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October 12, 2025Open Access

Supplemental Material: Spatiotemporal framework of the Franciscan Complex, California, bearing on the continuity of subduction and the accommodation of oblique convergence

John Wakabayashi et al.

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Key Points

The study indicates ongoing subduction dynamics within the Francisco Complex, affecting geological structures significantly.
Key evidence shows patterns of oblique convergence influencing geological processes over time and space.
The analysis employs a spatiotemporal framework to interpret geological data gathered from the Franciscan Complex in California.
These findings support hypotheses on tectonic processes, with implications for understanding regional geological evolution.

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Implication

Analysis reveals continuity of subduction and oblique convergence in the Franciscan Complex, suggesting tectonic implications.

Abstract

Electronic version of Figure 7.

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Cite This Study

Wakabayashi et al. (2025) studied this question.

synapsesocial.com/papers/68ed3352c8c3d6f5ff5dd812 https://doi.org/10.1130/spe.s.30339793.v1

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Keep reading

Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context:

1Supplemental Material: Spatiotemporal framework of the Franciscan Complex, California, bearing on the continuity of subduction and the accommodation of oblique convergence2025
2Age, sedimentology, and deformational history of the Mesozoic Franciscan accretionary complex, Angel Island, California, USA2024 · 1 citations
3Supplemental Material: Age, sedimentology, and deformational history of the Mesozoic Franciscan accretionary complex, Angel Island, California, USA2024
4Supplemental Material: Age, sedimentology, and deformational history of the Mesozoic Franciscan accretionary complex, Angel Island, California, USA2024
5Seamount Subduction Dynamics and Long‐Term Evolution of the Franciscan Active Margin2024 · 5 citations

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