A correct description and quantification of the geochemical behaviour of REE+ Y (rare earth elements and Y) and HFSE (high field strength elements) is a key requirement for modeling …
Intra-oceanic arcs are typically associated with intermediate (andesitic) cone volcanoes. However, caldera volcanoes may also form in these settings from very large eruptions …
C Sun, M Graff, Y Liang - Geochimica et Cosmochimica Acta, 2017 - Elsevier
Trace element partition coefficients between anorthitic plagioclase and basaltic melts (D) have been determined experimentally at 0.6 GPa and 1350–1400° C in a lunar high-Ti …
Clinopyroxene–liquid geothermobarometry is a widely used tool for estimating the conditions under which mafic magmas are stored before they erupt. However, redox …
Understanding the anatomy of magma plumbing systems of active volcanoes is essential not only for unraveling magma dynamics and eruptive behaviors but also to define the …
Concurrent mixing and crystallization of magmas has been identified in the plumbing of Icelandic magmatic systems from investigation of their erupted products. Thermobarometric …
O Namur, B Abily, AE Boudreau, F Blanchette… - Layered …, 2015 - Springer
Layering is a common feature in mafic and ultramafic layered intrusions and generally consists of a succession of layers characterized by contrasted mineral modes and/or mineral …
NASA's MESSENGER spacecraft has revealed geochemical diversity across Mercury's volcanic crust. Near-infrared to ultraviolet spectra and images have provided evidence for …
Dichotomous high-Ti and low-Ti magmas are ubiquitous in large igneous provinces (LIPs). These magmas often form economically critical Fe–Ti oxide ores in layered intrusions via …