Salt-mudstones are evaporative formations occurring in salt domes in significant
amounts. Until now salt-mudstones were considered as mere rock, due to the
depleted amount of salt in them. As a result, they have never been a subject of
mining exploitation.
They are a conglomerate, mainly of the rock salt and clay with a variable content.
In the Central Polish Region, in the whole profile of the Zechstein salt bearing
formation, starting from the half of the stage Z3, rock salt passes into the ‘‘brown
salt-mudstones’’, and in the Z4 stage into the ‘‘red’’ one (‘‘hepatite’’), but at the end
into the clay formation.
Salt-mudstones are of the following kinds:
Salt-mudstones are evaporative formations occurring in salt domes in significant
amounts. Until now salt-mudstones were considered as mere rock, due to the
depleted amount of salt in them. As a result, they have never been a subject of
mining exploitation.
They are a conglomerate, mainly of the rock salt and clay with a variable content.
In the Central Polish Region, in the whole profile of the Zechstein salt bearing
formation, starting from the half of the stage Z3, rock salt passes into the ‘‘brown
salt-mudstones’’, and in the Z4 stage into the ‘‘red’’ one (‘‘hepatite’’), but at the end
into the clay formation.
Salt-mudstones are of the following kinds:
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