Understanding the interaction between brine and impure salt rock is essential for the long-
term stability of salt caverns used in energy storage. This knowledge is crucial for optimizing …

Building upon our previous study that investigated the interactions between brine and
impure salt rock, this study extends the understanding of salt rock behavior by examining the …

Abstract Homogenous and thick (approximately 40–170 m) halite intervals in the upper part
of the Lotsberg Formation are most favored targets for hydrogen (H2) storage caverns in …

The stromatolite tufa mound at La Saline Lake developed along the Athabasca River Valley
in northeast Alberta consists of a 30 m-high structure with a multi-meter thick caprock of …

This case study documents the morphogenesis of a new karstic landform consisting of a
calcareous tufa mound with a gypsum caprock that developed at La Saline Lake, an oxbow …

A tufa mound developed at La Saline Lake, an oxbow of the Athabasca River in the
Athabasca Oil Sands deposit of north‐east Alberta, is characterised by an unusual …

Several lacustrine carbonate beds, each a metre‐thick interval of densely packed Mn‐rich
sideritic micro‐spherulites or Mn‐rich ferroan calcite micro‐spherulites, are recorded for the …

Calcite-cemented sand intervals are widely distributed in the lower interval of the McMurray
Formation of the Lower Cretaceous Athabasca Oil Sands deposit, northeastern Alberta …