LOW-PRESSURE REGIONAL METAMORPHISM IN THE OMEO METAMORPHIC COMPLEX, VICTORIA, AUSTRALIA

The Omeo Metamorphic Complex forms the southern end of the Wagga Metamorphic Belt, which is the main locus of Palaeozoic low‐pressure metamorphism in the Lachlan Fold Belt, south‐eastern Australia. It comprises metamorphosed Ordovician quartz‐rich turbidites originally derived from Precambrian cratonic rocks. Prograde regional metamorphism occurred in the early Silurian, very soon after sedimentation had ceased. The sequence of metamorphic zones, with increasing grade, is: chlorite, biotite, cordierite, andalusite–K‐feldspar and sillimanite–K‐feldspar. Migmatites occur in the sillimanite–K‐feldspar zone, but large bodies of S‐type granite were derived from rocks underlying the exposed Ordovician sequence. P and T estimates for the highest grade rocks are T= 700°C and P= 3.5 kbar, indicating a very high P–T gradient of 65°C/km. The high heat flow during prograde metamorphism probably resulted from a combination of a thermal anomaly persisting from a pre‐metamorphic back‐arc basin environment, and intrusion of hot, mantle‐derived magmas into the lower and middle crust. Regional retrograde metamorphism coincided with a general reheating of the crust in the Siluro‐Devonian, accompanied by intrusion of many I‐type plutons and resetting of the K–Ar dates of some earlier plutons. The Omeo Metamorphic Complex was exposed to erosion at this time. Copyright © 1990, Wiley Blackwell. All rights reserved