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flow banding |
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flow banding [′flō ‚band·iŋ] (geology) An igneous rock structure resulting from flowing of magmas or lavas and characterized by alternation of mineralogically unlike layers. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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| These fractures appear to be the result of flow banding and, although this unit has been included in the Cretaceous Lancones Formation, the authors believe that the well preserved features could indicate a younger age. |
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