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Box Ankle Fault

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Journal Article
Journal: Geology
Published: 01 July 1995
Geology (1995) 23 (7): 621–624.
...Thomas E. West, Jr.; Donald T. Secor, Jr.; John R. Pray; Irene B. Boland; Harmon D. Maher, Jr. Abstract Detailed field mapping at the east end of the Pine Mountain terrane in central Georgia indicates that the Box Ankle fault is an ∼4-km-thick ductile shear zone separating Grenvillian basement...
Journal Article
Journal: Geology
Published: 01 April 1988
Geology (1988) 16 (4): 307–310.
...Robert J. Hooper; Robert D. Hatcher, Jr. Abstract The Pine Mountain terrane is exposed in a complex window within the Piedmont of Georgia and Alabama. The eastern end of the terrane is framed by three ductile faults of demonstrably different ages. The polydeformed pre-thermal peak Box Ankle fault...
Image
Figure 2. Three principal hypotheses on the structure of the Pine Mountain ...
Published: 01 May 2005
at depth smoothly beneath the window with some offset beneath the Towaliga fault ( Hooper and Hatcher, 1988 ). (C) The décollement is presently at or just below the surface and is represented by the Box Ankle fault ( West et al., 1995 ). See text and respective cited papers for further explanation
Journal Article
Journal: GSA Bulletin
Published: 01 May 2005
GSA Bulletin (2005) 117 (5-6): 669–686.
... at depth smoothly beneath the window with some offset beneath the Towaliga fault ( Hooper and Hatcher, 1988 ). (C) The décollement is presently at or just below the surface and is represented by the Box Ankle fault ( West et al., 1995 ). See text and respective cited papers for further explanation...
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Series: GSA Special Papers
Published: 01 January 1988
DOI: 10.1130/SPE222-p185
... reactivated in either the ductile or brittle or both realms, possibly involving both dip-slip and strike-slip motion. The thrusts framing the Pine Mountain and Sauratown Mountains windows formed both pre- and post-thermal peak. The pre-thermal peak Box Ankle thrust in the Pine Mountain window...
Journal Article
Journal: Geosphere
Published: 01 February 2008
Geosphere (2008) 4 (1): 131–144.
... zones. The Bartletts Ferry, Goat Rock, and Box Ankle fault zones have juxtaposed the Uchee terrane with Grenville basement and its stratigraphic cover within the Pine Mountain window ( Figs. 1 and 2 , this paper; Schamel et al., 1980 ; Sears et al., 1981a ; Steltenpohl, 1988 ; Hooper and Hatcher...
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Journal Article
Journal: SEG Discovery
Published: 01 July 2013
SEG Discovery (2013) (94): 1–17.
... fault, which separates the window from the Inner Piedmont, the Box Ankle fault that closes the east end of the window and is truncated by the Towaliga fault, and the Dean Creek and Bartletts Ferry-Goat Rock faults that separate the window from the exotic, peri-Gondwanan Uchee terrane (Carolina...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1989
AAPG Bulletin (1989) 73 (7): 812–840.
... at the updip end of this block depends on seal by the fault on the southwest (closure indicated by asterisk). Transverse closure along the downthrown edge of the center block (indicated by two “X”s), in contrast, would mostly depend on the upturned limb or ankle of a block-edge flexure. Where a high side...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1990
AAPG Bulletin (1990) 74 (10): 1590–1609.
... by short faults and parallel folds that have several, repeated orientations ( Figures 6b , 7b ). (3) The fault has a tightly curving trace and parallels similar faults within a sinuous belt of tight salients and reentrants ( Figure 7c ). Box folds ( Harding, 1985 ) may be cored with upward...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 1988
AAPG Bulletin (1988) 72 (6): 738–757.
..., and important geologic parameters that determine fault seal are illustrated with examples from oil fields in Sumatra and southern California. These fields can be used as models for the recognition and delineation of prospects in other basins. 2 Exxon Production Research Company, P.O. Box 2189, Houston...
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Journal Article
Journal: Geosphere
Published: 01 August 2013
Geosphere (2013) 9 (4): 1044–1064.
... the Inner Piedmont to the northwest, the Box Ankle fault that closes the east end of the window and is truncated by the Towaliga fault, and the Dean Creek and Bartletts Ferry–Goat Rock faults that separate the Pine Mountain window from the Uchee terrane (peri-Gondwanan; Steltenpohl et al., 2008...
FIGURES | View All (5)
Journal Article
Journal: SEG Discovery
Published: 01 July 2013
SEG Discovery (2013) (94): 1–60.
..., ~150 m above the by the Towaliga fault, which separates that are parallel to the resulting folia- the window from the Inner Piedmont, tion (e.g., Pardee and Park, 1948; Stow- more easily eroded surrounding schists. the Box Ankle fault that closes the east ell et al., 1989, 1996). Later deformation end...
Series: Geophysical Developments Series
Published: 01 January 1991
EISBN: 9781560802532
... in Figure 11 shows the conclusion that both extensional fault blocks and divergent wrench assemblages are indicated. At the end of a consultation, a click in the “X” box brings a new menu. There is one more field in this menu than in the “help” menu. The user can choose to save the current consultation...
FIGURES | View All (11)
Journal Article
Journal: SEG Discovery
Published: 01 October 2018
SEG Discovery (2018) (115): 1–48.
... structural geology. These skills are sorely to undertake fieldwork. Project and lacking in many new graduates simply fieldwork. This has the unfortunate because, through no fault of their own, Fellowship applications with a strong they are not taught these skills in their effect that many academics...
Series: Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M34.22
EISBN: 9781862394094
..., showed little folding, and was suggested to be a detached outlier of the main Andes, which had been cut off by faults. The first phase of the exploration ended at Nazca. Fig. 22.2. Map of the route of Gregory's 1931 expedition across Peru from Lima to the fatal Pongo de Mainique gorge on the River...
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Series: Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M34.14
EISBN: 9781862394094
... that it was in this dark gas-lit staircase that Gregory, leading (after the ladies) a party of students upwards, encountered an extinguished gas light. As he had no matches, he turned to the students and asked if any of them had a box of matches. One damsel had one and passed it down to him but he found it difficult...
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