Charnockites could be of magmatic, metamorphic, or metasomatic origin and formed
in diverse geotectonic settings. Previous works on incipient charnockitic rocks
outcropping around Ikare, southwestern Nigeria, were inconclusive due to lack of
micro-chemical data for pressure-temperature estimation. Hence, this present study
was designed to determine the petrology, geochemistry, and pressure-temperature
estimates of these charnockitic rocks. Petrographic studies showed that the essential
minerals are quartz, plagioclase, alkali feldspar, biotite, orthopyroxene and
hornblende ± clinopyroxene. The accessory minerals are zircon, apatite, ilmenite, and
magnetite. Hornblende is stable with orthopyroxene. Plagioclase feldspars in the
charnockite are andesine and be expressed as An35Ab64. Orthopyroxene be
described as Fs57.5En42.5Wo0 are mainly hypersthene. Hornblende in the incipient
charnockite varies from pargasite to ferropargasite in composition. Alkali feldspar is
a microcline. Geothermobarometric computations using both hornblende-plagioclase
and two-feldspar thermometers obtained temperatures ranging from 7400C to 8000C
at assumed pressure of five kbar. The temperature range 8000C recorded on
thermodynamic modeling of a sample, further suggest a low pressure-high
temperature metamorphic conditions for the incipient charnockite around Ikare
Keywords: Magmatic, micro-chemical, geothermobarometric, incipient charnockite,
Ikare
