UNIGE document Scientific Article
previous document  unige:88288  next document
add to browser collection
Title

Illite-smectite rich clay parageneses from Quaternary tunnel valley sediments of the Dutch Southern North Sea – mineral origin and paleoenvironment implications
Authors
Segvic, Branimir
Benvenuti, Antonio
Moscariello, Andrea
Published in Clays and Clay Minerals. 2016
Abstract The Pleistocene sediment infill of elongated glacial incisions of the Southern North Sea (SNS) often is referred to as tunnel valleys (TV). Its depositional environment is not yet fully understood and present study addresses this challenge from a perspective of clay mineral transformation (illite to I-S) reported from the largest Elsterian TV of SNS. Material acquired from the K14-12 borehole in the Dutch offshore was analyzed by X-ray diffraction, electron microscopy, electron microprobe analyses, and laser particle-size analysis. Illite and illite-smectite appeared as dominant clays along with minor amounts of kaolinite, kaolinite-smectite, and chlorite. Highest amount of I-S is recognized in TV main portion, while in pre-glacial and uppermost deposits I-S is less abundant. The XRD peak fitting and deconvolution suggest I-S consists of several intermediates – ordered (well-crystallized illite + R3 I-S) and disordered (R0 I-S + R0 I-SS). Given the average particle sizes (> 2 μm) and Kübler index values (0.415-0.341°Δ2θ), illite as well as chlorite and kaolinite were interpreted as detrital. On the basis of I-S distinctive distribution, grain sizes, and compositional variations its formation by way of early diagenetic in-situ smectitization of illite under a cold climate is proposed. The process operated via a series of mixed-layer intermediates derived from an illite component being progressively converted to low-charged smectite. The reaction is marked by a significant net loss of K and Al with replacement by Si in a tetrahedral coordination. Layer charge imbalance is accommodated by Fe3+ and Mg entering an octahedral layer, whereas Ca partly fills the interlayer sites. Smectitization rates were controlled by illite grain sizes. The results of this study strongly support the existence of an ice-marginal fresh water depositional environment at the glacial maximum in SNS in which early diagenesis at low temperatures resulted in incomplete illite conversion into smectite.
Keywords Tunnel valley — Smectitization — Illite-smectite — Diagenesis — Southern North Sea — Proglacial lake — Middle Pleistocene
Identifiers
Full text
Article (Preprint) (1.8 MB) - public document Free access
Other version: http://www.ingentaconnect.com/content/cms/ccm/pre-prints/content-ccm-1032
Structures
Faculté des sciences / Section des sciences de la Terre et de l'Environnement / Département des sciences de la Terre
Research group Reservoir Geology and Sedimentary Basin Analyses
Project GRASP
Citation
(ISO format) 		SEGVIC, Branimir, BENVENUTI, Antonio, MOSCARIELLO, Andrea. Illite-smectite rich clay parageneses from Quaternary tunnel valley sediments of the Dutch Southern North Sea – mineral origin and paleoenvironment implications. In: Clays and Clay Minerals, 2016. https://archive-ouverte.unige.ch/unige:88288

164 hits

96 downloads

Contact an author

Update request

Update

Deposited on : 2016-10-18

Export document
Format :
Citation style :