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Derbyshire Platform

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Journal Article

Burial diagenetic evolution of the Lower Carboniferous (Dinantian) of the southern margin of the Askrigg Platform and a comparison with the Derbyshire Platform Available to Purchase

Cathy Hollis, Gordon Walkden
Published: 01 February 2012
Petroleum Geoscience (2012) 18 (1): 83–95.
DOI: https://doi.org/10.1144/1354-079311-049
... of the Askrigg Platform of North Yorkshire and a comparison with published data from the age-equivalent Derbyshire Platform. A pattern of consistent, diagenetic modification during early diagenesis is evident, but key differences occur in the burial realm. On both the southern margin of the Askrigg Platform...
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View PDF for article title, Burial diagenetic evolution of the Lower Carboniferous (Dinantian) of the southern margin of the Askrigg <span class="search-highlight">Platform</span> and a comparison with the <span class="search-highlight">Derbyshire</span> <span class="search-highlight">Platform</span>
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Journal Article

Controls on dolomitization in extensional basins: An example from the Derbyshire Platform, U.K. Open Access

Catherine Breislin, Stephen Crowley, Vanessa J. Banks, Jim D. Marshall, Ian L. Millar, James B. Riding, Cathy Hollis
Published: 13 November 2020
Journal of Sedimentary Research (2020) 90 (9): 1156–1174.
DOI: https://doi.org/10.2110/jsr.2020.58
.... The largest of these dolomite bodies (approx. 60 km 2 ) occurs on the Derbyshire Platform, on the southern margin of the Pennine Basin. This study tests the hypothesis that dolomitization occurred at this locality during deposition, platform drowning, and the earliest stages of burial, coincident...
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Journal Article

Sedimentary context and palaeoecology of Gigantoproductus shell beds in the Mississippian Eyam Limestone Formation, Derbyshire carbonate platform, central England Open Access

L. S. P. Nolan, L. Angiolini, F. Jadoul, G. Della Porta, S. J. Davies, V. J. Banks, M. H. Stephenson, M. J. Leng
Published: 25 July 2017
Proceedings of the Yorkshire Geological Society (2017) 61 (4): 239–257.
DOI: https://doi.org/10.1144/pygs2017-393
...L. S. P. Nolan; L. Angiolini; F. Jadoul; G. Della Porta; S. J. Davies; V. J. Banks; M. H. Stephenson; M. J. Leng Abstract A sedimentological study was conducted at two localities exposing the Mississippian Eyam Limestone Formation of the Derbyshire carbonate platform, UK. Ricklow Quarry comprises...
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View PDF for article title, Sedimentary context and palaeoecology of Gigantoproductus shell beds in the Mississippian Eyam Limestone Formation, <span class="search-highlight">Derbyshire</span> carbonate <span class="search-highlight">platform</span>, central England
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(a) Steeply dipping northern margin of the Derbyshire Platform cemented debrites. (b) The fabric of debrites is best observed on a polished surface. They comprise fragmented, centimetre-scale bioclasts which are cemented by white radiaxial–fibrous cements. The southern margin of the Derbyshire Platform comprises slumped, dolomitized floatstones. (c) and (d) Harborough Rocks.

( a ) Steeply dipping northern margin of the Derbyshire Platform cemented d... Available to Purchase

Published: 28 April 2021
Fig. 5. ( a ) Steeply dipping northern margin of the Derbyshire Platform cemented debrites. ( b ) The fabric of debrites is best observed on a polished surface. They comprise fragmented, centimetre-scale bioclasts which are cemented by white radiaxial–fibrous cements. The southern margin
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Conceptual model of dolomitisation on the Derbyshire Platform. A) During the Asbian and Brigantian, seawater convected through the porous and permeable platform margin facies, driven by a high geothermal gradient. B) By the early Serphukovian, the platform had drowned and sills were emplaced. Seawater continued to convect on the platform margin and along faults, with leaching of Mg from interbedded volcanics facilitated by a decrease in pH from mantle-derived CO2. At the same time, groundwater fluxed eastwards under gravity, across the East Midlands Shelf (Walkden and Williams 1991). C) Dolomitization from seawater waned as the platform was buried during the Serphukhovian. Once the platform was buried beneath shales, compactional dewatering and seismically-driven fluid expulsion (Frazer et al. 2014) led to dolomitization along faults (D2), overprinting D1 dolomite.

