TIME-ANIMATED GEOCHEMICAL VARIATION DIAGRAMS AS A TOOL FOR EXPLORING LARGE DATASETS
Geochemical data drawn from NAVDAT have been time-animated in a number of ways to reveal interesting trends in magmatism of the western U.S. One example, an animated K2O-SiO2 variation diagram for samples from eastern California and west-central Nevada, shows magma compositions changing from silicic and high-K to more mafic low- and intermediate-K over the interval 10-5 Ma, followed by a pulse of high-K mafic magmatism associated with the 3.5 Ma delamination(?) event. An animated total alkalis-silica volcanic classification diagram of rocks from the same area shows that they are distributed somewhat evenly across the range of rock types from 10-3 Ma, then separate into bimodal basaltic and rhyodacitic populations from 3 Ma to the present. In a third example, we evaluated the conclusion of Ormerod et al. (1988) that the Zr/Ba ratio in late Cenozoic basalts of the western Great Basin changes in concert with a transition in magmatism from basalts derived above a subduction zone to basalts derived from the convecting upper mantle following the south-to-north passage of the trailing edge of the subducting slab. Time-animation of a NAVDAT dataset incorporating six recent studies agrees with their south-to-north migration model.
Time-animation of geochemical variation makes interpretation of otherwise cumbersome datasets easier by putting them in a temporal context. User control over animations increases understanding of the dataset. The greater resolution of time-animations will become increasingly important in interpretation as the amount of information contained in databases such as NAVDAT grows.