Geochemistry of low‐temperature dolomite formation in coastal and continental saline to sabkha‐like environments
Early diagenetic dolomite forms at low temperatures (<50°C) in settings where relative contributions of microbial influences and pore‐fluid chemistry are difficult to separate. Here, dolomite and associated aragonite, calcite and Mg‐calcite from modern and ancient coastal and continental settings in Spain, Australia an...