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Lynn Mountain Syncline

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Journal Article
Journal: AAPG Bulletin
Published: 11 November 1996
AAPG Bulletin (1996) 80 (11): 1695-1709.
... in the Lynn Mountain syncline. Similar sequences may also exist well to the south, in the Boktukola syncline, where thick sand intervals have been identified. Petrographic study of samples from the Lynn Mountain syncline suggests that channel sequences may have significantly higher reservoir quality than...
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Image
—Part of the measured Jackfork section at McKinley Rocks, <b>Lynn</b> <b>Mountain</b> syn...
Published: 11 November 1996
Figure 11. —Part of the measured Jackfork section at McKinley Rocks, Lynn Mountain syncline, southern Latimer County, Oklahoma (location 2, Figure 10 ). Interpretation of the outcrop proposes a series of overlapping and amalgamated channels, consisting of clean quartzarenites and showing
Journal Article
Journal: AAPG Bulletin
Published: 01 January 1960
AAPG Bulletin (1960) 44 (1): 72-82.
... and as the flanking Muenster arch and Criner Hills were characterized by slight relief, little coarse clastic but much limestone and shale deposition took place. By middle Cisco time, folding and thrusting in the Arbuckle Mountain region had compressed the Marietta syncline, causing the Criner Hills...
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Series: GSA Field Guide
Published: 01 January 2014
DOI: 10.1130/2014.0037(08)
EISBN: 9780813756370
... is visible on the left, and the Gravelly Range on the right. 62.9 Sphinx Mountain in the Madison Range is at 10 o’clock. A syncline that formed during the Cretaceous Period by progressive crustal loading during thrust faulting was filled with coarse sediments that lithified into conglomerate that caps...
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Journal Article
Published: 01 July 2015
Rocky Mountain Geology (2015) 50 (1): 30-118.
... the area that later elevated as Elk Mountain, thus causing origin of Pass Creek Basin. Elk Mountain's ca. 12 km uplift could not have occurred prior to the early Eocene, and that event contributed to tight folding of the Hanna Syncline. Coal Bank Basin is a giant footwall syncline ahead of the out...
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Journal Article
Published: 01 March 2016
Bulletin of Canadian Petroleum Geology (2016) 64 (1): 1-23.
...Lynn T. Dafoe; John Shaw; Christopher Jauer; Peter S. Giles; John W.F. Waldron; D. Patrick Potter Abstract St. George’s Bay lies south of Port au Port Peninsula on the west coast of Newfoundland, Canada. The Carboniferous Bay St. George subbasin extends beneath the bay and onshore to the southeast...
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Series: SEPM Special Publication
Published: 01 January 2008
DOI: 10.2110/pec.08.89.0125
EISBN: 9781565762244
... reveals correlations between anticlines, synclines, and abrupt linear changes in dip vectors with magnetically inferred compositional and structural features of the basement ( Yarger, 1983 ; Van Schmus et al., 1987 ; Kruger, 1996 ) (Fig. 3 ). Fig. 3 .—Aeromagnetic map of Kansas acquired on 1/4 mi...
Series: GSA Field Guide
Published: 01 January 2010
DOI: 10.1130/2010.0016(05)
EISBN: 9780813756165
... Devonian quartz arenites and carbonates (inter-orogenic tectonic calm), and Upper Devonian to Lower Mississippian clastic rocks (associated with the Acadian orogeny). Alleghanian structural features include the Little North Mountain thrust, Cacapon Mountain anticlinorium, Broad Top synclinorium, and Wills...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1985
AAPG Bulletin (1985) 69 (6): 933-945.
...H. J. Meyer; H. W. McGee ABSTRACT Definite “hot spots” or positive geothermal anomalies are associated with 15 of 22 Rocky Mountain oil and gas fields examined in Montana, North Dakota, Wyoming, Utah, Colorado, and New Mexico. Of the remaining 7 fields, 5 have poor to sparse data, and the other 2...
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Journal Article
Published: 06 July 2011
Canadian Journal of Earth Sciences (2011) 48 (7): 1131-1154.
... the northern Rocky Mountain Basin and Range province. Gravity modelling, borehole data, and geologic mapping from the Flint Creek basin indicate that subsidence was focused along an extensionally reactivated Sevier thrust fault, which accommodated up to 800 m of basin fill while relaying stress between...