Conceptual model of dolomitisation on the Derbyshire Platform. A) During ... Open Access

Published: 13 November 2020
Fig. 11.— Conceptual model of dolomitisation on the Derbyshire Platform. A) During the Asbian and Brigantian, seawater convected through the porous and permeable platform margin facies, driven by a high geothermal gradient. B) By the early Serphukovian, the platform had drowned and sills were
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A) Geological map of the Derbyshire Platform. B) Detailed geological map of the Masson Hill area Sample localities and boreholes are identified on the maps. 1, Harborough Rocks; 2, Carsington Pastures; 3, Hopton Tunnel; 4, Brassington Moor Quarry; 5, Ryder Point Quarry; 6, Wapping Mine; 7, Upper Wood; 8, Temple Mine; 9, Coal Pit Rake; 10, Cromford; 11, Masson Hill; 12, High Peak Quarry; 13, Wyns Tor; 14, Grey Tor; 15, Golconda Mine; 16, Devonshire Cavern; 17, Masson Cavern; 18, Gurdall Wensley borehole; 19, Four Lanes End borehole; 20, Bottom Lees Farm borehole; 21, Gratton Dale. C) Cross section of line A–B, as shown in Part A.

A) Geological map of the Derbyshire Platform. B) Detailed geological map... Open Access

Published: 13 November 2020
Fig. 2.— A) Geological map of the Derbyshire Platform. B) Detailed geological map of the Masson Hill area Sample localities and boreholes are identified on the maps. 1, Harborough Rocks; 2, Carsington Pastures; 3, Hopton Tunnel; 4, Brassington Moor Quarry; 5, Ryder Point Quarry; 6, Wapping
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Paragenetic sequence for the Derbyshire Platform. Note that calcite cements (Z1–4) were defined by Walkden and Williams (1991), and the paragenesis and intergrowth of Zone 3A–B and 4A–D calcite cements with non-carbonate minerals was defined and described by Hollis and Walkden (2002).

Paragenetic sequence for the Derbyshire Platform. Note that calcite cements... Open Access

Published: 13 November 2020
Fig. 3.— Paragenetic sequence for the Derbyshire Platform. Note that calcite cements (Z1–4) were defined by Walkden and Williams (1991) , and the paragenesis and intergrowth of Zone 3A–B and 4A–D calcite cements with non-carbonate minerals was defined and described by Hollis and Walkden (2002) .
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(a) Section across the northern margin of the Derbyshire Platform (A–B in Fig. 1). The section detail is informed by the seismic profile shown in (b). The Castleton Fault that forms the southern margin of the Edale Basin is not exposed at the surface but is clear in the seismic profile. Dirtlow Rake is a splay of the Castleton Fault. Profile and section are from Andrews (2013).

( a ) Section across the northern margin of the Derbyshire Platform (A–B in... Available to Purchase

Published: 12 December 2018
Fig. 2. ( a ) Section across the northern margin of the Derbyshire Platform (A–B in Fig. 1 ). The section detail is informed by the seismic profile shown in ( b ). The Castleton Fault that forms the southern margin of the Edale Basin is not exposed at the surface but is clear in the seismic
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Basin evolution model for the Edale Gulf and adjacent Derbyshire Platform. The Visean–Namurian boundary both in the basin and on the platform is indicated. Isotherms are from the estimates of Colman et al. (1989) and Walkden &amp; Williams (1991). The age of the mineralization based on the range of evidence summarized at the bottom of the diagram is early Permian and towards the end of the late Visean uplift. Fluids originating from the shale units of the Bowland–Hodder group in the basin rise rapidly along the Castleton and associated faults to a depth of c. 1 km where mineralization takes place. The repeated rupture of the shale and subsequent faulting may occur as overpressured cells within sediment units pass through the lithostatic pressure gradient curve during uplift.

