Calcite pseudomorphs after evaporates from the Muschelkalk (Middle Triassic) of the Holy Cross Mountains (Poland)

• Autorzy: Bodzioch Adam
• Języki publikacji: EN

Abstrakty

EN

Pseudomorphs after sulphate minerals, together with accompanying phenomena, are the only evidence of evaporites in the Muschelkalk of the Holy Cross Mts. They appear as geodes or full-filled nodules built of coarse-crystalline calcite, and their after-evaporite origin have been interpreted on the ground of lithological, petrographical and geochemical characteristics. Evaporitic conditions of sedimentation are indicated mainly by remnants of sulphate minerals occurring commonly in the geodes, and by remnants of dolomite in the host rocks. Dissolution of sulphates, evidenced by collapse breccias, pseudomorphs, and pervasive calcitization of the geodes-bearing horizons, took place in consequence of fresh water influx, which is suggested by elemental and isotopic data.

Słowa kluczowe

EN

sulphates; carbonates; pseudomorphs; Muschelkalk; Świętokrzyskie Mountains

PL

siarczany; węglany; pseudomorfozy; wapień muszlowy; Góry Świętokrzyskie

• Wydawca: Uniwersytet im. Adama Mickiewicza. Instytut Geologii
• Czasopismo: Geologos
• Rocznik: 2003
• Tom: Vol. 6
• Strony: 169--180
• Opis fizyczny: Bibliogr. 30 poz.

Twórcy

autor

Bodzioch Adam

• A. Mickiewicz University, Institute of Geology, ul. Maków Polnych 16, 61-606 Poznań, Poland

Bibliografia

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).