The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin...
| Published in: | Terra Nova |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Wiley
1998
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| Online Access: | http://dx.doi.org/10.1046/j.1365-3121.1998.00193.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.1998.00193.x https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.1998.00193.x https://onlinelibrary.wiley.com/doi/full-xml/10.1046/j.1365-3121.1998.00193.x |
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crwiley:10.1046/j.1365-3121.1998.00193.x |
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openpolar |
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crwiley:10.1046/j.1365-3121.1998.00193.x 2024-06-02T07:55:41+00:00 The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. Ricou, L.‐E. 1998 http://dx.doi.org/10.1046/j.1365-3121.1998.00193.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.1998.00193.x https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.1998.00193.x https://onlinelibrary.wiley.com/doi/full-xml/10.1046/j.1365-3121.1998.00193.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Terra Nova volume 10, issue 4, page 201-205 ISSN 0954-4879 1365-3121 journal-article 1998 crwiley https://doi.org/10.1046/j.1365-3121.1998.00193.x 2024-05-03T11:17:44Z The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. Article in Journal/Newspaper Antarc* Antarctica Wiley Online Library Pacific Indian Terra Nova 10 4 201 205 |
| institution |
Open Polar |
| collection |
Wiley Online Library |
| op_collection_id |
crwiley |
| language |
English |
| description |
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| format |
Article in Journal/Newspaper |
| author |
Ricou, L.‐E. |
| spellingShingle |
Ricou, L.‐E. The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| author_facet |
Ricou, L.‐E. |
| author_sort |
Ricou, L.‐E. |
| title |
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| title_short |
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| title_full |
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| title_fullStr |
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| title_full_unstemmed |
The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains. |
| title_sort |
global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. we advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the pacific and african sides of the earth, respectively. the columns should merge upward between antarctica and australia to reach the single, long spreading subnetwork. the flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, atlantic–indian and pacific, hot spot domains. |
| publisher |
Wiley |
| publishDate |
1998 |
| url |
http://dx.doi.org/10.1046/j.1365-3121.1998.00193.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.1998.00193.x https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.1998.00193.x https://onlinelibrary.wiley.com/doi/full-xml/10.1046/j.1365-3121.1998.00193.x |
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Pacific Indian |
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Pacific Indian |
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Antarc* Antarctica |
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Antarc* Antarctica |
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Terra Nova volume 10, issue 4, page 201-205 ISSN 0954-4879 1365-3121 |
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http://onlinelibrary.wiley.com/termsAndConditions#vor |
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