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Showing 1 to 1 of 1 for “"Manzano Peak Quadrangle"”.
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Geologic and tectonic evolution of the Manzano Peak Quadrangle, central New Mexico
The Sandia and Manzano Mountains in central New Mexico are a N-S-striking, Precambrian-cored, uplift that forms the east flank of the Albuquerque Basin of the Rio Grande Rift. During the Paleoproterozoic, the Precambrian rocks exposed in the range were accreted onto the "southward" growing …