Intraplate seismicity, reactivation of preexisting zones of weakness, alkaline magmatism, and other tectonism postdating continental fragmentation¶
Sykes. Intraplate seismicity, reactivation of preexisting zones of weakness, alkaline magmatism, and other tectonism postdating continental fragmentation.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Rift Zone
- Extension may halt at any stage: arrested rifts (aulacogens) remain as long-lived crustal weaknesses prone to reactivation
This sourceReviews of Geophysics, 1978. A plate-tectonic survey recording that failed rifts and other preexisting zones of weakness are preferentially reactivated by later tectonism.
Supported in partVerified against the publisher's abstract
“Many preexisting zones of weakness (including fault zones, suture zones, failed rifts, and other tectonic boundaries), particularly those near continental margins, were reactivated during the early stages of continental separation.”
- Extension may halt at any stage: arrested rifts (aulacogens) remain as long-lived crustal weaknesses prone to reactivation
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Registry ID ref:829cddef587d · see in the full table