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The Thickness of the Mushy Layer on the Floor of the Skaergaard Magma Chamber at Apatite Saturation

Accepted version
Peer-reviewed

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Authors

Holness, MB 
Tegner, C 
Nielsen, TFD 
Charlier, B 

Abstract

We present a novel way of constraining the thickness of the crystal mush in fractionated layered intrusions using detailed microstructural analysis. The results are combined with geochemical data to create a snapshot of the crystal mush on the floor of the Skaergaard magma chamber in the period immediately before and after the saturation of the bulk liquid in apatite (the UZa–b boundary). The step-change in the fractional latent heat (that part of the total enthalpy budget associated with crystallization) accompanying the arrival of a new liquidus phase is recorded by a step-change in the median clinopyroxene–plagioclase–plagioclase dihedral angle, Θcpp, in fully solidified cumulates. Dihedral angles are formed during the last stages of solidification and hence the change of Θcpp associated with apatite-in marks a point close to the base of the mushy layer at the moment the bulk liquid became saturated in apatite, whereas the first appearance of abundant, homogeneously scattered, cumulus apatite crystals in the stratigraphy marks the top of the mushy layer at this moment. Comparison of the offset between these two markers in five widely spaced drill cores through the Skaergaard Layered Series suggests that the mushy layer was only a few metres thick at the UZa–b boundary in the centre and east of the floor, whereas it was ∼100 m thick on the floor near the western margin. There is no correlation between the efficiency of liquid expulsion (as recorded by bulk-rock P2O5 concentrations and the stratigraphic distribution of reactive symplectites) and the recorded mush thickness at the moment of apatite saturation, suggesting that existing models of adcumulate formation that depend on mush thickness need to be reconsidered.

Description

Keywords

microstructure, cumulate, mush thickness, layered intrusion, dihedral angle

Journal Title

Journal of Petrology

Conference Name

Journal ISSN

0022-3530
1460-2415

Volume Title

58

Publisher

Oxford University Press
Sponsorship
Natural Environment Research Council (NE/F020325/1)
Natural Environment Research Council (NE/J021520/1)
Royal Society (unknown)
Natural Environment Research Council (NE/N009894/1)
M.B.H. and C.T. acknowledge support from a Royal Society Joint International Grant. M.B.H. was supported by the Natural Environment Research Council (grant numbers NE/F020325/1 and NE/J021520/1). C.T. was supported by the Carlsberg Foundation, the Danish Council of Independent Research, and the Danish National Research Foundation.