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transcurrent fault |
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transcurrent fault [¦tranz¦kə·rənt ′fȯlt] (geology) A strike-slip fault characterized by a steeply inclined surface. Also known as transverse thrust. 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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