|
|||||
|
|
The origin of medium-K ankaramitic arc magmas from Lombok (Sunda arc, Indonesia): Mineral and melt inclusion evidence |
|
| Authors: | Marlina A Elburg VS Kamenetsky JD Foden A Sobolev |
| Institution: | aMax-Planck Institut für Chemie, Postfach 3060, 55020 Mainz, Germany bFaculty of Earth and Life Sciences, Free University, De Boelelaan 1085, Amsterdam, The Netherlands cDepartment of Geology and Soil Science, Ghent University, Krijgslaan 281 S8, 9000 Ghent, Belgium dCentre for Ore Deposit Research and School of Earth Sciences, University of Tasmania, Hobart, Tasmania 7001, Australia eDepartment of Geology and Geophysics, Adelaide University, Adelaide SA 5005, Australia |
| Abstract: | High-calcium, nepheline-normative ankaramitic basalts (MgO > 10 wt.%, CaO/Al2O3 > 1) from Rinjani volcano, Lombok (Sunda arc, Indonesia) contain phenocrysts of clinopyroxene and olivine (Fo85–92) with inclusions of spinel (Cr# 58–77) and crystallised melt. Olivine crystals have variable but on average low NiO (0.10–0.23 wt.%) and high CaO (0.22–0.35 wt.%) contents for their forsterite number. The CaO content of Fo89–91 olivine is negatively correlated with the Al2O3 content of enclosed spinel (9–15 wt.%) and positively correlated with the CaO/Al2O3 ratios of melt inclusions (0.9–1.5). Major and trace element patterns of melt inclusions are similar to that of the host rock, indicating that the magma could have formed by accumulation of small batches of melt, with compositions similar to the melt inclusions. The liquidus temperature of the magma was  1275 °C, and its oxygen fugacity ≤ FMQ + 2.5. Correlations between K2O, Zr, Th and LREE in the melt inclusions are interpreted to reflect variable degrees of melting of the source; correlations between Al2O3, Na2O, Y and HREE are influenced by variations in the mineralogy of the source. The melts probably formed from a water-poor, clinopyroxene-rich mantle source. |
| Keywords: | Arc magma Subduction Ankaramite Melt inclusions Olivine Spinel |
| 本文献已被 ScienceDirect 等数据库收录！ | |