Meteorización y marco tectónico de rocas siliciclásticas de la Formación Morita, noreste de Sonora, México

Translated title of the contribution: Weathering and tectonic framework of siliciclastic rocks of the Morita Formation, northeast of Sonora, Mexico

Erik Ramírez-Montoya, Jayagopal Madhavaraju*, Rogelio Monreal, Carlos M. González-León, Francisco J. Grijalva-Noriega, Julio Cesar Saucedo-Samaniego, Inocente G. Espinoza-Maldonado

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

6 Scopus citations

Abstract

Geochemistry of major oxides was carried out on the siliciclastic rocks collected from the Sierra Anibacachi and Rancho Búfalo sections of the Morita Formation (Early Cretaceous) exposed in the northeast of Sonora, to interpret the paleoweathering conditions and tectonic settings of the source rocks. Geochemically, the siliciclastic rocks were classified as sublitharenite, litharenite, subarkose and Fe-sand. The Morita Formation consists mainly of siliciclastic rocks that were deposited under fluvial conditions and the total thickness vary between 560 and 855 m in Sierra Anibacahi and Rancho Búfalo, respectively. The CIA and PIA values and A-CN-K diagram of sandstones from Sierra Anibacachi section indicate a low to intense chemical weathering of the source area, whereas CIA values for siltstone and shale show moderate intensity of chemical weathering in the source region. Similarly, the CIA and PIA values and the A-CN-K plot suggest that the sandstones from Rancho Búfalo section were derived from low to intensely weathered source region, whereas siltstones were received sediments from source rocks affected by low to moderate degree of chemical weathering. The siliciclastic rocks from Sierra Anibacachi and Rancho Búfalo sections show large variations in ICV values, indicating that these samples are compositionally immature to mature. The tectonic discriminant-function-based multidimensional diagram shows arc, rift and collision fields for the sandstones from Sierra Anibacachi section, rift and collision for siltstone, while collision setting for shales. However, most of the sandstones and siltstones from Rancho Búfalo section fall in the arc field, whereas some sandstones fall in the collision field. The siliciclastic rocks from Sierra Anibacachi and Rancho Búfalo section show large variations in the tectonic settings of the source rocks. However, the results obtained from the discriminant function diagrams are consistent with a regional tectonic evolution of the study area.

Translated title of the contributionWeathering and tectonic framework of siliciclastic rocks of the Morita Formation, northeast of Sonora, Mexico
Original languageSpanish
Pages (from-to)103-115
Number of pages13
JournalRevista Mexicana de Ciencias Geologicas
Volume35
Issue number2
DOIs
StatePublished - 2018

Bibliographical note

Publisher Copyright:
© 2018 Centro de Geociencias.

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