Basin evolution model for the Edale Gulf and adjacent Derbyshire Platform. ... Available to Purchase

Published: 12 December 2018
Fig. 9. Basin evolution model for the Edale Gulf and adjacent Derbyshire Platform. The Visean–Namurian boundary both in the basin and on the platform is indicated. Isotherms are from the estimates of Colman et al . (1989) and Walkden & Williams (1991) . The age of the mineralization based
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Fracture paragenesis on the Derbyshire Platform in (A) cathodoluminescence and (B) epifluorescence.

Fracture paragenesis on the Derbyshire Platform in ( A ) cathodoluminescenc... Available to Purchase

Published: 01 February 2012
Fig. 11. Fracture paragenesis on the Derbyshire Platform in ( A ) cathodoluminescence and ( B ) epifluorescence.
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Dolomitized Asbian–Brigantian limestone on the Derbyshire Platform: (A) outcrop of dolomitized Asbian Limestone; (B) de-dolomitization (a) and dissolution (b) of replacive dolomite. Field of view 4 mm. (C) Fracture-filling saddle dolomite (a) enveloped by Zone 4A calcite (see Fig. 5). Dashed line marks fracture margin. Field of view 1 mm.

Dolomitized Asbian–Brigantian limestone on the Derbyshire Platform: ( A ) o... Available to Purchase

Published: 01 February 2012
Fig. 10. Dolomitized Asbian–Brigantian limestone on the Derbyshire Platform: ( A ) outcrop of dolomitized Asbian Limestone; ( B ) de-dolomitization (a) and dissolution (b) of replacive dolomite. Field of view 4 mm. ( C ) Fracture-filling saddle dolomite (a) enveloped by Zone 4A calcite (see Fig
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Summary of geochemical data for Derbyshire Platform (summarized from Hollis &amp; Walkden (1996, 2002) and Hollis (1998)).

Summary of geochemical data for Derbyshire Platform (summarized from Holli... Available to Purchase

Published: 01 February 2012
Fig. 12. Summary of geochemical data for Derbyshire Platform (summarized from Hollis & Walkden (1996 , 2002 ) and Hollis (1998) ).
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Summarized paragenesis for the Derbyshire Platform, concentrating on burial calcite cementation (Zones 1-4).

Summarized paragenesis for the Derbyshire Platform, concentrating on burial... Available to Purchase

Published: 01 September 2002
Figure 3 Summarized paragenesis for the Derbyshire Platform, concentrating on burial calcite cementation (Zones 1-4).
Journal Article

Reconstructing Fluid Expulsion and Migration North of the Variscan Orogen, Northern England Available to Purchase

Cathy Hollis, Gordon Walkden
Published: 01 September 2002
Journal of Sedimentary Research (2002) 72 (5): 700–710.
DOI: https://doi.org/10.1306/012102720700
...Figure 3 Summarized paragenesis for the Derbyshire Platform, concentrating on burial calcite cementation (Zones 1-4). ...
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Journal Article

Unravelling evidence for global climate change in Mississippian carbonate strata from the Derbyshire and North Wales Platforms, UK Available to Purchase

Lucy Manifold, Peter del Strother, David P. Gold, Peter Burgess, Cathy Hollis
Published: 28 April 2021
Journal of the Geological Society (2021) 178 (5): jgs2020-106.
DOI: https://doi.org/10.1144/jgs2020-106
...Fig. 5. ( a ) Steeply dipping northern margin of the Derbyshire Platform cemented debrites. ( b ) The fabric of debrites is best observed on a polished surface. They comprise fragmented, centimetre-scale bioclasts which are cemented by white radiaxial–fibrous cements. The southern margin...
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View PDF for article title, Unravelling evidence for global climate change in Mississippian carbonate strata from the <span class="search-highlight">Derbyshire</span> and North Wales <span class="search-highlight">Platforms</span>, UK
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Summary of the five dolostone phases identified on the Derbyshire platforms... Open Access

Published: 13 November 2020
Table 2.— Summary of the five dolostone phases identified on the Derbyshire platforms and their structural relationships.
Journal Article

Clumped isotope evidence for episodic, rapid flow of fluids in a mineralized fault system in the Peak District, UK Available to Purchase

