Melt inclusions within forsterite-rich olivine crystals in two mixed magmas from the Indonesia–Australia collision zone provide information on the primary melts formed within this tectonic environment. Although whole rock Sr, Nd and Pb isotope data show a strong influence of subducted continental material, the melt inclusion major and trace element compositions are only subtly different from typical subduction-related magmas. The presence of low-Ca olivine crystals with inclusions of aluminous spinel in one sample can be explained by localised reactions during influx of hot basaltic magma in a partially crystallised magma chamber. The mineralogy of the samples is similar to that of other mixed arc magmas. Major and trace element data for re...
Ijen Volcanic Complex (IVC) in East Java, Indonesia is situated on thickened oceanic crust within th...
The Mariana arc forms part of the 2500 km Izu–Bonin–Mariana arc system caused by westward subduction...
Copyright © 2009 Elsevier B.V. All rights reservedMiddle Miocene to Quaternary magmatism in Central ...
Melt inclusions within forsterite-rich olivine crystals in two mixed magmas from the Indonesia–Austr...
Mineral and melt inclusions in olivines from the most Mg-rich magma from the southern West Sulawesi ...
Copyright © 2004 Elsevier B.V. All rights reserved.The islands of Alor, Lirang, Wetar and Romang are...
Copyright © 2006 The AuthorMineral and melt inclusions in olivines from the most Mg-rich magma from ...
Mineral and melt inclusions in olivines from the most Mg-rich magma from the southern West Sulawesi ...
Unravelling the origin of different components contributing to subduction-related magmas is a prereq...
Copyright © 2004 Geological Society of AmericaPb isotopes in igneous rocks from the Banda-Sunda arc ...
This thesis presents the results of a geochemical study of the Banda Arc (East Indonesia) where magm...
This thesis presents the results of a geochemical study of the Banda Arc (East Indonesia) where mag...
Subduction related magmas are characterised by distinctive minor and trace element ratios which are ...
Copyright © 1999 Elsevier Science Ltd. All rights reserved.The South arm of Sulawesi was an active c...
Ijen Volcanic Complex (IVC) in East Java, Indonesia is situated on thickened oceanic crust within th...
Ijen Volcanic Complex (IVC) in East Java, Indonesia is situated on thickened oceanic crust within th...
The Mariana arc forms part of the 2500 km Izu–Bonin–Mariana arc system caused by westward subduction...
Copyright © 2009 Elsevier B.V. All rights reservedMiddle Miocene to Quaternary magmatism in Central ...
Melt inclusions within forsterite-rich olivine crystals in two mixed magmas from the Indonesia–Austr...
Mineral and melt inclusions in olivines from the most Mg-rich magma from the southern West Sulawesi ...
Copyright © 2004 Elsevier B.V. All rights reserved.The islands of Alor, Lirang, Wetar and Romang are...
Copyright © 2006 The AuthorMineral and melt inclusions in olivines from the most Mg-rich magma from ...
Mineral and melt inclusions in olivines from the most Mg-rich magma from the southern West Sulawesi ...
Unravelling the origin of different components contributing to subduction-related magmas is a prereq...
Copyright © 2004 Geological Society of AmericaPb isotopes in igneous rocks from the Banda-Sunda arc ...
This thesis presents the results of a geochemical study of the Banda Arc (East Indonesia) where magm...
This thesis presents the results of a geochemical study of the Banda Arc (East Indonesia) where mag...
Subduction related magmas are characterised by distinctive minor and trace element ratios which are ...
Copyright © 1999 Elsevier Science Ltd. All rights reserved.The South arm of Sulawesi was an active c...
Ijen Volcanic Complex (IVC) in East Java, Indonesia is situated on thickened oceanic crust within th...
Ijen Volcanic Complex (IVC) in East Java, Indonesia is situated on thickened oceanic crust within th...
The Mariana arc forms part of the 2500 km Izu–Bonin–Mariana arc system caused by westward subduction...
Copyright © 2009 Elsevier B.V. All rights reservedMiddle Miocene to Quaternary magmatism in Central ...