GT Merge Process: Version 1.0
This document summarizes the process used to merge GT25 and better data between LANL and LLNL for use in a tomographic inversion for Pn velocity of Eurasia. The merge process is automated and includes extensive quality control operations at each step. Events in common between the labs are identified and resolved using GT level criteria. Arrivals in common between the labs are also resolved through the use of agreed upon arrival author rankings. Finally, baselined origin times are computed for all crustal events using either teleseismic P-arrivals and the iasp91 model or, in certain regions, regional P-arrivals and regional velocity models that are known to be consistent with teleseismic iasp91 P-wave predictions. We combine the core tables from each lab and first resolve unique and common GT events between LANL and LLNL. Phase names are then checked and possibly adjusted for consistency. Next, we merge at the pick level so that each distinct EVENT-STATION-PHASE tuple has a unique arrival. All BMEB (Bondar-Myers-Engdahl-Bergman) GT are evaluated for adherence to their criteria, and possibly re-calculated. Finally, new origin times are computed (baselining) for the merged GT events. In addition to the reconciliation of events and picks between LANL and LLNL, the merge process involves several quality control steps that are intended to remove outlier and irrelevant data from the final results.
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