Thermal structures of the Pacific lithosphere from magnetic anomaly inversion

Of the world's oceans, the Pacific has the most abundant distribution of seamount trails, oceanic plateaus and hot spots, and has the longest fracture zones. However, little is known of their thermal structures due to difficulties of heat flow measurement and interpretation, and in inferring th...

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Published in:Earth and Planetary Physics
Main Authors: Chun-Feng Li, Jian Wang
Format: Article in Journal/Newspaper
Language:English
Published: Science Press 2018
Subjects:
geo
Online Access:https://doi.org/10.26464/epp2018005
https://doaj.org/article/17949f8fa1114fcf870b2e46a33e9b88
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:17949f8fa1114fcf870b2e46a33e9b88 2023-05-15T17:31:05+02:00 Thermal structures of the Pacific lithosphere from magnetic anomaly inversion Chun-Feng Li Jian Wang 2018-01-01 https://doi.org/10.26464/epp2018005 https://doaj.org/article/17949f8fa1114fcf870b2e46a33e9b88 en eng Science Press 2096-3955 doi:10.26464/epp2018005 https://doaj.org/article/17949f8fa1114fcf870b2e46a33e9b88 undefined Earth and Planetary Physics, Vol 2, Iss 1, Pp 52-66 (2018) pacific curie depth heat flow seamount oceanic plateau magnetic anomaly geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.26464/epp2018005 2023-01-22T19:26:14Z Of the world's oceans, the Pacific has the most abundant distribution of seamount trails, oceanic plateaus and hot spots, and has the longest fracture zones. However, little is known of their thermal structures due to difficulties of heat flow measurement and interpretation, and in inferring thermal anomalies from low-resolution seismic velocities. Using recently published global magnetic models, we present the first independent constraint on Pacific geothermal state and mantle dynamics, by applying a fractal magnetization inversion model to magnetic anomaly data. Warm thermal anomalies are inferred for all known active hot spots, most seamount trails, some major fracture zones, and oceanic lithosphere between ~100 and ~140 Ma in age. While most Curie points are among the shallowest in the zone roughly bounded by the 20 Ma isochrons, abnormally deep Curie points are found along nearly all ridge crests in the Pacific, related to patchy, long-wavelength and large-amplitude magnetic anomalies that are most likely caused by prevailing magmatic or hydrothermal processes. Many large contrasts in the thermal evolution between the Pacific and North Atlantic support much stronger hydrothermal circulation occurring in Pacific lithospheres younger than ~60 Ma, which may have disguised from surface heat flow any deep thermal signatures of volcanic structures. Yet, at depths of the Curie points, our model argues for warmer Pacific lithosphere for crustal ages older than ~15 Ma, given a slightly higher spatial correlation of magnetization in the Pacific than in the North Atlantic. Article in Journal/Newspaper North Atlantic Unknown Pacific Earth and Planetary Physics 2 1 1 15
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic pacific
curie depth
heat flow
seamount
oceanic plateau
magnetic anomaly
geo
envir
spellingShingle pacific
curie depth
heat flow
seamount
oceanic plateau
magnetic anomaly
geo
envir
Chun-Feng Li
Jian Wang
Thermal structures of the Pacific lithosphere from magnetic anomaly inversion
topic_facet pacific
curie depth
heat flow
seamount
oceanic plateau
magnetic anomaly
geo
envir
description Of the world's oceans, the Pacific has the most abundant distribution of seamount trails, oceanic plateaus and hot spots, and has the longest fracture zones. However, little is known of their thermal structures due to difficulties of heat flow measurement and interpretation, and in inferring thermal anomalies from low-resolution seismic velocities. Using recently published global magnetic models, we present the first independent constraint on Pacific geothermal state and mantle dynamics, by applying a fractal magnetization inversion model to magnetic anomaly data. Warm thermal anomalies are inferred for all known active hot spots, most seamount trails, some major fracture zones, and oceanic lithosphere between ~100 and ~140 Ma in age. While most Curie points are among the shallowest in the zone roughly bounded by the 20 Ma isochrons, abnormally deep Curie points are found along nearly all ridge crests in the Pacific, related to patchy, long-wavelength and large-amplitude magnetic anomalies that are most likely caused by prevailing magmatic or hydrothermal processes. Many large contrasts in the thermal evolution between the Pacific and North Atlantic support much stronger hydrothermal circulation occurring in Pacific lithospheres younger than ~60 Ma, which may have disguised from surface heat flow any deep thermal signatures of volcanic structures. Yet, at depths of the Curie points, our model argues for warmer Pacific lithosphere for crustal ages older than ~15 Ma, given a slightly higher spatial correlation of magnetization in the Pacific than in the North Atlantic.
format Article in Journal/Newspaper
author Chun-Feng Li
Jian Wang
author_facet Chun-Feng Li
Jian Wang
author_sort Chun-Feng Li
title Thermal structures of the Pacific lithosphere from magnetic anomaly inversion
title_short Thermal structures of the Pacific lithosphere from magnetic anomaly inversion
title_full Thermal structures of the Pacific lithosphere from magnetic anomaly inversion
title_fullStr Thermal structures of the Pacific lithosphere from magnetic anomaly inversion
title_full_unstemmed Thermal structures of the Pacific lithosphere from magnetic anomaly inversion
title_sort thermal structures of the pacific lithosphere from magnetic anomaly inversion
publisher Science Press
publishDate 2018
url https://doi.org/10.26464/epp2018005
https://doaj.org/article/17949f8fa1114fcf870b2e46a33e9b88
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_source Earth and Planetary Physics, Vol 2, Iss 1, Pp 52-66 (2018)
op_relation 2096-3955
doi:10.26464/epp2018005
https://doaj.org/article/17949f8fa1114fcf870b2e46a33e9b88
op_rights undefined
op_doi https://doi.org/10.26464/epp2018005
container_title Earth and Planetary Physics
container_volume 2
container_issue 1
container_start_page 1
op_container_end_page 15
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