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USGS · 70010519

Bedrock geology of the Thiel Mountains, Antarctica

A. B. Ford·J.M. Aaron
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Abstract

Cordierite-bearing, hyper-sthene-quartz monzonite porphyry, the most widespread rock unit, is intruded by biotite granite and porphyritic biotite granite. Sedimentary and metasedimentary rocks, mainly quartzites and argillites, have been metamorphosed locally to hornfels and have been involved in high-angle faulting. Shear zones are common in the plutonic rocks.

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A. B. Ford, J.M. Aaron. 1962. Bedrock geology of the Thiel Mountains, Antarctica. https://doi.org/10.1126/science.137.3532.751

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