Copyright 2007 RMaximoNIU. All Rights Reserved.
Previous Works Thesis Project The Process
My area of study will be the Mayon Volcano in Albay Province in the Philippines. Mayon Volcano is one of the most active voclanoes in the Philippines as identified by PHIVOLCS. I will try to unravel the eruptive styles of the volcano by studying its melt inclusions.
Raymond Patrick R. Maximo
R.P.R. Maximo, C.A. Arcilla, L.C. Patino, T.A. Vogel, T.P. Flood, and M.C.B. Arpa, The Geochemistry of Silicic Domes in the Macolod Corridor, Philippines. Proceedings of the XXIII General Assembly, International Union of Geodesy and Geophysics, Royton Sapporo, Hokkaido, Japan. June 30 - July 11, 2003.
G.M. Besana, J.A. Daligdig, N.M. Tuñgol, M.I.T. Abigania, B.J.T. Punongbayan, R.P.R Maximo and M. Ando, The 2003 Earthquake along the Masbate Fault, Philippine Fault Zone, Philippines: Slow Earthquake? Proceedings and Abstract Volume, International Symposium on Slow Slip Events at Plate Subduction, Nagoya University, Japan. March 10-18, 2004.
C.A.Arcilla, R.P.R. Maximo, L.C. Patino, T.A. Vogel, M. Flower, and S. Mukasa, High-Nb Lavas from Northern Palawan: implications for high field strength enrichment in southern Philippine Arc. Proceedings and Abstract Volume, Joint Assembly of EGS-AGU-EUG, Nice, France. April 6-11, 2003.
What are melt inclusions (MI)? They are small blebs of silicate melts that are trapped within phenocrysts at particular magmatic temperatures and pressures. MI's are good trap of magma from degassing. These melt inclusions could contain the relative abundance of volatiles in the magma prior to eruption.
Running away from a crumbling lava with the samples.
Electron Probe Micro-analyser (EPMA)
Photomicrographs of quartz phenocrysts showing general characteristics of silicate-melt inclusions in lavas. a) Silicate-melt inclusion with negative crystal shape (bipyramidal habitus). The inclusion consists of glass, a bubble and a small daughter mineral present beside the gas bubble; from the Mt. Doré (J.L.R. Touret, private collection). b) Silicate-melt inclusions in quartz from the Mt. Doré (J.L.R. Touret, private collection). One inclusion consists of glass and various bubbles (indicated with a black arrow). Others are bubble-free (indicated with an empty arrow). c) Fluid-rich silicate-melt inclusion, which contains three large gas bubbles. This feature may be interpreted as trapping of a fluid saturated magma; from Mt. Amiata (Italy). d) Glassy bubble-free silicate-melt inclusion; the inclusion formed during trapping of a solid inclusion; from the Mt. Doré (J.L.R. Touret, private collection).