Dolomite dissolution: An alternative diagenetic pathway for the formation of palygorskite clay
Abstract
Palygorskite is a fibrous, magnesium-bearing clay mineral commonly associated with Late Mesozoic and Early Cenozoic dolomites. The presence of palygorskite is thought to be indicative of warm, alkaline fluids rich in Si, Al and Mg. Palygorskite has been interpreted to form in peritidal diagenetic environments, either as a replacement of detrital smectite clay during a dissolution–precipitation reaction or solid-state transformation, or as a...
Paper Details
Title
Dolomite dissolution: An alternative diagenetic pathway for the formation of palygorskite clay
Published Date
Feb 18, 2019
Journal
Volume
66
Issue
5
Pages
1803 - 1824
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