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Brush Valley Syncline

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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1982
AAPG Bulletin (1982) 66 (4): 477–482.
... province and the Valley and Ridge province, is 23 mi (37 km) east of the field. Cush Cushion is developed across the Brush Valley synclinal axis in eastern Indiana County. The Conemaugh Group (Penn-sylvanian) is exposed at the surface, and production is from the multistory sandstone reservoirs...
FIGURES
First thumbnail for: GEOLOGIC NOTE: High-Potential Gas Production and F...
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Journal Article
Journal: AAPG Bulletin
Published: 01 September 1981
AAPG Bulletin (1981) 65 (9): 1666.
... province and the Valley and Ridge province, is 23 mi (37 km) east of the field. Cush Cushion is developed across the Brush Valley synclinal axis in eastern Indiana County. The Conemaugh Group is exposed at the surface and production is from the multistory sandstone reservoirs of the Bradford Group (Upper...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1984
AAPG Bulletin (1984) 68 (12): 1920.
... Mine (producing from the lower Freeport coal bed) is experiencing an increase in the number of clastic dikes and associated roof failure as mining advances toward the axis of the Brush Valley syncline. Over 200 individual clastic dikes of claystone matrix with fragments of shale and coal have been...
Image
Structural cross sections across the Valley and Ridge province. Cross-section locations are shown in Figure 1A. Filled red circles are sample locations projected down-plunge from ~15 km on either side of the section. Restored sections (shown below each structural cross section) show the inferred syntectonic overburden (orange shading) and the approximate pre-deformation locations of samples used to determine syntectonic overburden (red filled circles). Also shown are the ranges of calculated overburden for each location based on fluid inclusion microthermometry (Table S1 [see text footnote 1]). Some locations have more than one trapping depth determination. Generalized stratigraphy is shown in Figure 1B. Solid blue unit is the Cambrian–Ordovician lithotectonic unit. Blue line is the top of the Silurian Tuscarora Formation. Red line is the top of the Lower Devonian Oriskany Formation. Brown line is the base of the Mississippian Pocono Group. Purple line is the base of the Pennsylvanian Pottsville Formation. Green in sections 1, 2, and 3 is Silurian Salina Group salt. Screw indicates the foreland pin line. Thrust blocks are numbered in order to relate present overburden determination to the estimated restored position. Sample numbers are keyed to Table S1 (see text footnote 1). C clastic—Cambrian clastic rocks, C-O—Cambrian–Ordovician carbonate rocks, M—Mississippian rocks, MD-UD—Middle to Upper Devonian rocks, P—Pennsylvanian rocks, PC—Precambrian rocks. AVS—Aughwick Valley syncline, BMA—Blue Mountain anticline, BMtA—Backlog Mountain anticline, BS—Bedford syncline, BVA—Brush Valley anticline, CMA—Conococheague Mountain anticline, CS—Clearville syncline, DVA—Decker Valley anticline, ECS—Evitts Creek syncline, MBS—Meadow Branch synclinorium, MGS—Meadow Ground syncline, MMS—Martin Mountain syncline, NLVA—New Lancaster Valley anticline, NMT—North Mountain thrust fault, PVA—Penns Valley anticline, PVNA—Penns Valley Narrows anticline, SHS—Sideling Hill syncline, SVA—Sugar Valley anticline, TA—Tuscarora anticline, THS—Town Hill syncline, TRS—Timber Ridge syncline, TVS—Tuscarora Valley syncline, WMtA—White Mountain anticline, WS—Wellersburg syncline.
Published: 02 March 2023
syncline, BMA—Blue Mountain anticline, BMtA—Backlog Mountain anticline, BS—Bedford syncline, BVA—Brush Valley anticline, CMA—Conococheague Mountain anticline, CS—Clearville syncline, DVA—Decker Valley anticline, ECS—Evitts Creek syncline, MBS—Meadow Branch synclinorium, MGS—Meadow Ground syncline, MMS
Journal Article
Journal: Geosphere
Published: 25 April 2024
Geosphere (2024) 20 (3): 711–734.
... of this cliff face using the drone-based model (section A-A′, Fig. 5 ; Fig. 6 ; Files S2 and S3) is that the isoclinal synform described by Brush et al. (2018) is the lower syncline in an anticline-syncline pair. The syncline encloses the lower Noonday Formation (Sentinel Peak Member) in the Thorndike...
FIGURES
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2011
GSA Bulletin (2011) 123 (1-2): 206–217.
... ). This monotonous stratigraphy precluded identifying stratigraphic marker beds, and thus, a bedding form-line map was the principal product. That initial work showed that there was a prominent anticline-syncline fold pair along the main ridge in an area of good outcrop, together with other subsidiary folds...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1988
AAPG Bulletin (1988) 72 (11): 1297–1322.
... Creek, (3) Grapevine Canyon, (4) Tecuya Creek, (5) Salt Creek, (6) Pleito Creek, (7) Lost Canyon, (8) San Emigdio Canyon, (9) Santiago Creek. DK = Devil’s Kitchen syncline, ERP = Eagle Rest Peak. Dotted line for White Wolf fault indicates approximate subsurface trace of fault. (C) Generalized...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 1934
AAPG Bulletin (1934) 18 (12): 1584–1596.
