The structure contours of the Calico sequence boundary in the Kaiparowits Plateau, southern Utah (csbstrc*g)
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This is a polygon coverage of the structure contours of the
Calico sequence boundary in the Kaiparowits Plateau,
southern Utah. Sequence boundary elevations are based on 166
drill sites. The Calico sequence boundary occurs from 50-100
ft below the base of the John Henry Member, therefore an
inferred elevation of the sequence boundary was used at
numerous locations along the outcrop where the John Henry
Member was mapped.
The outside polygon defines the base of the coal-bearing
Calico and A-sequences of the Straight Cliffs Formation east
of 112 degrees of longitude. The northern boundary is
delineated by the Paunsaugunt fault and volcanic rocks of
Tertiary age.
创建时间：
2016-10-29
