All Outputs (4)

Sub-lithospheric small-scale convection—a mechanism for collision zone magmatism (2014)
Journal Article
Kaislaniemi, L., van Hunen, J., Allen, M., & Neill, I. (2014). Sub-lithospheric small-scale convection—a mechanism for collision zone magmatism. Geology, 42(4), 291-294. https://doi.org/10.1130/g35193.1

We studied the effect of increased water content on the dynamics of the lithosphere-asthenosphere boundary in a postsubduction setting. Results from numerical mantle convection models show that the resultant decrease in mantle viscosity and the perid... Read More about Sub-lithospheric small-scale convection—a mechanism for collision zone magmatism.

Pliocene-Quaternary volcanic rocks of NW Armenia: Magmatism and lithospheric dynamics within an active orogenic plateau (2013)
Journal Article
Neill, I., Meliksetian, K., Allen, M., Navasardyan, G., & Karapetyan, S. (2013). Pliocene-Quaternary volcanic rocks of NW Armenia: Magmatism and lithospheric dynamics within an active orogenic plateau. Lithos, 180-181, 200-215. https://doi.org/10.1016/j.lithos.2013.05.005

The Pliocene–Quaternary volcanic rocks of Armenia are a key component of the Arabia–Eurasia collision, representing intense magmatism within the Turkish–Iranian plateau, tens of millions of years after the onset of continental collision. Here we pres... Read More about Pliocene-Quaternary volcanic rocks of NW Armenia: Magmatism and lithospheric dynamics within an active orogenic plateau.

Small-volume melts of lithospheric mantle during continental collision: late Cenozoic lavas of Mahabad, NW Iran (2013)
Journal Article
Kheirkhah, M., Neill, I., Allen, M., & Ajdari, K. (2013). Small-volume melts of lithospheric mantle during continental collision: late Cenozoic lavas of Mahabad, NW Iran. Journal of Asian Earth Sciences, 74, 37-49. https://doi.org/10.1016/j.jseaes.2013.06.002

Basanites and alkali basalts from Mahabad in the West Azerbaijan province of Iran are part of a widespread series of Late Miocene–Quaternary mantle-derived magmas erupted within the Turkish–Iranian orogenic plateau, itself part of the active Arabia–E... Read More about Small-volume melts of lithospheric mantle during continental collision: late Cenozoic lavas of Mahabad, NW Iran.

Generation of arc and within-plate chemical signatures in collision zone magmatism: Quaternary lavas from Kurdistan province, Iran (2013)
Journal Article
Allen, M., Kheirkhah, M., Neill, I., Emami, M., & Mcleod, C. (2013). Generation of arc and within-plate chemical signatures in collision zone magmatism: Quaternary lavas from Kurdistan province, Iran. Journal of Petrology, 54(5), 887-911. https://doi.org/10.1093/petrology/egs090

New whole-rock and Sr–Nd isotopic analyses of Quaternary lavas from Kurdistan Province, western Iran, shed light on the nature of orogenic plateau magmatism during continental collision and the possible role of accessory minerals during mantle partia... Read More about Generation of arc and within-plate chemical signatures in collision zone magmatism: Quaternary lavas from Kurdistan province, Iran.