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Sycamore Creek Fault

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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1980
AAPG Bulletin (1980) 64 (2): 221–241.
... rocks are less well developed but also appear to overlie basement faults. A distinctive monocline trends northwest-southeast from east Val Verde through northwest Kinney Counties, approaching parallelism with the Balcones fault zone In the southeastern part. This flexure, the Sycamore Creek monocline...
FIGURES | View All (15)
Image
—Relation of key surface and subsurface structural features from  Figures 9...
Published: 01 February 1980
FIG. 12 —Relation of key surface and subsurface structural features from Figures 9 and 10 . Sycamore Creek monocline and Carta Valley fault zone show close coincidence to underlying faults. Linear trend of surface fault zone suggests that east-west-trending basement fault may not actually
Image
Slip tendency plot for best fit stress inversion from small displacement fa...
Published: 01 November 2014
Figure 9 Slip tendency plot for best fit stress inversion from small displacement faults at Sycamore Creek pavement study location, performed using the technique of McFarland et al. ( 2012 ) and 3DStress® v. 4.0 software.
Image
(A) Cross section along the eastern canyon wall of <span class="search-highlight">Sycamore</span> Canyon, with fo...
Published: 05 July 2018
the fault movement in Sycamore Canyon (red dashed line) shows a gentle slope with ∼460 m of mid-Miocene relief. (B) Cross section through Dry Beaver Creek Canyon with four-fold vertical exaggeration and reconstruction of the Paleozoic–Cenozoic unconformity. The profile was created from the geologic map
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—Migrated seismic profile across wrench-<span class="search-highlight">fault</span> zone in Ardmore basin of Okla...
Published: 01 July 1979
FIG. 6 —Migrated seismic profile across wrench-fault zone in Ardmore basin of Oklahoma demonstrating flower-structure geometry (adapted from unmigrated interpretation by R. F. Gregory and E. C. Lookabaugh, 1973). Msp , Mississippian Springer, Msy , Mississippian Sycamore, and Ooc , Ordovician
Image
Source-rock analysis of Eagle Ford and equivalent Boquillas Formation sampl...
Published: 15 February 2020
samples (Sycamore Creek, Long, and Langtry) are all from within the immediate vicinity of the faults analyzed in this paper and are all immature. Samples from the Iona core are from Sun et al. (2016) . Samples are distinguished as being from either the lower Eagle Ford (LEF) or the upper Eagle Ford (UEF
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Figure 8. Map showing trace (dashed lines) of Shinarump Conglomerate (Trcs)...
Published: 01 November 2001
lava flows, geomorphology of lava-capped mesas, and offset related to reverse movement on the Oak Creek Canyon fault in Laramide time (D is down, U is up). Thicknesses of the conglomerate and elevation of the top contact are shown at preserved localities; isolated position and low elevation
Image
Conceptual illustration of the stress evolution and related brittle faultin...
Published: 01 November 2014
Figure 14 Conceptual illustration of the stress evolution and related brittle faulting and jointing interpreted from the Sycamore Creek pavements study site. σ = normal stress and τ = shear stress. Effective stress was adjusted for pore fluid pressure. Hoek-Brown failure envelopes
Journal Article
Journal: AAPG Bulletin
Published: 01 November 2014
AAPG Bulletin (2014) 98 (11): 2477–2506.
...Figure 9 Slip tendency plot for best fit stress inversion from small displacement faults at Sycamore Creek pavement study location, performed using the technique of McFarland et al. ( 2012 ) and 3DStress® v. 4.0 software. ...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1939
AAPG Bulletin (1939) 23 (5): 625–642.
...Robert H. Cuyler ABSTRACT The Travis Peak formation and its members were named and described by Hill in 1889. At the type locality in Travis County, the formation consists of the Sycamore sands and conglomerates, composing the lowest member, the Cow Creek limestones and shell beds forming...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1922
AAPG Bulletin (1922) 6 (5): 475–476.