Paul F. Dennis, Daniel J. Myhill, Alina Marca, Ruth Kirk
Published: 12 December 2018
Journal of the Geological Society (2019) 176 (3): 447–461.
DOI: https://doi.org/10.1144/jgs2016-117
...Fig. 2. ( a ) Section across the northern margin of the Derbyshire Platform (A–B in Fig. 1 ). The section detail is informed by the seismic profile shown in ( b ). The Castleton Fault that forms the southern margin of the Edale Basin is not exposed at the surface but is clear in the seismic...
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(a) Lateral log of the carbonate mound of the Little Orme, North Wales Platform; (b) lateral log of the carbonate mound of Pin Dale Quarry, Derbyshire Platform; (c) vertical log of the carbonate mound of Pin Dale Quarry, Derbyshire Platform. Note the different scales of each log.

( a ) Lateral log of the carbonate mound of the Little Orme, North Wales Pl... Available to Purchase

Published: 28 April 2021
Fig. 7. ( a ) Lateral log of the carbonate mound of the Little Orme, North Wales Platform; ( b ) lateral log of the carbonate mound of Pin Dale Quarry, Derbyshire Platform; ( c ) vertical log of the carbonate mound of Pin Dale Quarry, Derbyshire Platform. Note the different scales of each log.
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A) Tectono-stratigraphy of the Mississippian of southern Britain, after Fraser and Gawthorpe (2003). BH, Bowland High; BT, Bowland Trough; CLH, Central Lancashire High; DF, Dent Fault; DP, Derbyshire Platform; FHF, Flamborough Head Fault; GT, Gainsborough Trough; HdB, Huddersfield Basin; HB, Humber Basin; LDH, Lake District High; MCF, Morley–Campsall Fault; MH, Manx High; NCF, North Craven Fault; PF, Pennine Fault; SF, Stublick Fault; WG, Widmerpool Gulf. Approximate locations of dolostone bodies on the margins of carbonate platforms are indicated by the red arrows, with the yellow box highlighting the position of the Derbyshire Platform, the focus of this study. B) Stratigraphic framework for the Mississippian of the Derbyshire Platform. Ages derived from Gradstein and Ogg (2004), seismic sequences from Fraser et al. (1990).

A) Tectono-stratigraphy of the Mississippian of southern Britain, after F... Open Access

Published: 13 November 2020
Fig. 1.— A) Tectono-stratigraphy of the Mississippian of southern Britain, after Fraser and Gawthorpe (2003) . BH, Bowland High; BT, Bowland Trough; CLH, Central Lancashire High; DF, Dent Fault; DP, Derbyshire Platform; FHF, Flamborough Head Fault; GT, Gainsborough Trough; HdB, Huddersfield
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(a) Exposure-related facies. (i) Type A, undulating limestone, North Wales Platform; (ii) Type B, nodular limestone, north wales Platform; (iii) red-coloured unconsolidated muds and clays, North Wales Platform; (iv) brown-coloured unconsolidated muds and clays with plant material and quartz clasts, Derbyshire Platform; (v) yellow-coloured unconsolidated muds and clays, North Wales Platform. (b) Igneous facies in core. (i) Contact between extrusive volcanics (weathered basalt) and Bee Low limestone, Derbyshire Platform; (ii) multicoloured volcanic ash from core, Derbyshire Platform. (c) (i) Mudrock overling and draping a Type A mammilated surface, Trefor Rocks, North Wales Platform; (ii) mudrock bed between two limestone beds, with no evidence of emergence, suggesting marine deposition, Trefor Rocks, North Wales Platform; (iii) dark green palaeosol overlying karstic surface beneath the Asbian–Brigantian boundary, Tarmac Hendre Quarry, near Mold. Green-brown weathered limestone is Asbian, grey-weathered limestone is Brigantian.

( a ) Exposure-related facies. (i) Type A, undulating limestone, North Wale... Available to Purchase

Published: 28 April 2021
and quartz clasts, Derbyshire Platform; (v) yellow-coloured unconsolidated muds and clays, North Wales Platform. ( b ) Igneous facies in core. (i) Contact between extrusive volcanics (weathered basalt) and Bee Low limestone, Derbyshire Platform; (ii) multicoloured volcanic ash from core, Derbyshire Platform