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Showing 1 to 6 of 6 for “"Manzano Mountains"”.

  1. Banded metasiltstones in Trigo Canyon : the story they tell about the Proterozoic deformational history of the Manzano Mountains

    Proterozoic banded metasiltstones in the Manzano Mountains of central New Mexico are a distinctive structural marker in the Capilla Peak Quadrangle. These rocks are important because they preserve a record of early history of the Manzano thrust belt. The rocks are newly interpreted as mylonitized …

    unm Repository record for Banded metasiltstones in Trigo Canyon : the story they tell about the Proterozoic deformational history of the Manzano Mountains (opens in a new tab)

  2. New structural interpretation, microstructural analyses, and preliminary monazite geochronology of Proterozoic rocks in the central Manzano Mountains, New Mexico

    The Manzano Mountains of central New Mexico, on the east flank of the Rio Grande Rift, provide excellent outcrops of Proterozoic basement. Rock types in the area include Sevilleta metarhyolite, amphibolitic metavolcanic rocks, schist, meta-lithic arenite, banded metarhyolite, the White Ridge and …

    unm Repository record for New structural interpretation, microstructural analyses, and preliminary monazite geochronology of Proterozoic rocks in the central Manzano Mountains, New Mexico (opens in a new tab)

  3. Polyphase tectonics and metamorphism and their relation to movement on the Monte Largo shear zone in the Manzano Mountains, central New Mexico

    The Proterozoic rocks of the Manzano Mountains of central New Mexico preserve evidence of multiple deformation events. The dominant foliation is the northeast-trending S2 that overprints the older S1 foliation in most places. Later S3 fabrics are present in many areas as well as S4 crenulations in …

    unm Repository record for Polyphase tectonics and metamorphism and their relation to movement on the Monte Largo shear zone in the Manzano Mountains, central New Mexico (opens in a new tab)

  4. 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 …

    unm Repository record for Geologic and tectonic evolution of the Manzano Peak Quadrangle, central New Mexico (opens in a new tab)

  5. Prehistoric Roads of New Mexico: A Synthesis of GIS and Remote Sensing Techniques

    … three different study areas of New Mexico; the Manzano Mountains, Chaco Canyon, and the Salinas Pueblos. A comprehensive methodology for predictive modeling of ancient road locations was created using multiple GIS and remote-sensing analyses on two previously identified prehistoric road study …

    unm Repository record for Prehistoric Roads of New Mexico: A Synthesis of GIS and Remote Sensing Techniques (opens in a new tab)

  6. Proterozoic thermal and deformational history and geochemical evolution of the 1.4 Ga Priest pluton and its aureole

    … The 1.43 Ga Priest pluton in the southern Manzano Mountains provides a key area for understanding middle crustal processes of regional aureole metamorphism and foliation reactivation and for deciphering the tectonic history of Proterozoic rocks in New Mexico. Because of its limited size (9 …

    unm Repository record for Proterozoic thermal and deformational history and geochemical evolution of the 1.4 Ga Priest pluton and its aureole (opens in a new tab)