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Cited by 262

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Gulf of California: A Result of Ocean-Floor Spreading and Transform Faulting

Larson, Roger L., Menard, H. W., Smith, S. M.·1968·Science

Abstract

Ocean-floor spreading tore southern Baja California from mainland Mexico 4 million years ago and has subsequently rafted it 260 kilometers to the northwest along the Tamayo Fracture Zone. Magnetic-anomaly profiles indicate spreading at the mouth of the gulf at 3.0 centimeters per year and a rise-crest offset of 75 kilometers inside the gulf across the Tamayo Fracture Zone.

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Metadata

Authors
Larson, R. L., Menard, H. W., & Smith, S. M.
Venue
Science
Published
1968-08-23
Volume
161
Issue
3843
Pages
781-784
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2080888474
Cited by
262
References
0
FWCI
12.02
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Gulf of California: A Result of Ocean-Floor Spreading and Transform Faulting. https://app.cochat.ai/papers/10.1126/science.161.3843.781
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Larson, R. L., Menard, H. W., & Smith, S. M. (1968). Gulf of California: A Result of Ocean-Floor Spreading and Transform Faulting. Science. https://doi.org/10.1126/science.161.3843.781

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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.