| Abstract: | Cordierite-bearing, hypersthene-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. |
| Genre: | Article |
| ProdID: | 70010519 |
| Citation Author: | Ford, A. B.; Aaron, J. M. |
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| Citation End Page: | 752 |
| Citation Issue: | 3532 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 2 |
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| Citation Search Results Text: | Bedrock geology of the thiel mountains, Antarctica; 1962; Article; Journal; Science; Ford, A. B.; Aaron, J. M. |
| Citation Start Page: | 751 |
| Citation Volume: | 137 |
| Citation Year: | 1962 |
| Type: | citation/reference |
| Text: | Bedrock geology of the thiel mountains, Antarctica; 1962; Article; Journal; Science; Ford, A. B.; Aaron, J. M. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Mon, 1 Jan 1962 00:00 -0600 |
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