CFB events are temporally associated to the greatest paleoenvironmental events of the last 300 Myr. SO2 is considered the main cause of environmental change during CFB events. Paranà-Etendeka province is not associated to any en-vironmental perturbation. In order to understand the role of SO2 is necessary to quantify the SO2 emitted during the Paranà- Etendeka magmatism. A new method has been proposed for determing the pre-eruptive S content of Parana lavas, hing-ing on augites. Several augites from Paranà basalts have been selected and ana-lyzed with electronic microprobe and syncrotrone. In this work, electron micro-probe results are described and discussed.

Analisi elementi maggiori e S in augiti di basalti del Paraná: implicazioni paleoambientali

Piccolo, Andrea
2012/2013

Abstract

CFB events are temporally associated to the greatest paleoenvironmental events of the last 300 Myr. SO2 is considered the main cause of environmental change during CFB events. Paranà-Etendeka province is not associated to any en-vironmental perturbation. In order to understand the role of SO2 is necessary to quantify the SO2 emitted during the Paranà- Etendeka magmatism. A new method has been proposed for determing the pre-eruptive S content of Parana lavas, hing-ing on augites. Several augites from Paranà basalts have been selected and ana-lyzed with electronic microprobe and syncrotrone. In this work, electron micro-probe results are described and discussed.
2012-03-03
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.12608/17083