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Core of a syncline (concave up fold) in Miocene (24-5 million years) sandstone and shale from the western Tarim Basin, China.

Core of a syncline (concave up fold) in Miocene (24-5 million years) sandstone and shale from the western Tarim Basin, China.

Douglas Burbank, Director
Bradley Hacker, Associate Director

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page last modified on: 2006-10-17

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