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AN ENERGY-DISPERSIVE X-RAY FLUORESCENCE ANALYSIS OF OBSIDIAN ARTIFACTS FROM LA 104416, SOUTHEAST NEW MEXICO
Abstract
All the artifacts were produced from the Cerro Toledo Rhyolite source from the Jemez Mountains, northern New Mexico, although the obsidian is available as secondary deposits in Rio Grande Quaternary alluvium (Church 2000; Shackley 2012; Table 1 and Figure 1 here).
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