Accretion tectonics of the global seafloor and its evolution

On the basis of the third generation map of the magnetic lineations of the world’s ocean basins (Cande et al., 1989), a systematic element division is made for the accretion tectonics of the world’s seafloor by use of the conception of accretion area and accretion period. This work reveals the evolu...

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Veröffentlicht in:Science China. Earth sciences 1998-12, Vol.41 (6), p.616-625
Hauptverfasser: Ma, Zongjin, Li, Cunti, Gao, Xianglin
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Gao, Xianglin
description On the basis of the third generation map of the magnetic lineations of the world’s ocean basins (Cande et al., 1989), a systematic element division is made for the accretion tectonics of the world’s seafloor by use of the conception of accretion area and accretion period. This work reveals the evolution process of the seafloor, which is divided into 49 accretion areas and 6 accretion periods. It is found that the latter accretion processes play reform roles such as splitting and wedging action to the former. From the viewpoint of the whole it seems that the accretion process of the seafloor is characterized by the global episodic synchroneity and strong heterogeneity in spatial distribution as well as the local discontinuity.
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ispartof Science China. Earth sciences, 1998-12, Vol.41 (6), p.616-625
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language eng
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source Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings
subjects Accretion
Deposition
Evolution
Heterogeneity
Marine
Ocean basins
Ocean bottom
Ocean floor
Physical oceanography
Plate tectonics
Spatial distribution
Tectonics
title Accretion tectonics of the global seafloor and its evolution
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