Summary
Core from the Rookhope borehole and suites of samples from natural outcrops have been used in a detailed investigation of the petrology and chemistry of the Little Whin Sill. Orthopyroxene (Fs
23–27
), plagioclase, clinopyroxene and olivine (Fa
15
) occur as phenocrysts; this is the first report of fresh olivine. The groundmass is composed of clinopyroxene (Ca
45
Mg
51
Fe
4
-Ca
38
Mg
38
Fe
24
), plagioclase (An
70–35
) and iron-titanium ores. Eleven new analyses for major elements are presented, together with a new analysis of the White Whin. Statistical analysis of trace element data suggests that only Mn and Sr show significant variation within a given section across the sill, but these elements and Rb show significant variation between sections. A comparison of the chemistry of the Great and Little Whin Sills suggests that the latter is poorer in SiO
2
, K
2
O, and Rb than the Great Whin Sill but carries more CO
2
. The White Whin, consisting of Ca-Mg-Fe-carbonates, illite, kaolin, plagioclase, anatase and quartz, is shown to be chilled whin to which CO
2
, H
2
O and K
2
O have been added, and from which Na
2
O, CaO, MgO and Fe have been lost. It is suggested that the Little Whin Sill represents the initial magma of the whole Whin Sill complex, the high CO
2
content being a result of later alteration. The chemistry of the whin suite of intrusions has characteristics intermediate between tholeiitic and alkaline dolerites, and the initial magma may itself be a differentiate. Although crystal settling is absent, a trend towards iron enrichment is found, with an insrease in the ratio FeO : Fe
2
O
3
towards the centre of the Little Whin Sill. In addition there may be another trend toward silica enrichment in a lateral direction.
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