GEOLOGY, PETROLOGY, AND SIGNIFICANCE OF RAMOS CRATER, DEATH VALLEY, CA
Magmas from Ramos Crater are relatively alkaline (transitional), conspicuously porphyritic, and vary in composition from trachyandesite to trachydacite (61-65 percent SiO2, 7-8 percent Na2O+K2O). Phenocryst assemblage is variable and includes plagioclase, olivine (altered), clinopyroxene, hornblende, and biotite. Plagioclase phenocrysts are twinned and characterized by sieve textures; subhedral to euhedral hornblende crystals are rimmed by Fe-Ti oxides. The pilotaxitic groundmass consists of plagioclase, Fe-Ti oxides, and other phases similar to the phenocrysts; voids filled with secondary carbonate and zeolite are common.
Geochemical composition of the magmas at Ramos Crater is quite evolved (Mg-number 44-50, low values of compatible trace elements). Rare earth elements are relatively high in abundance (total REE 160-176 ppm) and moderately enriched in LREE relative to HREE (La/YbCN 13.5-15.9). The crater and flows yield εNd values between -5.8 and -6.9, T-DM model ages between 975 and 1,055 Ma, and 87Sr/86Sr values between 0.70812 and 0.70842. Our stratigraphic, geochemical, and isotopic data suggest that magmas from Ramos Crater are post extension, may represent a relatively evolved endmember of extension-related Neogene-Recent volcanism across Death Valley (cf. Calzia et al., 2016, GSA Cordilleran Section Meeting), and suggest the presence of an Fe-enriched (peridotitic/pyroxenitic) lithospheric source component underneath Mojavia.