R. Almeev results 11
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Hydrous equilibrium crystallization experiments were conducted on two boninitic melt compositions, low-Si boninite (LSB) and high-Si boninite (HSB), from the Izu-Bonin-Mariana (IBM) fore-arc to constrain the evolution of magma storage conditions and differentiation during subduction initiation. Experiments were performed at temperatures between 1020 and 1220 °C and at pressures of 200 and 400 MPa. Additionally, 14 natural boni...
Formation mechanisms of macroscopic globules in andesitic glasses from the Izu–Bonin–Mariana forearc (IODP Expedition 352)NARA Subscribed
The Izu–Bonin–Mariana volcanic arc is situated at a convergent plate margin where subduction initiation triggered the formation of MORB-like forearc basalts as a result of decompression melting and near-trench spreading. International Ocean Discovery Program (IODP) Expedition 352 recovered samples within the forearc basalt stratigraphy that contained unusual macroscopic globular textures hosted in andesitic glass (Unit 6, Hole...
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