pith. sign in
theorem

richter_b_value_in_aki_window

proved
show as:
module
IndisputableMonolith.Geology.GutenbergRichterFromLedger
domain
Geology
line
149 · github
papers citing
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plain-language theorem explainer

The RS-derived Gutenberg-Richter b-value lies inside the Aki window 0.85 < b < 1.15. Seismologists comparing ledger-based predictions to global catalogs would cite this result to show consistency with the observed b ≈ 1. The proof reduces the claim to the equality b = 1 and verifies the numerical bounds directly.

Claim. The base-10 slope $b$ of the Gutenberg-Richter frequency-magnitude relation satisfies $0.85 < b < 1.15$, where $b$ equals the product of rungs per magnitude and the natural-log rung slope divided by $ln 10$.

background

In the Recognition Science treatment of geology, earthquake magnitudes correspond to stress-drop events on the phi-ladder of recognition costs. The Gutenberg-Richter law states that the cumulative number of events $N(M)$ with magnitude at least $M$ obeys $log_{10} N(M) = a - b M$. The module derives that each Richter magnitude unit spans $R = log_{10} (phi^{-1})$ rungs, and the frequency ratio per rung is $1/phi$, forcing the slope $b$ to equal 1.

proof idea

The proof applies the equality theorem that sets the b-value to 1, then uses norm_num to confirm that 0.85 is less than 1 and 1 is less than 1.15.

why it matters

This result supplies the numerical bound required by the master certificate gutenbergRichterCert for the Gutenberg-Richter law. It confirms that the forced value b = 1 from the phi-ladder lies inside the empirical Aki window (0.85, 1.15) commonly reported in seismology. The derivation ties to the Recognition Composition Law and the self-similar fixed point phi, ensuring the frequency drop per energy rung matches observations without free parameters.

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