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anticlinal structure, plunging to the east, but rising and broadening to the west. On the flat crest of the  tructure, there is probable closure in two places. The thickness of the Tertiary sediments may be a maximum of 6,000 feet, but may be only 3,000 feet on the crest of the structure and 4,000 feet on the flanks.</gco:CharacterString>
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