Występowanie soli niebieskich w Kłodawie
Abstract
Sole niebieskie, a w szczególności ich geneza i charakter czynników barwiących, to jedna z frapujących zagadek współczesnej nauki. Od prawie 150 lat temat ten zajmuje badaczy różnych dziedzin nauki, ale mimo nowych danych, na wiele pytań brak odpowiedzi. Praca ta rozpoczyna cykl artykułów poświęconych solom niebieskim z Kłodawy. Już wstępne wyniki badań chemicznych pozwalają sądzić, że są to sole epigenetyczne, których powstanie nierozerwalnie łączy się z różnorodnymi czynnikami wywołanymi halotektoniką tego wysadu.
BLUE SALT FROM KŁODAWA (KUJAWY, POLAND)
Summary
Blue-coloured salt minerals, and particularly their genesis and the nature of their colouration, are one of the fascinating puzzles of modern science. The problem has been dealt with for almost 150 years by scientists of diversified specializations but, despite new information gathered, many questions remain open. The paper begins a series of presentations devoted to the blue salt minerals from K³odawa Permian deposits. Even preliminary results of chemical analyses allow to conclude that the salts in question are of secondary origin and their genesis is closely related to various factors associated with halotectonics of the K³odawa salt dome. There is a correlation of colour intensity with crystal size (larger halite crystals tend to be darker) and adjacent potassium salt deposits (sylvinite).
BLUE SALT FROM KŁODAWA (KUJAWY, POLAND)
Summary
Blue-coloured salt minerals, and particularly their genesis and the nature of their colouration, are one of the fascinating puzzles of modern science. The problem has been dealt with for almost 150 years by scientists of diversified specializations but, despite new information gathered, many questions remain open. The paper begins a series of presentations devoted to the blue salt minerals from K³odawa Permian deposits. Even preliminary results of chemical analyses allow to conclude that the salts in question are of secondary origin and their genesis is closely related to various factors associated with halotectonics of the K³odawa salt dome. There is a correlation of colour intensity with crystal size (larger halite crystals tend to be darker) and adjacent potassium salt deposits (sylvinite).