Abstract
Continental flood basalts undergo crystallization at a variety of pressures in the crust and sometimes even in the
mantle. Polybaric fractionation, when magmas may pause and undergo crystallization at different pressures, results in
complex fractionation of major elements. Crystallization at high pressures where clinopyroxene is an early crystallizing
phase can result in erupted compositions that have major element characteristics which mimic those expected for
melts derived from pyroxenite-rich sources. The trace element compositions of early-crystallizing olivine can add
further detail to crystallization histories and potentially allow an examination of the crystallization of basalts from melt
segregation to the surface. The North Atlantic Igneous Province (NAIP) comprises sub-regions which had diverse
crystallization histories. Plateau basalts of the British Palaeogene Igneous Province (BPIP) were generated by partial
melting of mantle peridotite starting at ~3.8 GPa with melting ceasing by ~2.7 GPa. Major elements indicate that some
basalts crystallized at <1 GPa with plagioclase joining the liquidus before clinopyroxene. However, the majority of
BPIP magmas crystallized clinopyroxene before plagioclase feldspar over the pressure range 1.0-2.0 GPa. Trace
elements in olivine indicate crystallization of olivine + clinopyroxene over the pressure interval 1.6-2.0 GPa. However,
olivine data also show that some near-primary magmas reached near-surface pressures without substantial
modification by fractional crystallization. Olivines formed at ≥1.6 GPa have Ni and Ca contents that are consistent with
an origin by partial melting of mantle peridotite with no role for pyroxenite being detected. This contrasts with the low
pressure dominated crystallization histories exhibited by lavas from West Greenland and Iceland. Whole-rock data for
many BPIP lavas exhibit CaO depletion at a given MgO content compared with those from West Greenland and
Iceland, which might be cited as an indicator of pyroxenite in their source, but this is solely a consequence of augite
fractionation at depth. An absence of augite phenocrysts in lavas may have resulted either from augite crystallization in
the mantle or from a change from augite saturation to under-saturation with decreasing pressure, and consequent
augite dissolution. The lack of any significant contribution from recycled oceanic crust to magmatism in the NAIP
suggests that the petrological structure of the mantle source from which NAIP lavas were derived does not conform
with the generally accepted models for mantle plumes such as those responsible for magmatism in Hawaii and the
Siberian Traps.
Original language | English |
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Pages (from-to) | 51-67 |
Number of pages | 17 |
Journal | Earth Science Reviews |
Volume | 176 |
Early online date | 6 Oct 2017 |
DOIs | |
Publication status | Published - Jan 2018 |
Bibliographical note
Data set https://data.mendeley.com/datasets/3psjbpjb3r/draft?a=04945c5fa324-478b-9bb1-061c8c5f0808Acknowledgements: Prof. Claude Herzberg is thanked for a thoughtful, critical and technical review of this manuscript. John Millett is thanked for his comments on earlier drafts of the paper. Members of the NAIP workshops at Durham University provided significant background information and a context for this study.
Keywords
- Continental flood basalts
- polybaric fractional crystallization
- olivine chemistry
- pyroxenite
- model primary magmas