2b71a3612025-08-20T02:08:46ZengAcadémie des sciencesComptes Rendus. Géoscience1778-70252022-12-01354S2354610.5802/crgeos.13010.5802/crgeos.130Heat flow measurements in the Northern Mozambique ChannelRolandone, Frédérique0https://orcid.org/0000-0001-5339-4275Poort, Jeffrey1https://orcid.org/0000-0001-5964-9697Masquelet, Charles2Leroy, Sylvie3https://orcid.org/0000-0002-3188-8802Thinon, Isabelle4https://orcid.org/0000-0001-8358-2699Lemoine, Anne5https://orcid.org/0000-0002-2545-0193Paquet, Fabien6https://orcid.org/0000-0002-8803-7312Sorbonne Université, CNRS, Institut des Sciences de la Terre de Paris (ISTeP), Paris, FranceSorbonne Université, CNRS, Institut des Sciences de la Terre de Paris (ISTeP), Paris, FranceSorbonne Université, CNRS, Institut des Sciences de la Terre de Paris (ISTeP), Paris, FranceSorbonne Université, CNRS, Institut des Sciences de la Terre de Paris (ISTeP), Paris, FranceBureau de Recherches Géologiques et Minières (BRGM), Orléans, FranceBureau de Recherches Géologiques et Minières (BRGM), Orléans, FranceBureau de Recherches Géologiques et Minières (BRGM), Orléans, FranceHeat flow in the Northern Mozambique Channel is poorly constrained, with only a few old measurements indicating relatively low values of 55–$62~\text{mW/m}^2$. During the SISMAORE cruise to the Northern Mozambique Channel, we obtained new heat flow measurements at four sites, using sediment corers equipped with thermal probes. Three of the sites yield values of 42–47 $\text{mW/m}^2$, confirming low regional heat flow in this area. Our values are consistent with a Jurassic oceanic lithosphere around Mayotte, although the presence of very thin continental crust or continental fragments could also explain the observed heat flow. Our values do not support a regional thermal anomaly and so do not favor a hotspot model for Mayotte. However, at a fourth site located 30 km east of the submarine volcano that appeared in 2018 east of Mayotte, we measured a very high heat flow value of $235~\text{mW/m}^2$, which we relate to the circulation of hot fluids linked to recent magmatic activity.https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.130/Heat flowOceanic lithosphereVolcanismNorthern Mozambique ChannelComoros archipelago2018–2021 Mayotte eruption
spellingShingle Rolandone, Frédérique
Poort, Jeffrey
Masquelet, Charles
Leroy, Sylvie
Thinon, Isabelle
Lemoine, Anne
Paquet, Fabien
Heat flow measurements in the Northern Mozambique Channel
Comptes Rendus. Géoscience
Heat flow
Oceanic lithosphere
Volcanism
Northern Mozambique Channel
Comoros archipelago
2018–2021 Mayotte eruption
title Heat flow measurements in the Northern Mozambique Channel
title_full Heat flow measurements in the Northern Mozambique Channel
title_fullStr Heat flow measurements in the Northern Mozambique Channel
title_full_unstemmed Heat flow measurements in the Northern Mozambique Channel
title_short Heat flow measurements in the Northern Mozambique Channel
title_sort heat flow measurements in the northern mozambique channel
topic Heat flow
Oceanic lithosphere
Volcanism
Northern Mozambique Channel
Comoros archipelago
2018–2021 Mayotte eruption
url https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.130/
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