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Pennell Bank

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Journal Article
Journal: GSA Bulletin
Published: 01 October 1999
GSA Bulletin (1999) 111 (10): 1486–1516.
...-zone positions in the central Ross Sea, reflecting the higher sediment supply and a stepped deglaciation. Ice remained grounded on the Pennell Bank to the west; a series of moraines marks the retreat of ice across the bank. Mega-scale glacial lineations and other streamlined, subglacial geomorphic...
Image
Photomicrographs illustrating intensity and impact of chemical processes.  ...
Published: 11 May 2020
of lower density and borings enlarged by dissolution. Sample collected from piston core NBP93-8-7 on Ross Bank. C) Photograph of skeletal separate containing gastropods (arrows) from 34–35 cm depth in core ELT32-09 on Pennell Bank (FA 4). D) Aragonitic shell material from gastropod from 58–60 cm depth
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Photomicrographs showing intensity and impact of endolithic boring.  A)  Cr...
Published: 11 May 2020
depth in piston core ELT52-09 on the flank of Mawson Bank. B) Stylasterid fragment with abundant sponge borings (3–10 cm in piston core 87-8, Pennell Bank). C) Bryozoan fragment with borings of fungus Flagrichnus baiulus (yellow arrow; C. Färber, personal communication 2015). Sample collected from
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Ross Sea (Ross Embayment) sector of the Antarctic ice sheets (West Antarcti...
Published: 01 November 2012
Harbour; JB—JOIDES Basin; KG—Koettlitz glacier; MB—Mount Bird; MBf—Minna Bluff; ME—Mount Erebus; MG—Mulock glacier; MkG—Mackay glacier; MS—McMurdo Sound; MT—Mount Terror; MTN—Mount Terra Nova; MwG—Mawson glacier; PB—Pennell Bank; PT—Pennell Trough; RB—Ross Bank; RI—Ross Island; RS—Royal Society Range; RvI
Journal Article
Journal: GSA Bulletin
Published: 11 May 2021
GSA Bulletin (2022) 134 (1-2): 348–370.
..., the Little America, Whales, and Glomar Challenger basins are separated by the Houtz and Hayes banks. In the western Ross Sea, Pennell, Joides, and Drygalski basins are separated by Pennell and Crary-Mawson banks, which are composed of sedimentary strata. Landwards, the Pennell and Joides basins merge...
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Map of the Ross Sea embayment and surroundings, showing the locations of pi...
Published: 11 May 2020
Fig. 1.— Map of the Ross Sea embayment and surroundings, showing the locations of piston cores (open circles) used in this study. Northeast–southwest-trending banks include Crary (C.B.), Mawson (M.B.), Pennell (P.B.), and Ross (R.B.) banks. Gray shading indicates extent of continental shelf
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Ross Sea examples of the mounded-elongated bodies interpreted as morainal b...
Published: 11 May 2021
Figure 8. Ross Sea examples of the mounded-elongated bodies interpreted as morainal bank complexes. (A) Little America Basin below RSU4 (in RSS4) in the single channel profile PD90_51. (B) Glomar Challenger Basin below RSU4a (in RSS3-II) in multichannel seismic (MCS) profile TH82_16. (C) Glomar
Journal Article
Journal: Economic Geology
Published: 01 May 2002
Economic Geology (2002) 97 (3): 471–480.
... Zn-Pb orebody , in Andrew , C.J. , Crowe , R.W.A. , Findlay , S. , Pennell , W.M. , and Pyne , J.F. , eds., Geology and genesis of mineral deposits in Ireland : Dublin , Irish Association for Economic Geology , p. 243 – 280 . Banks , D.A. , 1985 , A fossil...
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Journal Article
Published: 11 May 2020
Journal of Sedimentary Research (2020) 90 (5): 449–467.
