Syntectonic unconformities demonstrate simultaneous subsidence and tectonic activity.
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Growth strata, also known as syntectonic strata, are sedimentary layers that are deposited when folding is.
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Geochronology on the granites is sparse, but has constrained the intrusions to 1680 to 1620 Ma, which is syntectonic to post-tectonic with the Mangaroon Orogeny.
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The polarity ( throw direction ) of the main bounding faults typically alternate along the length of the rift . The asymmetry of a half-graben strongly affects syntectonic deposition.
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