CO2 fluid inclusion barometry in mantle xenoliths from central Mexico: A detailed record of magma ascent
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- 作者：Gilles Levressea ; glevresse@geociencias.unam.mx" class="auth_mail" title="E-mail the corresponding author ; Karina Elizabeth Cervantes-de la Cruza ; José ; Jorge Aranda-Gó ; meza ; Marí ; a Guadalupe Dá ; valos-Elizondoa ; Sergio Jimé ; nez-Sandovalb ; Francisco Rodrí ; guez-Melgarejob ; Leticia Araceli Alba-Aldavec
- 关键词：Maar ; Xenoliths ; P&ndash ; T evolution ; Fluid inclusions barometry ; Mexico
- 刊名：Journal of Volcanology and Geothermal Research
- 出版年：2016
- 出版时间：15 January 2016
- 年：2016
- 卷：310
- 期：Complete
- 页码：72-88
- 全文大小：2007 K
文摘
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CO2 pore pressure in fluid inclusions is a valuable proxy to determinate the magma ascent rate and the main transitions in the continental crust
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Chemical equilibrium geobarometers and CO2 pore pressure are complementary techniques to understand mar volcanism emplacement