... Creek, in Val Verde County. Texas. The structure is an anticline with its axis extending west by north, crossing Sycamore Creek about 2 miles south of the Southern Pacific Railway near Johnstone siding, and extending across San Felipe Creek 3 or 4 miles north of Del Rio. The abnormal eastward extension...
Journal Article
Journal: Geosphere
Published: 05 July 2018
Geosphere (2018) 14 (4): 1690–1709.
... the fault movement in Sycamore Canyon (red dashed line) shows a gentle slope with ∼460 m of mid-Miocene relief. (B) Cross section through Dry Beaver Creek Canyon with four-fold vertical exaggeration and reconstruction of the Paleozoic–Cenozoic unconformity. The profile was created from the geologic map...
FIGURES | View All (12)
Journal Article
Published: 01 August 1989
Bulletin of the Seismological Society of America (1989) 79 (4): 1270–1278.
... of the 1969 to 1988 earthquakes occur in the vicinity of the north-trending faults. A cluster of events apparently associated with a north- trending fault(s) north of the Sycamore Creek fault has a focal mechanism (No. 25) that exhibits a north-trending, right-lateral strike-slip nodal plane, consistent...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1927
AAPG Bulletin (1927) 11 (12): 1307–1320.
... locality, Sycamore Creek, is in western Johnson County. The occurrence of the Sycamore limestone in the Arbuckle Mountains is also peripheral and is just outside the Woodford ridge previously mentioned. It has been described by Taff 2 as a lentil because of its wedge shape. On the southwestern flank...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2007
GSA Bulletin (2007) 119 (11-12): 1347–1367.
... strata and terminate against the Clayton–Marsh Creek fault, which is at a low angle to bedding and is interpreted to be the basal detachment for part of the graben system. The Clayton–Marsh Creek fault in turn is linked to a system of faults that juxtapose blueschist facies rocks of the underlying...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1970
AAPG Bulletin (1970) 54 (5): 758–782.
... of the original “Big Injun” of southwestern Pennsylvania and northern West Virginia. All recently discovered “Big Injun” production in the Vadis-Leading Creek area of Lewis and Gilmer Counties, the Spruce Creek area of Ritchie County, the New Milton and other areas in Doddridge County, and the Sycamore and other...
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Journal Article
Published: 18 July 2019
Journal of Sedimentary Research (2019) 89 (7): 629–653.
...-scale from Ernst Tinaja (in Big Bend National Park), Langtry, Texas, and Sycamore Creek and Pinto Creek on a private ranch near Del Rio, Texas (on the periphery of the Maverick Basin), Super Target in western San Antonio, Texas, and Garden Ridge near Garden Ridge, Texas (on the San Marcos Arch). We...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2018
AAPG Bulletin (2018) 102 (10): 1963–1984.
... end of the Balcones fault system. Similar to the Eagle Ford Formation in the subsurface, the Sycamore Creek pavements are gently dipping to nearly horizontal and exhibit extensional deformation ( Ferrill et al., 2014a ). The Sycamore Creek pavements displayed approximately 1.77 m (5.81 ft...
FIGURES | View All (10)
Image
—Sketch cross sections, showing overturning in surface exposures.   A . Par...
Published: 01 May 1934
°. D . Section across Big Spring Creek in Sec. 28, T. 2 N., R. 6 E., near asphalt deposits, 2 miles northwest of Franks. In bed of creek, Sylvan shale rests on Hunton limestone, dipping south at 80°. South of covered area, members of Simpson group dip north at angles of 10°–20°. Fault can not be seen
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1945
AAPG Bulletin (1945) 29 (2): 187–209.
... member of the formation. In this well it is evident, however, that some of the Viola limestone and possibly as much as 100 feet of the Bromide formation have been cut out by faulting. The Viola group occurs in both the Sulphur and Mill Creek synclines. It is found in four isolated, overlapped...
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