
%0 Journal Article
%A Mason, D.R. 
%T Part 5. Plate boundary evolution in the New Guinea region: Subdivision and geochemistry of tertiary intrusive complexes from part of the New Guinea Mobile Belt
%J Exploration Geophysics
%D 1975/09/01
%V 6
%N 3
%P 69-71
%K 
%R https://doi.org/10.1071/EG975069
%U https://www.publish.csiro.au/paper/EG975069 
%X Within the New Guinea Mobile Belt (Dow et al.,1968), orogeny reached a climax in mid-Miocene times with emplacement of calc-alkaline intrusive complexes and eruption of effusive equivalents (Page, 1971 ). The intrusive rocks have been collectively termed the 'Maramuni Diorite' (Dow et al., 1967, 1968). 
