--> Abstract: Paleomagnetic Orientation of Fractures and Bedding in Rotliegende and Zechstein Cores from the Southern Permian Basin, North Sea, by D. R. Van Alstine and J. E. Butterworth; #90990 (1993).

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VAN ALSTINE, DAVID R., and JOSEPH E. BUTTERWORTH, Applied Paleomagnetics, Inc., Redmond, WA, and Emeryville, CA

ABSTRACT: Paleomagnetic Orientation of Fractures and Bedding in Rotliegende and Zechstein Cores from the Southern Permian Basin, North Sea

Fractures and bedding in Rotliegende sandstone and Zechstein dolomite cores of the southern Permian Basin can be accurately oriented using our standard paleomagnetic core-orientation technique. In recent projects involving vertical, deviated, and horizontal wells, we have paleomagnetically oriented 1874 ft of Rotliegende and Zechstein cores from 113 intervals ranging in length from 8 in. to 119 ft.

Accuracy of our paleomagnetic core-orientations can be demonstrated by (1) consistency in fracture patterns derived from vertical and horizontal cores near the same reservoir location, (2) consistency in Rotliegende paleowind directions derived from paleomagnetically oriented cores with paleowind directions derived from mechanically oriented cores from the southern Permian Basin, and (3) agreement between structural dip determined from paleomagnetically oriented interdune bedding planes with structural dip determined from paleomagnetically oriented strike-parallel, strike-perpendicular, and bedding-plane fractures.

Paleomagnetic orientation of Rotliegende cores can be especially cost effective. Excellent core recovery and use of long core barrels in the Rotliegende means that "continuous intervals" (defined as the maximum lengths of core that can be reliably reconstructed by fitting adjacent core pieces) of more than 100 ft long can be achieved by following our recommended core-handling procedures. We statistically average the same number of paleomagnetic plug samples regardless of the length of a "continuous interval."

The paleomagnetic signals in Rotliegende sandstone and Zechstein dolomite are sufficiently stable that fractures and bedding can be paleomagnetically oriented even in slabbed cores drilled decades ago.

AAPG Search and Discovery Article #90990©1993 AAPG International Conference and Exhibition, The Hague, Netherlands, October 17-20, 1993.