All Outputs (3)

Foreland Magmatism during the Arabia–Eurasia Collision: Pliocene–Quaternary Activity of the Karacadağ Volcanic Complex, SW Turkey (2014)
Journal Article
Ekici, T., Macpherson, C., Otlu, N., & Fontignie, D. (2014). Foreland Magmatism during the Arabia–Eurasia Collision: Pliocene–Quaternary Activity of the Karacadağ Volcanic Complex, SW Turkey. Journal of Petrology, 55(9), 1753-1777. https://doi.org/10.1093/petrology/egu040

Pliocene to Quaternary magmatism in the Karacadağ Volcanic Complex in SE Turkey occurred in the foreland region of the Arabia–Eurasia collision and can be divided into two phases. The earlier Karacadağ phase formed a north–south-trending volcanic rid... Read More about Foreland Magmatism during the Arabia–Eurasia Collision: Pliocene–Quaternary Activity of the Karacadağ Volcanic Complex, SW Turkey.

Insights from Pb and O isotopes into along-arc variations in subduction inputs and crustal assimilation for volcanic rocks in Java, Sunda arc, Indonesia (2014)
Journal Article
Handley, H., Blichert-Toft, J., Gertisser, R., Macpherson, C., Turner, S., Zaennudin, A., & Abdurrachman, M. (2014). Insights from Pb and O isotopes into along-arc variations in subduction inputs and crustal assimilation for volcanic rocks in Java, Sunda arc, Indonesia. Geochimica et Cosmochimica Acta, 139, 205-226. https://doi.org/10.1016/j.gca.2014.04.025

New Pb isotope data are presented for Gede Volcanic Complex, Salak and Galunggung volcanoes in West Java, Merbabu and Merapi volcanoes in Central Java and Ijen Volcanic Complex in East Java of the Sunda arc, Indonesia. New O isotope data for Merbabu... Read More about Insights from Pb and O isotopes into along-arc variations in subduction inputs and crustal assimilation for volcanic rocks in Java, Sunda arc, Indonesia.

Assimilation of sediments embedded in the oceanic arc crust: myth or reality? (2014)
Journal Article
Bezard, R., Davidson, J., Turner, S., Macpherson, C., Lindsay, J., & Boyce, A. (2014). Assimilation of sediments embedded in the oceanic arc crust: myth or reality?. Earth and Planetary Science Letters, 395, 51-60. https://doi.org/10.1016/j.epsl.2014.03.038

Arc magmas are commonly assumed to form by melting of sub-arc mantle that has been variably enriched by a component from the subducted slab. Although most magmas that reach the surface are not primitive, the impact of assimilation of the arc crust is... Read More about Assimilation of sediments embedded in the oceanic arc crust: myth or reality?.