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Marginal offsets, fracture zones, and the early opening of the North Atlantic

Le Pichon, Xavier, Fox, Paul J.·1971·Journal of Geophysical Research

Abstract

A simplified model is proposed that can explain the evolution of marginal offsets, ridges, and fracture zones. Submarine features of the equatorial Atlantic margins are examined and are found to be in reasonable agreement with the model. The results reaffirm the suggestion that the South Atlantic opened in two stages beginning about 140 m.y. and 80 m.y. ago. The pole of rotation describing the relative motion of the South American and African plates changed radically when the constraints imposed by adjacent continental blocks were relaxed.

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Metadata

Authors
Le Pichon, X., & Fox, P. J.
Venue
Journal of Geophysical Research
Published
1971-09-10
Volume
76
Issue
26
Pages
6294-6308
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2120954655
Cited by
397
References
0
FWCI
29.15
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Marginal offsets, fracture zones, and the early opening of the North Atlantic. https://app.cochat.ai/papers/10.1029/jb076i026p06294
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Le Pichon, X., & Fox, P. J. (1971). Marginal offsets, fracture zones, and the early opening of the North Atlantic. Journal of Geophysical Research. https://doi.org/10.1029/jb076i026p06294

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.