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Oatka Creek Shale Member

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Journal Article
Journal: GSA Bulletin
Published: 01 May 2016
GSA Bulletin (2016) 128 (5-6): 707–718.
...D. Minguez; K.P. Kodama; T. Engelder Abstract This study presents paleomagnetic results from the Oatka Creek Member of the Marcellus Formation. Paleomagnetic specimens were subsampled from a 50.8-mm-diameter subsurface drill core obtained from the Valley and Ridge physiographic province...
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Isopach maps of <b>shale</b> lithofacies in the <b>Oatka</b> <b>Creek</b> <b>Member</b>, modeled by seq...
Published: 01 December 2013
Figure 15 Isopach maps of shale lithofacies in the Oatka Creek Member, modeled by sequential indicator simulation method. (A) Organic siliceous shale isopach (OSS). (B) Organic mixed shale isopach (OMS). (C) Organic mudstone isopach (OMD). (D) Gray siliceous shale isopach (GSS). (E) Gray mixed
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Cross-section illustrating eastward thickening of the <b>Oatka</b> <b>Creek</b> <b>Member</b>. T...
Published: 01 January 2011
Figure 13 Cross-section illustrating eastward thickening of the Oatka Creek Member. The Oatka Creek is subdivided into an organic-rich (radioactive) basal interval overlain by organic-lean shale (low radioactivity). The cross-section is hung on the top of the Oatka Creek Member.
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Contact of the <b>Oatka</b> <b>Creek</b> <b>Member</b>, Marcellus Formation, and the overlying S...
Published: 01 January 2011
Figure 14 Contact of the Oatka Creek Member, Marcellus Formation, and the overlying Stafford Member of the Skaneateles Formation exposed on Oatka Creek, village of LeRoy, New York. TOC of the Oatka Creek Member immediately beneath the contact is 4%. Note heavily jointed nature of the organic-rich
Journal Article
Journal: GSA Bulletin
Published: 01 July 1984
GSA Bulletin (1984) 95 (7): 814–828.
... central Lake Erie, the Union Springs, Cherry Valley, and Oatka Creek Members of the Marcellus merge into the Bell Shale, Rockport Quarry Limestone, and Arkona Shale of Ontario. The Arkona can be traced across Lake Erie into the Plum Brook and Lower Olentangy Shales of Ohio. The lower part...
Series: GSA Special Papers
Published: 01 September 2015
DOI: 10.1130/2015.2515(08)
... cycle (MSS2), which comprises the bulk of the Oatka Creek Member of the Marcellus Shale, indicates improved bottom-water conditions. Redox conditions recorded by framboid diameters of the MSS1 cycle of the Greene County core are generally similar to those of the Upshur County core; however, conditions...
Series: GSA Special Papers
Published: 12 August 2020
DOI: 10.1130/2020.2545(09)
EISBN: 9780813795454
..., we conducted multivariate analyses (cluster and correspondence analysis) of marine faunas in 81 large samples (~300 specimens each) in shallowing-upward sequences of the Cardiff and Pecksport Members (Marcellus Subgroup, Oatka Creek Formation) of the Hamilton Group. Eight statistically...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP278.5
EISBN: 9781862395268
... of the Appalachian Basin. Similar grey, fossiliferous beds, high in the Bell Shale of Ontario, may represent the Cardiff (Solsville-Pecksport) Member (Fig.  5 ). These beds appear to be traceable into the Bell Shale of Michigan. In Ohio, the Oatka Creek sequence is probably represented by the upper portion (M-zone...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP278.4
EISBN: 9781862395268
... in barite nodules ( Ver Straeten et al. 1994 ). These shales, termed the Lincoln Park Submember of the Hurley Member by Ver Straeten et al. (1994) , have the goniatite subspecies Agoniatites vanuxemi nodiferus . The Cherry Valley Member of the redefined Oatka Creek Formation is a 0.4 to 5 m thick...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 2014
AAPG Bulletin (2014) 98 (3): 483–513.
