Two episodes of deformation at Mt. Madison, Antarctica general they strike to the northeast and dip steeply northwest or southeast. In rare instances fold closures can be seen in the S foliation (figure 2). They are tigh

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Date: 2011-05-06 06:32:17 Metamorphic petrology Crenulation Fold Glacier Foliation Geology Structural geology Metamorphic rocks		Two episodes of deformation at Mt. Madison, Antarctica general they strike to the northeast and dip steeply northwest or southeast. In rare instances fold closures can be seen in the S foliation (figure 2). They are tigh Add to Reading List Source URL: s3.amazonaws.com Download Document from Source Website File Size: 2,71 MB Share Document on Facebook