Options
June 2026
Journal Article
Title
Identifying the magnesium source in hydrothermal dolostone reservoirs: A multi-proxy approach using δ26Mg, δ44/40Ca, and 87Sr/86Sr
Abstract
Dolostone, especially replacement dolostone, is a significant component of Earth's carbonate rock archive. Hydrothermal dolostones, often associated with fault zones, play a crucial role in the dolostone record. However, the origin—particularly the sources of magnesium involved in their for
mation—remains unclear. This study focuses on two case examples of upper Ediacaran hydrothermal dolomite from the Yangtze Block, utilising a multi-proxy approach that examines δ 26 Mg, δ 44 / 40 Ca, 87 Sr/ 86 Sr ratios, and elemental concentrations. In the first study site (i.e., the central Sichuan Basin in the
upper Yangtze Block), saddle dolomites of Ediacaran dolostones were measured to have fluid inclusion homogenization temperatures up to 260 ◦ C, which are significantly higher than those the strata experienced, and are characterised by low δ 26 Mg values ( 2.23‰ ± 0.18‰) and δ 44 / 40 Ca values (0.81‰
and 1.10‰), along with high strontium (Sr) contents (103.9 ± 56.0 ppm) and 87 Sr/ 86 Sr ratios (0.7119 ± 0.0017). These geochemical data indicate that hydrothermal dolomites were precipitated from hydrothermal fluids after obtaining Mg from chlorite-bearing crustal lithologies. Hydrothermal dolo
mitisation likely occurred in the mixing of crust-derived fluids and burial brines. In contrast, at the second study site (i.e., Nanshanping outcrop at the middle Yangtze Block), the presence of 26 Mg enriched (δ 26 Mg: 0.6‰ to 0.5‰) saddle dolomite with low Sr contents (47.0 ± 9.6 ppm) suggests the
influence of mantle-derived fluids. The hydrogeochemistry of the parent fluid appears to be the primary factor controlling the δ 26 Mg and δ 44 / 40 Ca values, as well as the 87 Sr/ 86 Sr ratios of hydrothermal dolomite.
This is further verified by hydrothermal dolomite from the Ediacaran to the Phanerozoic and diagenetic models. Low δ 26 Mg values combined with high 87 Sr/ 86 Sr ratios in hydrothermal dolomite generally indicate the presence of crustal fluids. Conversely, high δ 26 Mg values, along with low 87 Sr/ 86 Sr ratios, are
typically associated with the involvement of the mantle-derived fluids. The study presents two distinct sources of Mg, typically for the formation of hydrothermal dolostones, providing some clues to solve the puzzle for the origin of dolomite, particularly in settings characterised by widespread hydrothermal
fluid activity.
mation—remains unclear. This study focuses on two case examples of upper Ediacaran hydrothermal dolomite from the Yangtze Block, utilising a multi-proxy approach that examines δ 26 Mg, δ 44 / 40 Ca, 87 Sr/ 86 Sr ratios, and elemental concentrations. In the first study site (i.e., the central Sichuan Basin in the
upper Yangtze Block), saddle dolomites of Ediacaran dolostones were measured to have fluid inclusion homogenization temperatures up to 260 ◦ C, which are significantly higher than those the strata experienced, and are characterised by low δ 26 Mg values ( 2.23‰ ± 0.18‰) and δ 44 / 40 Ca values (0.81‰
and 1.10‰), along with high strontium (Sr) contents (103.9 ± 56.0 ppm) and 87 Sr/ 86 Sr ratios (0.7119 ± 0.0017). These geochemical data indicate that hydrothermal dolomites were precipitated from hydrothermal fluids after obtaining Mg from chlorite-bearing crustal lithologies. Hydrothermal dolo
mitisation likely occurred in the mixing of crust-derived fluids and burial brines. In contrast, at the second study site (i.e., Nanshanping outcrop at the middle Yangtze Block), the presence of 26 Mg enriched (δ 26 Mg: 0.6‰ to 0.5‰) saddle dolomite with low Sr contents (47.0 ± 9.6 ppm) suggests the
influence of mantle-derived fluids. The hydrogeochemistry of the parent fluid appears to be the primary factor controlling the δ 26 Mg and δ 44 / 40 Ca values, as well as the 87 Sr/ 86 Sr ratios of hydrothermal dolomite.
This is further verified by hydrothermal dolomite from the Ediacaran to the Phanerozoic and diagenetic models. Low δ 26 Mg values combined with high 87 Sr/ 86 Sr ratios in hydrothermal dolomite generally indicate the presence of crustal fluids. Conversely, high δ 26 Mg values, along with low 87 Sr/ 86 Sr ratios, are
typically associated with the involvement of the mantle-derived fluids. The study presents two distinct sources of Mg, typically for the formation of hydrothermal dolostones, providing some clues to solve the puzzle for the origin of dolomite, particularly in settings characterised by widespread hydrothermal
fluid activity.
Author(s)