... and equivalents lies a second organic-carbon–rich unit that we informally call the Oatka Creek member (unnamed member in ver Straeten, 2007 ). These units sit within the Pragian-1 through Givetian-4 lower Kaskaskia supersequence, which is bounded below by the Walbridge unconformity or correlative conformity...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP314.2
EISBN: 9781862395626
... ( Koch & Day 1996 ; DeSantis et al. 2007 ). As in the case of the Stony Hollow fauna, the appearance of much of the Hamilton fauna in the Appalachian Basin coincides with a major transgressive black shale, the East Berne Member of the Oatka Creek Formation. It represents a major incursion of new...
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Journal Article
Journal: Interpretation
Published: 22 May 2015
Interpretation (2015) 3 (3): SV17–SV33.
..., and the establishment and breakdown of seasonal thermoclines were the predominant mode of water stratification during Marcellus Shale deposition. However, their study was primarily confined to the Oatka Creek Mbr. of the Marcellus Formation and other stratigraphically higher black shale units in New York State ( Werne...
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... ), many geologists use the name informally. The upper unit of the Marcellus Shale is the Oatka Creek Member. This unit is well exposed at the type section near Mar- cellus, New York ( Cooper, 1930 ), and is less organic and more clay rich than the Union Springs. The Oatka Creek Member is soft, fissile...
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Journal Article
Journal: Interpretation
Published: 26 July 2013
Interpretation (2013) 1 (1): B7–B26.
... mudstone-dominated formations are subdivided by geologists into stratigraphic packages termed members that are typically tens of meters thick and are composed of bedsets (Figure  9 ). The “member-scale” subdivisions of the Marcellus Shale (Union Springs, Cherry Valley, and Oatka Creek members) are one...
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Journal Article
Journal: Economic Geology
Published: 01 November 2004
Economic Geology (2004) 99 (7): 1385–1414.
... are mainly from the Key Creek plate. Most samples of the drowned shelf facies of the Lisburne Group are from the Ivotuk plate. Stratigraphic coverage is good for the Kayak Shale and the Kuna and Siksikpuk Formations, although only six samples of shale were collected from the uppermost Kuna Formation (< 5...
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Journal Article
Journal: The Leading Edge
Published: 01 May 2018
The Leading Edge (2018) 37 (5): 356–361.
... Marcellus member (sometimes known as the Oatka Creek Shale member) and the Lower Marcellus member (sometimes known as the Union Springs Shale member). The Upper and Lower Marcellus shales are separated by the Cherry Valley Limestone member. The average thickness of the entire Marcellus formation is about...
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Journal Article
Published: 01 August 2015
Journal of Sedimentary Research (2015) 85 (8): 937–954.
... contact, at the last occurrence of black or dark-gray mudstone (last occurrence of strata with a gamma-ray value greater than 200 API units). The tripartite stratigraphy of Lash and Engelder (2011) is serviceable in our study area: Union Springs, Cherry Valley, and Oatka Creek Members from bottom to top...
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Journal Article
Journal: AAPG Bulletin
Published: 01 December 2013
AAPG Bulletin (2013) 97 (12): 2173–2205.
...Figure 15 Isopach maps of shale lithofacies in the Oatka Creek Member, modeled by sequential indicator simulation method. (A) Organic siliceous shale isopach (OSS). (B) Organic mixed shale isopach (OMS). (C) Organic mudstone isopach (OMD). (D) Gray siliceous shale isopach (GSS). (E) Gray mixed...
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Journal Article
Published: 01 December 2011
Environmental Geosciences (2011) 18 (4): 217–257.
...) interpreted as a drowning unconformity. The Oatka Creek in the subsurface of most of the Appalachian Plateau of Pennsylvania is dominated by organic-rich shale (the Chittenango Member of the Oatka Creek Formation in New York; see Figure 7 ). Like the Union Springs Member, this shale has a high TOC value (up...
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Journal Article
Journal: Interpretation
Published: 09 September 2019
Interpretation (2019) 7 (4): SJ33–SJ43.
... 100 ft (30 m) in northeastern Pennsylvania. Overlying the Cherry Valley Member is the Oatka Creek Formation, informally referred to as the upper Marcellus. This unit is defined as a medium to dark-gray mudstone with an underlying interval of black organic-rich mudstone. A 105 ft Marcellus Shale...
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