The petrogenesis of volcanics from Mt. Bulusan and Mt. Mayon in the Bicol arc, the Philippines

• Published in: Contributions to mineralogy and petrology 2005-12, Vol.150 (6), p.652-670
• Main Authors: McDermott, Frank, Jr, Francisco G. Delfin, Defant, Marc J., Turner, Simon, Maury, Rene
• Format: Article
• Language: English
• Subjects: Archipelagoes; Calderas; Earth Sciences; Geochemistry; Mineralogy; Petrology; Pliocene; Sciences of the Universe; Silica; Volcanic rocks; Volcanoes
• ISSN: 0010-7999; 1432-0967
• DOI: 10.1007/s00410-005-0042-7

Pliocene to recent volcanic rocks from the Bulusan volcanic complex in the southern part of the Bicol arc (Philippines) exhibit a wide compositional range (medium- to high-K basaltic-andesites, andesites and a dacite/rhyolite suite), but are characterised by large ion lithophile element enrichments and HFS element depletions typical of subduction-related rocks. Field, petrographic and geochemical data indicate that the more silicic syn- and post-caldera magmas have been influenced by intracrustal processes such as magma mixing and fractional crystallisation. However, the available data indicate that the Bicol rocks as a group exhibit relatively lower and less variable 87Sr/86Sr ratios (0.7036-0.7039) compared with many of the other subduction-related volcanics from the Philippine archipelago. The Pb isotope ratios of the Bicol volcanics appear to be unlike those of other Philippine arc segments. They typically plot within and below the data field for the Philippine Sea Basin on 207Pb/204Pb versus 206Pb/204Pb and 208Pb/204Pb versus 206Pb/204Pb diagrams, implying a pre-subduction mantle wedge similar to that sampled by the Palau Kyushu Ridge, east of the Philippine Trench. 143Nd/144Nd ratios are moderately variable (0.51285-0.51300). Low silica (