The maximum temperature from hornblende-plagioclase thermometer is $816 C, which probably reflects late-stage crystallisation of the magma.HP Print and Scan Doctor (formerly HP Scan Diagnostic Utility) helps HP printer users quickly and easily diagnose and resolve various printing as well as scanning problems and even connectivity errors. The highest temperature for the rocks comes from orthopyroxene-clinopyroxene solvus thermometry, and is $1000 C this is interpreted to reflect the initial crystallisation of the diorite magma immediately after its em-placement. Several geothermometers have been applied to the Quarry Diorite, the outermost intrusion of the complex. Thermometry, using ternary and binary feldspar systems, yields low temperatures, which probably reflect late-stage, post-magmatic re-equilibration of these minerals. Application of Al-in-hornblende barometry and crossite contents of amphiboles indicates a pressure <3 kbar for the intrusion, in good agreement with published independent pressure estimates of $2 kbar from mineral equilibria in metasedimentary hornfelses in the Etive thermal aureole. Six samples, representing the major rock units in the southern parts of the Etive complex were chosen for mineral chemical studies and for estimation of the pressure and temperature conditions of magmatic crystallisation. The Etive complex, one of the Caledonian 'Newer Granites' of Scotland, is a ring complex of Devonian age, ranging in composition from pyroxene-diorite to leucogranite.
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