Lanterman Range Wilson Gneiss

The comparison of the initial Sr/ Sr ratios in Fig. 4.17 supports the conclusion that the feldspar in the till of the Morozumi Range originated primarily from the Granite Harbor Intrusives (GHI) and not from the Rennick Schist (RS) and the Wilson Gneiss (WG) which are exposed in the Daniels Range and in the adjacent Lanterman and Salamander ranges in Fig. 4.14. 

The K-Ar dates of the Wilson Gneisses of the Lanterman Range in Appendix 4.8.3.12 and in Fig. 4.18 indicate that biotite, muscovite, and hornblende reached their blocking temperature for radiogenic Ar... 

The Salamander Range is located southeast of the Lanterman Range and is separated from the Freyberg Mountains by the upper Canham Glacier. The northern part of the Salamander Range consists of Wilson Gneisses which, in the southernmost part, is overlain by residual outcrops of the Beacon Supergroup and of the Kirkpatrick Basalt. 

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