Evaluation of gate valve performance
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North-trending anticlines and synclines are the dominant structures in the area. The major portion of the range is an asymmetrical syncline that plunges gently to the south. Several small scale folds on the east side of the area have been overturned to the east. The rocks were deformed both prior to and following the deposition of the Newark Canyon Formation. Numerous normal faults, many of which are transverse to the trend of the folds, and a reverse fault have displaced the folded rocks.
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