The dominant driving force for supercontinent breakup: Plume push or subduction retreat?

Understanding the dominant force responsible for supercontinent breakup is crucial for establishing Earth's geodynamic evolution that includes supercontinent cycles and plate tectonics. Conventionally, two forces have been considered: the push by mantle plumes from the sub-continental mantle wh...

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Main Authors: Nan Zhang, Zhuo Dang, Chuan Huang, Zheng-Xiang Li
Format: Article
Language:English
Published: Elsevier 2018-07-01
Series:Geoscience Frontiers
Online Access:http://www.sciencedirect.com/science/article/pii/S167498711830046X
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spelling doaj-655f11beffb44360acdfdfee6da892862020-11-25T01:01:56ZengElsevierGeoscience Frontiers1674-98712018-07-01949971007The dominant driving force for supercontinent breakup: Plume push or subduction retreat?Nan Zhang0Zhuo Dang1Chuan Huang2Zheng-Xiang Li3Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China; Earth Dynamics Research Group, ARC Center of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, AustraliaKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, ChinaKey Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China; Corresponding author.Earth Dynamics Research Group, ARC Center of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR), School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, AustraliaUnderstanding the dominant force responsible for supercontinent breakup is crucial for establishing Earth's geodynamic evolution that includes supercontinent cycles and plate tectonics. Conventionally, two forces have been considered: the push by mantle plumes from the sub-continental mantle which is called the active force for breakup, and the dragging force from oceanic subduction retreat which is called the passive force for breakup. However, the relative importance of these two forces is unclear. Here we model the supercontinent breakup coupled with global mantle convection in order to address this question. Our global model features a spherical harmonic degree-2 structure, which includes a major subduction girdle and two large upwelling (superplume) systems. Based on this global mantle structure, we examine the distribution of extensional stress applied to the supercontinent by both sub-supercontinent mantle upwellings and subduction retreat at the supercontinent peripheral. Our results show that: (1) at the center half of the supercontinent, plume push stress is ∼3 times larger than the stress induced by subduction retreat; (2) an average hot anomaly of no higher than 50 K beneath the supercontinent can produce a push force strong enough to cause the initialization of supercontinent breakup; (3) the extensional stress induced by subduction retreat concentrates on a ∼600 km wide zone on the boundary of the supercontinent, but has far less impact to the interior of the supercontinent. We therefore conclude that although circum-supercontinent subduction retreat assists supercontinent breakup, sub-supercontinent mantle upwelling is the essential force. Keywords: Supercontinent breakup, Plume push, Subduction retreathttp://www.sciencedirect.com/science/article/pii/S167498711830046X
collection DOAJ
language English
format Article
sources DOAJ
author Nan Zhang
Zhuo Dang
Chuan Huang
Zheng-Xiang Li
spellingShingle Nan Zhang
Zhuo Dang
Chuan Huang
Zheng-Xiang Li
The dominant driving force for supercontinent breakup: Plume push or subduction retreat?
Geoscience Frontiers
author_facet Nan Zhang
Zhuo Dang
Chuan Huang
Zheng-Xiang Li
author_sort Nan Zhang
title The dominant driving force for supercontinent breakup: Plume push or subduction retreat?
title_short The dominant driving force for supercontinent breakup: Plume push or subduction retreat?
title_full The dominant driving force for supercontinent breakup: Plume push or subduction retreat?
title_fullStr The dominant driving force for supercontinent breakup: Plume push or subduction retreat?
title_full_unstemmed The dominant driving force for supercontinent breakup: Plume push or subduction retreat?
title_sort dominant driving force for supercontinent breakup: plume push or subduction retreat?
publisher Elsevier
series Geoscience Frontiers
issn 1674-9871
publishDate 2018-07-01
description Understanding the dominant force responsible for supercontinent breakup is crucial for establishing Earth's geodynamic evolution that includes supercontinent cycles and plate tectonics. Conventionally, two forces have been considered: the push by mantle plumes from the sub-continental mantle which is called the active force for breakup, and the dragging force from oceanic subduction retreat which is called the passive force for breakup. However, the relative importance of these two forces is unclear. Here we model the supercontinent breakup coupled with global mantle convection in order to address this question. Our global model features a spherical harmonic degree-2 structure, which includes a major subduction girdle and two large upwelling (superplume) systems. Based on this global mantle structure, we examine the distribution of extensional stress applied to the supercontinent by both sub-supercontinent mantle upwellings and subduction retreat at the supercontinent peripheral. Our results show that: (1) at the center half of the supercontinent, plume push stress is ∼3 times larger than the stress induced by subduction retreat; (2) an average hot anomaly of no higher than 50 K beneath the supercontinent can produce a push force strong enough to cause the initialization of supercontinent breakup; (3) the extensional stress induced by subduction retreat concentrates on a ∼600 km wide zone on the boundary of the supercontinent, but has far less impact to the interior of the supercontinent. We therefore conclude that although circum-supercontinent subduction retreat assists supercontinent breakup, sub-supercontinent mantle upwelling is the essential force. Keywords: Supercontinent breakup, Plume push, Subduction retreat
url http://www.sciencedirect.com/science/article/pii/S167498711830046X
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