What is it about?
It is decribed how the aragonites that appear embedded in clay deposits of upper Triassic age in The Iberian basin are the result of hydrothermal fluids and marine waters during the upper Middle Jurassic
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Why is it important?
New approach to explain authigenic minerals at high temperature, but instead of due to burial diagenesis, they are formed under the influence of hydrothermal fluids. New implications to interpret the thermal histroy and evolution of certain sedimentary basisn.
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This page is a summary of: Hydrothermal activity within a sedimentary succession: aragonites as indicators of Mesozoic Rifting (Iberian Basin, Spain)., International Geology Review, June 2019, Taylor & Francis,
DOI: 10.1080/00206814.2019.1636317.
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