LitMod2D_2.0: An Improved Integrated Geophysical‐Petrological Modeling Tool for the Physical Interpretation of Upper Mantle Anomalies

• Published in: Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2020-03, Vol.21 (3), p.n/a
• Main Authors: Kumar, Ajay, Fernàndez, Manel, Jiménez‐Munt, Ivone, Torne, Montserrat, Vergés, Jaume, Afonso, Juan Carlos
• Format: Article
• Language: English
• Subjects: Anomalies; Chemical composition; Density; Elastic waves; Geoid; Gravity anomalies; Lithosphere; Magma; Mantle; Mineral assemblages; Nonlinearity; Ocean circulation; Regions; Seismic activity; Seismic tomography; Seismic velocities; Seismic wave velocities; Seismological data; Subduction; Temperature; Tomography; Upper mantle; Upwelling; Velocity; Wave dispersion; Wave velocity
• ISSN: 1525-2027; 1525-2027
• DOI: 10.1029/2019GC008777

LitMod2D integrates geophysical and petrological data sets to produce the thermal, density, and seismic velocity structure of the lithosphere and upper mantle. We present a new LitMod2D_2.0 package with improvements focused on (i) updated anelastic attenuation correction for anharmonic seismic velocities, (ii) chemical composition in the sublithospheric mantle, and (iii) incorporation of sublithospheric mantle anomalies. Sublithospheric mantle anomalies can be defined with different chemical composition, temperature, seismic velocities, and a combination of them, allowing the application of LitMod2D_2.0 to regions affected by mantle upwelling, subduction, delamination, and metasomatism. We demonstrate the potential application of LitMod2D_2.0 to such regions and the sensitivity of thermal and compositional anomalies on density and seismic velocities through synthetic models. Results show nonlinearity between the sign of thermal and seismic velocity anomalies, and that S wave velocities are more sensitive to temperature whereas P wave velocities are to composition. In a synthetic example of subduction, we show the sensitivity of sublithospheric mantle anomalies associated with the slab and the corner flow on surface observables (elevation, geoid height, and gravity anomalies). A new open‐source graphic user interface is incorporated in the new package. The output of the code is simplified by writing only the relevant physical parameters (temperature, pressure, material type, density, and seismic velocities) to allow the user using predefined post‐processing codes from a toolbox (flexure, mineral assemblages, synthetic passive seismological data, and tomography) or designing new ones. We demonstrate a post‐processing example calculating synthetic seismic tomography, Rayleigh surface‐wave dispersion curves, and P wave receiver functions from the output file of LitMod2D_2.0. Key Points LitMod2D_2.0 allows studying the thermal and chemical nature of upper mantle anomalies A new open‐source graphic user interface is provided Post‐processing toolbox for tailored processing of the output is added