Early Cambrian alkaline volcanism on the southern margin of Laurentia: evidence in the volcaniclastic units from the Puerto Blanco Formation in the Caborca block, NW Mexico


Por: Joaquin Barron-Diaz, Arturo, Abraham Paz-Moreno, Francisco, Lozano-Santa Cruz, Rufino, Herrera-Urbina, Saul, Centeno-Garcia, Elena, Lopez-Martinez, Margarita

Publicada: 3 jul 2019
Categoría: Geology

Resumen:
Volcaniclastic units are exposed at the base of the Puerto Blanco Formation in the Caborca region, northwestern Mexico. The lower unit reveals the presence of Early Cambrian mafic volcanism in this region. It consists of a volcano-sedimentary sequence represented by tuffaceous conglomerates, agglomerates, lapillistones, tuffs, and altered mafic volcanic flows. Petrographic analysis classified the volcanic clasts as albite-sphene-calcite-actinolite granofels, with a moderate to intense hydrothermal alteration, precisely characterized by EPMA analysis. Albite-actinolite geothermometry indicates temperatures from 400 to 500 degrees C, suggesting metamorphic conditions in the upper temperature greenschist facies. Geochemistry analysis shows a high TiO2 basic-ultrabasic volcanism that originated the volcanic clasts. Rock protoliths were studied using immobile trace elements, which classified them as OIB-type alkaline basalts with the characteristic spider hump-shaped pattern, situated in an anorogenic intracontinental tectonic setting with enriched mantle signatures. Ar-40/Ar-39 geochronology shows metamorphic ages of 52.58 +/- 2.0 and 91.67 +/- 0.55 Ma, consistent with the emplacement of Laramidic granitoids identified in the region. Possible correlations of this alkaline volcanism include the Southern Oklahoma Aulacogen and the late stages of the rifting of north western Laurentia represented in western United States.

Filiaciones:
Joaquin Barron-Diaz, Arturo:
 Univ Nacl Autonoma Mexico, Inst Geol, Hermosillo, Sonora, Mexico

Abraham Paz-Moreno, Francisco:
 Univ Sonora, Dept Geol, Hermosillo, Sonora, Mexico

Lozano-Santa Cruz, Rufino:
 Univ Nacl Autonoma Mexico, Inst Geol, Lab Nacl Geoquim & Mineral, Mexico City, DF, Mexico

 Laboratorio Nacional de Geoquímica y Mineralogía, Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad de México, Mexico

Herrera-Urbina, Saul:
 Univ Sonora, Dept Geol, Hermosillo, Sonora, Mexico

 Departamento de Geología, Universidad de Sonora, Hermosillo, Mexico

Centeno-Garcia, Elena:
 Univ Nacl Autonoma Mexico, Inst Geol, Lab Nacl Geoquim & Mineral, Mexico City, DF, Mexico

 Laboratorio Nacional de Geoquímica y Mineralogía, Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad de México, Mexico

Lopez-Martinez, Margarita:
 Ctr Invest Cient & Educ Super Ensenada, Ensenada, Baja California, Mexico

 Centro de Investigación Científica y Educación Superior de Ensenada, Ensenada, Mexico

Instituto d e Geología, Universidad Nacional Autónoma de México, Hermosillo, Mexico
ISSN: 00206814
Editorial
Taylor and Francis Inc., 8640 GUILFORD RD, STE 200, COLUMBIA, MD 21046 USA, Estados Unidos America
Tipo de documento: Article
Volumen: 61 Número: 10
Páginas: 1189-1206
WOS Id: 000466372400002

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