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Journal Article
Published: 01 September 2002
Bulletin of Canadian Petroleum Geology (2002) 50 (3): 407-418.
... of the 1.77–0.78 Ga ( Ross et al., 2001 ) Muskwa assemblage or rocks of an older package possibly equivalent to the 1.84–1.71 Ga ( Thorkelson, 2000 ) Wernecke Supergroup. The Muskwa assemblage, exposed in the Rocky Mountains between latitudes 57°35′ and 59°15′N, comprises marine sandstone, shale and carbonate...
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Journal Article
Journal: Geosphere
Published: 01 October 2014
Geosphere (2014) 10 (5): 1043-1060.
... 2014 © 2014 Geological Society of America 2014 The RMF steps northeastward ∼50 km from the eastern edge of the Wet Mountains to the eastern edge of the southern Front Range ( Figs. 6 and 7 ); between are the Cañon City embayment, its northern extension, the Garden Park syncline...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1960
AAPG Bulletin (1960) 44 (2): 137-155.
...Henry L. Berryhill, Jr.; Reginald P. Briggs; Lynn III Glover ABSTRACT Rocks of Late Cretaceous age (Turonian to Maestrichtian) in Puerto Rico are of three types: (1) primary volcanic rocks, including tuffs, tuff breccias, and lavas; (2) intermixed pyroclastic and epiclastic rocks, including...
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Series: GSA Reviews in Engineering Geology
Published: 01 January 2008
DOI: 10.1130/2008.4020(01)
EISBN: 9780813758206
... Abstract The city of Seattle, Washington State, lies within the Puget Sound Lowland, an elongate structural and topographic basin between the Cascade Range and Olympic Mountains. The area has been impacted by repeated glaciation in the past 2.4 m.y. and crustal deformation related...
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Series: GCSSEPM
Published: 01 December 2004
DOI: 10.5724/gcs.04.24.0293
EISBN: 978-0-9836096-6-7
... City strata have been drilled along strike, but the thickness we have given to Queen City strata in the depotrough should be treated as speculative. The interval labeled “Y” and colored orange in Figure 3B , contains Weches, Sparta, Cook Mountain, and Yegua age strata. A slight thickening...
Journal Article
Journal: GSA Bulletin
Published: 01 May 2011
GSA Bulletin (2011) 123 (5-6): 979-996.
...Majie Fan; Peter G. DeCelles; George E. Gehrels; David L. Dettman; Jay Quade; S. Lynn Peyton Abstract Shallow subduction of the Farallon plate beneath the western United States has been commonly accepted as the tectonic cause for the Laramide deformation during Late Cretaceous through Eocene time...
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Journal Article
Published: 01 April 2011
The Canadian Mineralogist (2011) 49 (2): 441-458.
...Kara-Lynn Scallion; Rebecca A. Jamieson; Sandra M. Barr; Chris E. White; Saskia Erdmann Abstract The Governor Lake area, Meguma terrane, Nova Scotia, is underlain mainly by ca. 373 Ma granitoid rocks of the Trafalgar plutonic suite that intruded metasedimentary rocks of the Goldenville and Halifax...
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Journal Article
Journal: AAPG Bulletin
Published: 01 November 1959
AAPG Bulletin (1959) 43 (11): 2575-2591.
...Lynn Jacobsen ABSTRACT The major oil reserves found in Springer sandstones have been found in the giant Velma and Sholom Alechem fields and in the adjacent smaller fields of Carter and Stephen counties, Oklahoma. These oil fields occur on prominent high-relief closed structural features...
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Journal Article
Published: 01 August 2008
Bulletin of the Seismological Society of America (2008) 98 (4): 1696-1719.
...Lynn R. Sykes; John G. Armbruster; Won-Young Kim; Leonardo Seeber Abstract A catalog of 383 earthquakes in southeastern New York, southwestern Connecticut, northern New Jersey, and eastern Pennsylvania, including metropolitan New York City and Philadelphia, is compiled from historical...
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Journal Article
Published: 01 January 2004
Rocky Mountain Geology (2004) 39 (1): 7-64.
...Jason A. Lillegraven; Arthur W. Snoke; Malcolm C. McKenna Abstract The Hanna Basin of south-central Wyoming has been considered anomalous among other Laramide depocenters of the Rocky Mountain region because of its combination of small size and great thickness of synorogenic strata. Most prior...
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