The distribution patterns of clay and non-clay minerals has been studied for 30 samples from sediments NW of Zocca, using XRD and volumetric CO 2 analyses. Dioctahedral smectites are abundant and there are high volcanogenic cristobalite contents; serpentine is constantly present due to the erosion of serpentinized ophiolitic rocks during the time of deposition of these pelitic sediments
Studio mineralogico delle porzioni pelitiche nelle Marne di Antognola della zona di Zocca (Modena)
PINI, GIAN ANDREA
1981-01-01
Abstract
The distribution patterns of clay and non-clay minerals has been studied for 30 samples from sediments NW of Zocca, using XRD and volumetric CO 2 analyses. Dioctahedral smectites are abundant and there are high volcanogenic cristobalite contents; serpentine is constantly present due to the erosion of serpentinized ophiolitic rocks during the time of deposition of these pelitic sedimentsFile in questo prodotto:
Non ci sono file associati a questo prodotto.
Pubblicazioni consigliate
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
