stripes
This is the most southerly of the Franspoort line of intrusions and comprises an oval plug of foyaite having a maximum diameter of 1.6 km. The foyaite is composed of 5 mm-long prisms of microperthite, euhedral nepheline (1-3 mm), aegirine prisms with diopsidic cores, as well as rosettes of aegirine needles within analcime, sodalite and purple fluorite. An analysis is given by Shand (1922). Numerous inclusions of monchiquite and ijolite occur in the foyaite and it is traversed by dykes of monchiquite and foyaite. Around the northern margin are poorly exposed trachytic and phonolitic lavas which are intruded by the foyaite.
HARMER, R.E. 1985. Rb-Sr isotopic study of units of the Pienaars River alkaline complex, north of Pretoria, South Africa. Transactions of the Geological Society of South Africa, 88: 215-23.SHAND, S.J. 1922. The alkaline rocks of the Franspoort line, Pretoria district. Transactions of the Geological Society of South Africa, 25: 81-100.