Whitewell Anticline

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Journal Article
Published: 01 May 2010
Proceedings of the Yorkshire Geological Society (2010) 58 (1): 1-8.
... and eastern closure of the Whitewell Anticline) and in Waulsortian limestones. These values are consistent with the limited vitrinite reflectance data and are a result of the Carboniferous sedimentary and tectonic history of the region. There is no evidence of significant modification by subsequent burial...
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.11
EISBN: 9781862396944
... foraminifer Eoparastaffella, suggesting the group is entirely Tournaisian in age. Foraminiferal assemblages from the Chatburn Limestone and Clitheroe Limestone formations exposed in the Whitewell Anticline (Fig. 35 , Col. 2) indicate the Cf4α1 Subzone O1 ( Aitkenhead et al. 1992 ). The base of the group...
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Journal Article
Journal: AAPG Bulletin
Published: 01 March 1957
AAPG Bulletin (1957) 41 (3): 511-537.
... in the Whitewell area of the Slaidburn anticline Fig. 5 there is a continuous section of reef and non-reef beds, and Black (1953 , 1954 ) has been able to make a fairly precise estimate of the depositional dip of the reef beds. The reef limestones here are partly non-bedded and partly bedded. He found...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 1985
AAPG Bulletin (1985) 69 (10): 1856-1870.
... encountered no hydrocarbons and was plugged and abandoned as a dry hole. Montague 1 was drilling at 3,979 m at year end after experiencing severe drilling problems and without recording significant signs of hydrocarbons. Talisman 1 was drilled to test an anticlinal structure located on the Legendre trend...
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Journal Article
Published: 29 May 2018
Petroleum Geoscience (2018) 24 (3): 287-322.
... (Chatburn Limestone) are exposed in the cores of a series of en echelon NE–SW-trending anticlines, including the Ashnott, Whitewell, Sykes, Slaidburn, Clitheroe and Skipton anticlines (see Fig. 1b ). Arthurton (1984) demonstrated that these structures were formed in a dextral strike-slip shear zone...
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