Artificial juvenile pyroclasts from wet and dry “eruptions”: impact of magma composition on grain sizes and particle shapes.

We concur with Mandler and Elkins-Tanton (2013) that the melting of the cumulates formed during the cooling of the magma ocean cannot be the parental melts of both diogenites

This study stresses the importance of both intrusive rates and pulse sizes on the spatial and temporal characteristics of magma chambers, and so on the relationship between

dyke thickness depends on the magma viscosity , the density difference between country rocks 17. and magma , the gravitational acceleration g , the dyke horizontal extent B and

Rates of magma transfer in the crust: Insights into magma reservoir recharge and pluton growth.. Thierry Menand, Catherine Annen, Michel de

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des

We consider time periods when significant magma accumulation is known to have occurred at these volcanoes: From September 1977 to January 1983 at Kilauea volcano, the 1975–

From  cosmos  to  cosmopolitics.  The  last  layer  of  our  list  is  by  far  the  trickiest.  Its  understanding  requires  abandoning  one  of  the 

Plot of Fe 3+ /  Fe ratio determined by Fe K-edge XANES spectroscopy compared with calculated entrapment pressures (Oppenheimer et al., 2011) for each melt