P. Werner
The extent of continental material in oceans: C-Blocks and the Laxmi Basin example
Werner, P.; Foulger, G.R.; Gernigon, L.; Guan, H.; Geoffroy, L.
Abstract
We propose a tectonic interpretation for the outer-SDRs (SDRs: Seaward-Dipping Reflectors) and Pannikar central ridge in the aborted Laxmi Basin west of India from wide-angle seismic reflection data. The outer-SDRs comprise syn-tectonic extrusives (lavas and/or volcaniclastics) emplaced above passively exhumed mid-to-lower mafic crust of continental origin. They erupted following sudden lithosphere weakening associated with isolation of a continental block (a ‘C-Block’). Continuous magmatic addition during crustal extension allowed stretching of the lower crust whilst maintaining constant or even increasing thickness. A similar process occurred at both conjugate margins allowing bulk, pure-shear plate separation and formation of linear magnetic anomalies. The Laxmi example can explain enigmatic features observed in mature oceans such as presence of distal buoyant plateaus of thick continental crust away from the margins.
Citation
Werner, P., Foulger, G., Gernigon, L., Guan, H., & Geoffroy, L. (2020). The extent of continental material in oceans: C-Blocks and the Laxmi Basin example. Geophysical Journal International, 222(3), 1471-1479. https://doi.org/10.1093/gji/ggaa215
Journal Article Type | Article |
---|---|
Acceptance Date | Apr 30, 2020 |
Online Publication Date | May 5, 2020 |
Publication Date | 2020-09 |
Deposit Date | Oct 7, 2020 |
Publicly Available Date | Oct 7, 2020 |
Journal | Geophysical Journal International |
Print ISSN | 0956-540X |
Electronic ISSN | 1365-246X |
Publisher | Oxford University Press |
Peer Reviewed | Peer Reviewed |
Volume | 222 |
Issue | 3 |
Pages | 1471-1479 |
DOI | https://doi.org/10.1093/gji/ggaa215 |
Public URL | https://durham-repository.worktribe.com/output/1254703 |
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Copyright Statement
This article has been accepted for publication in Geophysical journal international ©: 2020 Published by Oxford University Press on behalf of The Royal Astronomical Society. All rights reserved.
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