... or of the flatness of the Powell Valley anticline. FIG. 2. —Topographic and geologic cross section of western part of Cumberland overthrust block along line CD ( Fig. 1 ), showing flat-topped Powell Valley anticline and flat-bottomed Middlesboro syncline; also showing earlier, now disproved, conception...
FIGURES
First thumbnail for: Mechanics of Low-Angle Overthrust Faulting as Illu...
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Journal Article
Published: 01 August 1979
Bulletin of the Seismological Society of America (1979) 69 (4): 1081–1105.
... cast in the form of 382 amplitude ratios between the individual sites. Four of the five ridges (Powell Mountain, Gap Mountain, Bays Mountain, and River Mountain) show amplification at the mountaintops with respect to the valleys. However, one ridge, with a less pronounced crest than the others (Brush...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1932
AAPG Bulletin (1932) 16 (2): 135–143.
... the Santa Maria district and the San Joaquin Valley remained open well into lower Pliocene time. Relatively small thicknesses of strata on anticlines, and greater thicknesses in synclinal areas suggest that submarine folding or faulting, or both, operated in the basin during Pliocene deposition...
FIGURES
First thumbnail for: Lower Pliocene in Santa Maria District, California
Second thumbnail for: Lower Pliocene in Santa Maria District, California
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1924
AAPG Bulletin (1924) 8 (1): 55–60.
...Walter Stalder © 1924 American Association of Petroleum Geologists. All rights reserved 1924 American Association of Petroleum Geologists On the west side of the Salinas Valley in the vicinity of King City, Monterey County, California, is an area of bituminous shale. This is a part...
FIGURES
First thumbnail for: A Section of the Monterey (Salinas) Shales in Pine...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 2021
AAPG Bulletin (2021) 105 (8): 1679–1720.
... to stratigraphic age information provided by boreholes 329D and 723C ( Figures 3 , 5B ). Our age assignments are broadly consistent with, and are thus supported by, regional seismic and stratigraphic data presented in several previous studies (e.g., Modica and Brush, 2004 ; Moreira et al., 2007 ; Contreras et...
FIGURES
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Journal Article
Published: 01 November 2010
Scottish Journal of Geology (2010) 46 (2): 125–142.
...C. J. Vincent; W. J. Rowley; A. A. Monaghan Abstract Synopsis Basin subsidence and thermal history models of the eastern part of the Midland Valley of Scotland have been constructed to characterize the development of the Midlothian-Leven synclinal basin from the mid Mississippian to the present day...
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Journal Article
Published: 01 June 2017
Environmental Geosciences (2017) 24 (2): 95–112.
... folds. The West Middletown Syncline cuts through the eastern section of the park as the axis trends north from Bavington. The Pittsburgh Coal seam outcrops along the stream valleys ( Figure 1 ). Large-scale surface mining of the Pittsburgh coal began in the 1940s when the Harmon Creek Coal...
FIGURES
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... alluvium fills the valley of Brush Creek, and loess caps upland divides. The Volker anticline and Penn Valley syncline trend generally NW–SE across the Brush Creek vicinity. Figure 18. Detailed topographic map of Brush Creek, Country Club Plaza, and Westport vicinity. The Civil War memorial...
Journal Article
Journal: GSA Bulletin
Published: 13 February 2019
GSA Bulletin (2019) 131 (7-8): 1295–1311.
... the Potomac River basin. The Appalachian Plateau is the only physiographic province where sediment export dominates, likely as the result of ongoing relief growth in catchments draining the Appalachian Mountain divide. 10 Be m concentrations measured in the 150 k.y. Hybla Valley sediment core, taken from...
FIGURES
First thumbnail for: Erosion rates and sediment flux within the Potomac...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 June 2012
Lithosphere (2012) 4 (3): 187–208.
... related structures such as the Coal Valley syncline in the south and the Morgan Ranch steep-axis hinge zone in the center. Next, we describe blocks of structurally high basement rock satellite to the main Wassuk Range block in the northeast (pop-up blocks, Fig. 3 ), followed by transverse structural...
FIGURES
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Journal Article
Published: 01 June 2001
Bulletin of Canadian Petroleum Geology (2001) 49 (2): 186–201.
... Syncline), or an erosional surface that in places cuts deeply into the underlying, older Silurian and Ordovician rocks (Northern Outcrop Belt in the Connecticut Valley–Gaspé Synclinorium). The third unconformity is angular and occurs between Middle or Upper Devonian and Carboniferous rocks. It is related...
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Journal Article
Published: 01 January 1999
Jour. Geol. Soc. India (1999) 53 (1): 120–133.
... Copyright © 1999 Geological Society of India 1999 Geological Society of India DISCUSSION DISCOVERY OF LOWER CAMBRIAN SMALL SHELLY FOSSILS AND BRACHIOPODS FROM THE LOWER VINDWIrAN OF SON VALLEY, CENTRAL INDIA by R.J. Azmi, Jour. Geol. Soc. India, v.52, pp.381-389, 1998 J. Swami Nath, M...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1984
AAPG Bulletin (1984) 68 (7): 850–873.
... of the Transverse Ranges of southern California ( Figure 1 ), and separate the Simi Valley from the western part of the San Fernando Valley. Beneath the Simi Valley is a broad westerly plunging synclinal depression with the Upper Cretaceous strata cropping out along the southern limb of the syncline. These strata...
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