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Dolomitization by hypersaline reflux into dense groundwaters as revealed by vertical trends in strontium and oxygen isotopes: Upper Muschelkalk, Switzerland
Author(s) -
Adams Arthur,
Diamond Larryn W.,
Aschwanden Lukas
Publication year - 2019
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/sed.12530
Subject(s) - geology , dolomitization , petrography , isotopes of strontium , strontium , meteoric water , geochemistry , recrystallization (geology) , isotopes of oxygen , radiogenic nuclide , borehole , diagenesis , δ18o , structural basin , hydrothermal circulation , stable isotope ratio , paleontology , facies , chemistry , mantle (geology) , organic chemistry , quantum mechanics , physics
The Trigonodus Dolomit is the dolomitized portion of the homoclinal ramp sediments of the Middle Triassic Upper Muschelkalk in the south‐east Central European Basin. Various dolomitizing mechanisms, followed by recrystallization, have been previously invoked to explain the low δ 18 O, high 87 Sr/ 86 Sr, extensive spatial distribution and early nature of the replacive matrix dolomites. This study re‐evaluates the origin, timing and characteristics of the dolomitizing fluids by examining petrographic and isotopic trends in the Trigonodus Dolomit at 11 boreholes in northern Switzerland. In each borehole the ca 30 m thick unit displays the same vertical trends with increasing depth: crystal size increase, change from anhedral to euhedral textures, ultraviolet‐fluorescence decrease, δ 18 O VPDB decrease from −1·0‰ at the top to −6·7‰ at the base and an 87 Sr/ 86 Sr increase from 0·7080 at the top to 0·7117 at the base. Thus, dolomites at the top of the unit record isotopic values similar to Middle Triassic seawater ( δ 18 O VSMOW = 0‰; 87 Sr/ 86 Sr = 0·70775) while dolomites at the base record values similar to meteoric groundwaters from the nearby Vindelician High ( δ 18 O VSMOW = −4·0‰; 87 Sr/ 86 Sr = >0·712). According to water–rock interaction modelling, a single dolomitizing or recrystallizing fluid cannot have produced the observed isotopic trends. Instead, the combined isotopic, geochemical and petrographic data can be explained by dolomitization via seepage‐reflux of hypersaline brines into dense, horizontally‐advecting groundwaters that already had negative δ 18 O and high 87 Sr/ 86 Sr values. Evidence for the early groundwaters is found in meteoric calcite cements that preceded dolomitization and in fully recrystallized dolomites with isotopic characteristics identical to the groundwaters following matrix dolomitization. This study demonstrates that early groundwaters can play a decisive role in the formation and recrystallization of massive dolomites and that the isotopic and textural signatures of pre‐existing groundwaters can be preserved during seepage‐reflux dolomitization in low‐angle carbonate ramps.