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Greendale Syncline

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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1957
AAPG Bulletin (1957) 41 (4): 643–655.
...W. D. Lowry ABSTRACT Abnormally great thicknesses of Paleozoic sediments in the Massanutten and Greendale synclines in western Virginia indicate that gentle folding accompanied sedimentation. This folding was underway in Ordovician time. The major disconformity between Lower and Middle Ordovician...
FIGURES | View All (7)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1979
AAPG Bulletin (1979) 63 (9): 1577.
..., to evaluate rationales and optimize local geologic factors in site selection. The development of seven exploration prospects associated with the Newman Ridge and Greendale synclines in eastern Tennessee and southwestern Virginia illustrates EGSP’s exploration strategy. © 1979 American Association...
Image
—Data for comparison purposes plotted on conventional base map of central Appalachians. Compare this map with Figures 8 and 9. Map shows generalized isopachs for Huntersville Formation (chert) of “Onondagan” age. Note also position of three important basins: Massanutten, Salem, and Greendale synclines.
Published: 01 April 1963
, and Greendale synclines.
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1982
AAPG Bulletin (1982) 66 (8): 1167.
... in the Greendale syncline in southwestern Virginia. Subsurface mapping clearly outlines an arcuate area from western New York through northwestern Pennsylvania, eastern Ohio, and western West Virginia to southwestern Virginia, in which the black shales are laterally continuous. Presumably, depositional...
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1982
AAPG Bulletin (1982) 66 (8): 1165.
... Grove gas field was developed on an anticlinal flexure within the Greendale syncline. The field produced gas from porous anhydrite beds in the Lower Mississippian Little Valley Formation until shut-in in 1957. Five new wells since March 1980 have encountered near-virgin pressures in the old Little...
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1974
AAPG Bulletin (1974) 58 (9): 1892–1893.
... contains four morphostructural zones, from northwest to southeast, the folded foreland (southeastern Appalachian Plateau), the frontal imbricates (Nittany anticlinorium, Wills Mountain-Friends Cove anticlinorium), the interthrust syncline (Broadtop synclinorium, Greendale-Kimberling syncline) and the back...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1977
AAPG Bulletin (1977) 61 (3): 416–430.
... edge of many of the overthrust slices and also along the axis of the Powell Valley anticline. On the other hand, rocks of Mississippian age are preserved in the trough of the Greendale syncline. Northwest of the Valley and Ridge province, rocks of Pennsylvanian age are preserved at the surface...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1938
AAPG Bulletin (1938) 22 (2): 129–174.
... rapidly whenever environmental conditions became favorable. According to Newcombe 20 the Southern Peninsula of Michigan is, a major, isolated, structural and stratigraphic basin which is somewhat elongate or synclinal northwest and southeast. Structurally, it is limited by the bifurcating...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1963
AAPG Bulletin (1963) 47 (4): 666–680.
..., and Greendale synclines. ...
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Series: GSA Special Papers
Published: 12 August 2020
DOI: 10.1130/2020.2545(06)
EISBN: 9780813795454
... is Bacon Bend in Monroe County (BB in Fig. 1 ; Glover, 1959) . Butterfly Gap Greasy Cove Formation. This formation occupies the stratigraphic position of the Newman Limestone and/or Maccrady Formation in the Greendale syncline to the northwest. Only the lower 54 m of the 120 m exposed...
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Journal Article
Published: 01 November 2002
Proceedings of the Yorkshire Geological Society (2002) 54 (2): 65–93.
... caldera ( Branney & Kokelaar 1994 ). More than 900 m accumulated in the area that now forms the Scafell Syncline though substantial amounts occur to the south in the Coniston Fells and south of Devoke Water, where the ignimbrites are overstepped by younger strata of the Duddon Basin succession ( Fig...
Journal Article
Published: 01 August 2012
Bulletin of the Seismological Society of America (2012) 102 (4): 1514–1542.
... w  7.1, 4 September 2010 Darfield, and M w  6.2, 22 February 2011 Christchurch earthquakes. While the Greendale fault, source of the Darfield earthquake, has been added to the fault source model, the large data set of earthquakes and strong‐motion records from the two events have not been included...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 1984
AAPG Bulletin (1984) 68 (1): 92–105.
... syncline shows structural culmination 3 km (2 mi) north of the projected lineament. The Greendale-Sabinsville anticlinal axis shows an abrupt northwesterly deflection where it crosses the lineament. The Shawmut-Worthville synclinal axis shows structural culmination across the lineament. Both...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1985
AAPG Bulletin (1985) 69 (10): 1518–1533.
...) in Washington County about 5 mi north of Bristol near the community of Benhams. The well was a new-field wildcat located on the crest of the Wolf Run anticline, an anticlinal wrinkle in the trough of the Greendale syncline about 6 mi northeast of and on trend with Early Grove field. The Wolf Run structure...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1984
AAPG Bulletin (1984) 68 (10): 1383–1399.
... ( Table 15 , no. 6) is located in Rich Valley, just south of the surface trace of the Saltville thrust fault, where the fault overrides the southeast limb of the Greendale syncline. This well was drilled as a new-field wildcat to test the Silurian Clinch sandstone in what was apparently believed...
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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1976
AAPG Bulletin (1976) 60 (8): 1288–1322.
... southwest of the town of Saltville near the Smyth County line and completely across the county northeast of previous production in the old Early Grove gas field. The location is just south of the Greendale syncline and the surface trace of the Saltville thrust fault where Cambrian rocks have been thrust...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1983
AAPG Bulletin (1983) 67 (10): 1570–1592.
... of the Greendale syncline just north of the trace of the Saltville fault. The well was drilled about 5 mi northeast of the old Early Grove gas field; it bottomed in the Devonian Chemung shale at 7,140 ft. A gas show was encountered in the Mississippian Fido Sandstone, but it was noncommercial and the well...
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Journal Article
Published: 01 November 2004
Proceedings of the Yorkshire Geological Society (2004) 55 (2): 73–105.
... ). An initial Plinian fall-out phase may be indicated by 1–2 m of bedded pumice lapilli-tuff at the base ( Millward et al. 2000 a ), but thickness variation in the overlying ignimbrite is systematic and fault controlled. West of the Greendale Fault, more than 1000 m of massive eutaxitic lapilli-tuff...
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Journal Article
Published: 19 December 2011
Canadian Journal of Earth Sciences (2012) 49 (1): 346–358.
... into a regional NNE-trending, gently plunging syncline ( Fig. 2 b ) with a local, penetrative, axial planar fabric ( Boucot et al. 1974 ; Murphy and Keppie 1998 ; Braid and Murphy 2006 ). Arisaig Group strata are unconformably overlain by the Late Devonian McArras Brook Formation ( Fig. 2 b ), which consists...
Series: SEPM Special Publication
Published: 01 January 2003
DOI: 10.2110/pec.03.78.0011
EISBN: 9781565763340
... in the overthrust belt in the Greendale Syncline, southwestern Virginia, where Mississippian units thicken to over 2000 meters of basinal, slope, and ramp-margin facies ( Cooper, 1948 ; Bartlett and Webb, 1971 ). Several synsedimentary positive structures occur in West Virginia and eastern Kentucky ( Yeilding...
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