Thermal effects of massive CO2 emissions associated with subduction volcanism

Large volumes of CO2 are emitted during volcanic activity at convergent plate boundaries, not only from volcanic centres. Their C isotopic signature indicates that this CO2 is mainly derived from the decarbonation of subducted limestones or carbonated metabasalts, not as often admitted from magma de...

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Veröffentlicht in:	Comptes rendus. Geoscience 2004-09, Vol.336 (12), p.1053-1059
1. Verfasser:	SCHUILING, Roelof D
Format:	Artikel
Sprache:	eng
Schlagworte:	Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Igneous and metamorphic rocks petrology, volcanic processes, magmas
Online-Zugang:	Volltext
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