Magmatic differentiation by means of segregation and diapiric ascent of anorthositic crystal mush - the Murotomisaki Gabbroic Complex, Shikoku, Japan

Abstract

The Murotomisaki Gabbro is a sill like layered igneous complex that contains several layers of olivine enrichment. In our previous paper (Hoshide et al, 2006), we have identified two zones of olivine enrichment: 'the crystal accumulation zone (AC zone)', formed by gravity settling and accumulation of olivine crystals, and 'the crystal growth zone (GR zone)', in which increase of modal olivine was caused by crystal growth of olivine and not by crystal accumulation.Based on whole rock compositional data, we have found that the AC zone rocks define a linear compositional trend (termed as 'AC trend') which is consistent with the crystal settling and accumulation hypothesis. However the GR zone data define another linear trend with a slope different from that of the AC trend. Moreover, the compositions of the coarse gabbros and the upper olivine gabbros that occur above the GR zone and an anorthosite vein from the GR zone roughly lie on the same trend, but on the opposite side of the GR zone composition, defining the 'GR trend' as a whole. Some anorthositic veins and wavy pegmatitic veins have plume like structures, suggesting that these veins are remnant of crystal mushes that have been mobilized and ascended diapirically during magmatic differentiation.Considering the observed compositional relationships and the mode of occurrences of the anorthosite and wavy pegmatitic veins, we conclude that the segregation and separation of anorthositic material out of semi solidified crystallization boundary layers was responsible for the formation of the GR zone and the GR trend. Phase equilibrium calculations reveal that the hypothetical anorthosite material was a mixture of fractionated melt and plagioclase crystals that precipitated from the melt. The GR zone represents a residue from the separation of anorthositic crystal mushes and the coarse gabbros and the upper olivine gabbro parts represent mixtures of the crystal mush and the initial melt.

Anorthosites in Nishiyama volcanic products from the Hachijo–jima island, Izu–Bonin arc: The direct evidence for ‘plagioclase control’ in shallow magma reservoir

“…In this region, such anorthositic enclaves, which could be the direct evidence A d v a n c e P u b l i c a t i o n A r t i c l e of plagioclase accumulation, were not found in previous studies. In addition, the production of anorthosites has rarely been reported in subalkaline volcanic rocks though anorthosites were found from some alkalic intrusive layered rocks (e.g., Suwa, 1976;Czamanske and Bohlen, 1990;Akatsuka et al, 1999;Hoshide et al, 2006;Cawthorn and Ashwal, 2009;Maier et al, 2016;McCarthy and Müntener, 2016). In this paper, we report the occurrence of anorthositic enclaves and the attendant petrographic characteristics, while the genetic relationships between the host magma composition and the anorthositic enclaves are also discussed.…”

Zoning and resorption of plagioclase in a layered gabbro, as a petrographic indicator of magmatic differentiation

“…Anorthosite has strong crystal shape fabrics, with plagioclase crystals aligned parallel to the wavy contacts (see also fig. 3B in Hoshide et al 2006b). Some anorthositic layers have thin discontinuous basal layers of medium-grained mafic rocks (olivine grain size: about 2-3 mm in length), like the picritic floor of the podiform gabbroic pegmatite, implying its genetic link with podiform gabbroic pegmatites (Fig.…”

“…Types A or B) cannot be found in the Upper Zone, the source of these plagioclases must be sought in the Lower Zone. Occurrence of the Type-B and B# plagioclase in the Middle Zone may be understood by considering the diapirism of anorthositic crystal mushes generated from the GR subzone below, as advocated by Hoshide et al (2006b). In the samples containing Type-B and B# plagioclase, the Ancontents of plagioclase cores have a wide range amongst the different grains within one sample.…”