Литология нижнепермских карбонатных и сульфатных эвапоритов района «классического» кунгура (Пермский край)

T A Kalinina

Аннотация


Литологическое изучение карбонатных и сульфатных эвапоритов района «классического» кунгура на территории Пермского края позволило показать, что данный комплекс пород сформировался в течение пяти циклов развития эвапоритового бассейна, которое завершилось его полным усыханием (исключение составила территория Соликамской впадины). Смена тонкослоистого пелитоморфного или массивного оолитового доломита шевронной, массивной, желваковой и линзовидно-желваковой сульфатной породой в пределах ритмопачки может свидетельствовать о закономерном изменении концентрации вод бассейна в течение одного цикла. Выдержанное строение ритмопачек и их неоднократное чередование в разрезе нижнепермских эвапоритов говорят об осадконакоплении в обширном мелководном, периодически опресняющемся бассейне. Установлено, что текстура сульфатов формируется на стадии седиментации и диагенеза и зависит от содержания несульфатного материала в породе и анизотропии минералообразующей среды. Литологические особенности строения более молодых соликамских соляно-мергельных отложений, сформировавшихся после отложений хлоридных солей в Соликамской впадине, позволяют предполагать их образование в условиях, близких к современным себхам.

Ключевые слова


Пермский край; карбонатные и сульфатные эвапориты; литология; иренская свита; кунгур

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Литература


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DOI: http://dx.doi.org/10.17072/psu.geol.28.6

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