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Early clay diagenesis in Gulf Coast sediments: New insights from XRD profile modeling

Published online by Cambridge University Press:  01 January 2024

Douglas K. McCarty ,
Boris A. Sakharov  and
Victor A. Drits
Douglas K. McCarty*
Affiliation:
Chevron ETC, 3901 Briarpark, Houston, TX, 77063 USA
Boris A. Sakharov
Affiliation:
Geological Institute of the Russian Academy of Science, Pyzevskij per. D.7, 119017, Moscow, Russia
Victor A. Drits
Affiliation:
Geological Institute of the Russian Academy of Science, Pyzevskij per. D.7, 119017, Moscow, Russia
*
* E-mail address of corresponding author: dmccarty@chevron.com
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Abstract

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Samples from different depths in the Oligocene Frio formation (offshore Gulf of Mexico) were studied by X-ray diffraction (XRD), thermal analyses, and scanning electron microscopy. The experimental XRD patterns recorded from oriented and ethylene glycol (EG) solvated clay fractions of the samples were similar to those typical of random, mixed-layered illite-smectite (R0 I-S). The experimental XRD patterns recorded in air-dried (AD) and EG states were simulated using three different models. One of them corresponds to R0 I-S for which thickness and content of the interstratified layers were determined by the Środoń technique. The second model is represented by a single homogeneous I-S in which illite and smectite layers are interstratified with a tendency to segregation. The expandability of the segregated I-S model varies from 48% to 75% without any rational relationship between the smectite layer content and depth.

The third model assumes that the clay fraction is a physical mixture of smectite and an R0 I-S. In this model the I-S contains 65% illite and 35% smectite layers independent of depth, whereas the smectite content varies from 28% to 63%. This model has consistently smaller profile factors, Rp, for both EG and AD XRD scans compared with the Rp values determined for the other two models.

The mineralogical association, volcanic origin, narrow stratigraphic interval (427 m), and low maximum temperature (42°C) of the studied Frio Formation are considered. These features are completely consistent with the two-phase model and so the segregation model must be rejected. An authigenic origin of the pure smectite and an alternative detrital or authigenic origin of the R0 I-S are discussed.

Keywords

DiagenesisGulf CoastIllite-SmectiteFrio FormationSmectite
Type
Article
Information
Clays and Clay Minerals , Volume 56 , Issue 3 , June 2008 , pp. 359 - 379
Copyright
Copyright © 2008, The Clay Minerals Society

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