Structural evolution of the southeastern portion of the Anadarko Basin region

Perry, William J., Jr.

Abstract:

Field investigations in the Lake Classen-Turner Falls, Oklahoma, area of the northern Arbuckle anticline, on the southeastern margin of the Anadarko basin, indicate that transpressional (oblique compressional) deformation of Late Pennsylvanian age dominated the structural development of this area. The Arbuckle anticline is detached along the NW -trending, SW -dipping, left-reverse Arbuckle fault and is thrust obliquely onto the margin of the Tishomingo block to the east. Paleostress analysis of slip lines on mesoscopic faults along the northeastern limb of the Arbuckle anticline, associated in style and geometry with oblique Arbuckle thrusting, indicates compression directed N. 35-60° E.

Genre:

Book chapter

ProdID:

70044329

Citation Author:

Perry, William J., Jr.

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Citation Language:

English

Citation Larger Work Title:

Anadarko Basin symposium, 1988 (Circular 90)

Citation LatN:

37.0

Citation LatS:

33.62

Citation LonE:

-94.43

Citation LonW:

-103.0

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Citation Phsyical Description:

1 p.

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Citation Public Comments:

Proceedings of a symposium held April 5-6, 1988, at Norman, Oklahoma; cosponsored by the Oklahoma Geological Survey and the U.S. Geological Survey

Citation Publisher:

Oklahoma Geological Survey

Citation Series:

Circular

Citation Series Code:

CIR

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Citation Search Results Text:

Structural evolution of the southeastern portion of the Anadarko Basin region; 1989; Book chapter; CIR; 90; Other Government Series; Anadarko Basin symposium, 1988 (Circular 90); Perry, William J., Jr.