Palygorskite-dominated clayey sedimentary beds of the Çameli formation in the Neogene Sapaca lacustrine basin, Honaz, Denizli Province, SW Turkey

Kadır, Selahattın; Akbulut, Aydogan

doi:10.1127/0077-7757/2011/0198

njma

2011

DOI: 10.1127/0077-7757/2011/0198

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Palygorskite-dominated clayey sedimentary beds of the Çameli formation in the Neogene Sapaca lacustrine basin, Honaz, Denizli Province, SW Turkey

Selahattın Kadır¹,

Aydogan Akbulut²

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“…Singer, 1984;Rodas et al, 1994;Verrecchia & Le Coustumer, 1996;Colson et al, 1998;Pimentel, 2002), including occurrences in Turkey (e.g. Kapur et al, 1987Kapur et al, , 1993Karakas°& Kadir, 1998;Eren et al, 2004Kadir & Akbulut, 2011). The aforementioned studies include mineralogical, geochemical, stable-isotopic and micromorphological investigations of palygorskite and the associated calcretes and mudstones.…”

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Genesis of Late Miocene-Pliocene lacustrine palygorskite and calcretes from Kırşehir, central Anatolia, Turkey

et al. 2014

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AB ST R ACT : This paper addresses the mineralogy, geochemistry, and genesis of palygorskite and associated calcretes in the Kırs°ehir region. In this area, the Quaternary calcretes are present within and/or on lacustrine mudstones of the Kızılırmak Formation (Late Miocene-Pliocene). The calcretes occur in the form of nodules, tubes, fracture-infills, and hard laminated crusts (hardpans). Calcrete samples are predominantly composed of calcite associated with smectite, quartz, feldspar, and minor palygorskite. The lacustrine mudstone samples consist mainly of smectite and palygorskite with minor calcite, quartz, feldspar, illite, kaolinite and amorphous material. Petrographic studies revealed that the calcrete samples are predominantly micrites that were partially converted to microsparites by recrystallization. Scanning and transmission electron microscopy images indicate that palygorskite fibres formed authigenically on and between calcite rhombs in the calcrete samples and at the edges of smectite flakes of host rocks adjacent to the calcretes. The oxygen and hydrogen stable isotope values of the calcite suggest that it precipitated from meteoric water under arid or seasonally arid climatic conditions. Calcite precipitation occurred in the vadose zone, as evidenced by desiccation cracks and vadose pisolites. The enrichment of Rb+BaÔSr and Light Rare Earth Elements (LREE) relative to Heavy Rare Earth Elements (HREE)with a distinct negative Eu anomaly are responses to the fractionation of volcanogenic feldspar and hornblende under the influence of meteoric water. The palygorskite associated with calcretes was precipitated from alkaline water rich in Si, Al and Fe and low in Mg. The palygorskite precipitation occurred at increased temperatures, characterising the advanced stage of calcrete formation which lowers the Ca content in the soil water. The required chemical elements for palygorskite and calcite were most likely derived from the dissolution of smectitic clays, ignimbrites and carbonate minerals.The occurrence of palygorskite in calcretes has been studied extensively over the past 30 years (e.g.

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Genesis of Late Miocene-Pliocene lacustrine palygorskite and calcretes from Kırşehir, central Anatolia, Turkey

et al. 2014

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Genesis of palygorskite and calcretes in Pliocene Eskişehir Basin, west central Anatolia, Turkey

Kadır

Eren

Külah

et al. 2018

CATENA

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Mineralogy, geochemistry, and genesis of lithium-bearing argillaceous sediments associated with the Neogene Bigadiç borate deposits, Balıkesir, western Anatolia, Türkiye

Kadır

Külah

Erkoyun

et al. 2023

Applied Clay Science

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Palygorskite-dominated clayey sedimentary beds of the Çameli formation in the Neogene Sapaca lacustrine basin, Honaz, Denizli Province, SW Turkey

Cited by 3 publications

References 0 publications

Genesis of Late Miocene-Pliocene lacustrine palygorskite and calcretes from Kırşehir, central Anatolia, Turkey

Genesis of Late Miocene-Pliocene lacustrine palygorskite and calcretes from Kırşehir, central Anatolia, Turkey

Genesis of palygorskite and calcretes in Pliocene Eskişehir Basin, west central Anatolia, Turkey

Mineralogy, geochemistry, and genesis of lithium-bearing argillaceous sediments associated with the Neogene Bigadiç borate deposits, Balıkesir, western Anatolia, Türkiye

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