Boletín de la Sociedad Geológica Mexicana Volumen 74, núm. 1, A161021, 2022 http://dx.doi.org/10.18268/BSGM2022v74n1a161021

Magnetic fabric and sedimentary characterization of near-slope to basinal deposits from the Chicontepec Formation, central and southern region of the Tampico-Misantla basin

Fábrica magnética y caracterización de depósitos sedimentarios cercanos a la cuenca de la Formación Chicontepec, región centro y sur de la cuenca Tampico-Misantla

Roberto Stanley Molina-Garza^1,† , María Isabel Sierra-Rojas^2,*

¹ Centro de Geociencias, Universidad Nacional Autónoma de México, Blvd. Juriquilla 3001, Querétaro, México.

² Departamento de Geociencias, Universidad de los Andes, Cra 1 # 18a-12, Bogotá D.C., Colombia.

^† En memoria de su trabajo.

* Corresponding author: (M. I. Sierra-Rojas) This email address is being protected from spambots. You need JavaScript enabled to view it.

How to cite this article:

Molina-Garza, R., Sierra-Rojas, M., 2022, Magnetic fabric and sedimentary characterization of near-slope to basinal deposits from the Chicontepec Formation, central and southern region of the Tampico-Misantla basin: Boletín de la Sociedad Geológica Mexicana, 74 (1), A161021. http://dx.doi.org/10.18268/BSGM2022v74n1a161021

ABSTRACT

We report results of a study of the Chicontepec Formation magnetic fabric in the central and southern region of the Tampico-Misantla basin in the state border region between Veracruz and Hidalgo. Samples were collected at 16 sites corresponding to two main facies associations: channel-fill facies and channel overbank facies. The channel facies dominate the relief developing prominent geoforms adjacent to low hills developed in facies dominated by shales. Measurements were made on channel and overbank facies. Laboratory analyses include anisotropy of magnetic susceptibility (AMS) and remanence anisotropy (AARM), as well as isothermal remanence acquisition (IRM) and thermomagnetic curves to characterize magnetic mineralogy. The magnetic susceptibility values of the entire collection are of the order of 40 to 70 x10^-6 SI, so the susceptibility fabric is controlled by the paramagnetic fraction. The IRM acquisition curves are near saturation with inductions < 0.3 T and can be modeled with a low coercivity component contributing ~ 90% and a high coercivity component contributing < 10%. The thermomagnetic curves are dominated by paramagnetic phases. In the AMS fabric, three types of behavior are observed, corresponding to a lesser extent to sedimentary fabrics (k3 ~ vertical), and mostly to incipient and well-developed tectonic fabrics. The sedimentary fabrics are characterized by the imbrication of the magnetic foliation perpendicular to the paleocurrent data obtained in the field, which are generally consistent from NW to SE. At sites with tectonic fabric, which generally correspond to sites closer to the deformation front, the magnetic lineaments are well clustered in the NW quadrant with low plunges. AMS and AARM fabrics may combine in complex patterns. AARM appears to record either maximum axis directions that correspond to alignment of elongated particles perpendicular to flow or the direction of thrust motion.

Key words: magnetic fabric, Chicontepec Formation, turbidite systems.