... of lower density and borings enlarged by dissolution. Sample collected from piston core NBP93-8-7 on Ross Bank. C) Photograph of skeletal separate containing gastropods (arrows) from 34–35 cm depth in core ELT32-09 on Pennell Bank (FA 4). D) Aragonitic shell material from gastropod from 58–60 cm depth...
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Journal Article
Published: 01 August 1989
Journal of the Geological Society (1989) 146 (4): 715–720.
... 66 93 Andrew C. J. Crowe R. W. A. Finlay S. Pennell W. M. Pyne J. F. Geology and genesis of mineral deposits in Ireland 1986 Dublin Irish Association for Economic Geology Berner R. A. Sedimentary pyrite formation: an update Geochimica et Cosmochimica Acta...
Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 191–193.
.... , Pennell , W.M. , and Pyne , J.F. , eds., Geology and genesis of mineral deposits in Ireland: Dublin, Irish Association for Economic Geology , p. 377 – 417 . Ashton , J.H. , Downing , D.T. , and Finlay , S. , 1986 , The geology of the Navan Zn-Pb orebody , in Andrew , C.J...
Series: Geological Society, London, Memoirs
Published: 01 January 2016
EISBN: 9781862397088
..., Little American Basin; GCB, Glomar-Challenger Basin; RB, Ross Bank; PT, Pennell Trough; PB, Pennell Bank; JT, JOIDES Trough; MB, Mawson Bank; CB, Central Bank; CrB Crary Bank; FrIS, Franklin Island; DT, Drygalski Ice Tongue; VLB, Victoria Land Basin; McM, McMurdo Sound. ( c ) Two sets of linear features...
Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 194–198.
... that the fissures resulted from dilatational stresses probably related to differential loading caused by the accumulating banks on unstable substrates… Most fractures opened and were filled during the formation of the buildups" ( Lees and Miller, 1995 , p. 251). In conclusion, the CFC and the stage B-D cements...
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Journal Article
Journal: Economic Geology
Published: 01 March 2010
Economic Geology (2010) 105 (2): 417–442.
... of Ireland, 1994) and Everett et al. (2003) . The Waulsortian Limestone Formation developed in a ramp environment in the Courceyan as biomicrite mounds surrounded by argillaceous bioclastic limestones at moderate water depths of up to several hundred meters. Waulsortian banks dominate in the south...
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Journal Article
Published: 01 January 2001
Journal of the Geological Society (2001) 158 (1): 37–46.
... , & D.A. (eds). Mineralization in the British Isles . Chapman and Hall , London 208 - 269 . Ashton , J.H. , Downing , D.T. & Finlay , S. 1986 . The geology of the Navan Zn-Pb orebody . In : Andrew , C.J , Crowe , R.W.A , Finlay , S , Pennell , W.M...
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Journal Article
Journal: Economic Geology
Published: 01 January 2003
Economic Geology (2003) 98 (1): 31–50.
... the Tynagh lead-zinc deposit in Ireland : Nature , v. 313 , p. 128 – 131 . Banks , D.A. , 1986 , Hydrothermal chimneys and fossil worms from the Tynagh Pb-Zn deposit , Ireland , in Andrew , C.J. , Crowe , R.W.A. , Finlay , S. , Pennell , W.M. , and Pyne , J. , eds...
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Journal Article
Published: 01 June 1995
Journal of the Geological Society (1995) 152 (3): 523–534.
... of London 1995 1995 Geological Society of London Iapetus Caledonian Orogeny terranes magnetotelluric surveys References Ashton J. H. Downing D. T. Finlay S. Andrew C. J. Crowe R. W. A. Finlay S. Pennell W. M. Pyne J. F. The geology of the Navan Zn-Pb...
Journal Article
Published: 01 May 2006
Vadose Zone Journal (2006) 5 (2): 570–598.
... dodecane, octane, toluene unsaturated homogeneous Ramsburg and Pennell, 2001 surfactant–alcohol flushing combination 61 × 40 × 1.4 glass tetrachloroethene saturated heterogeneous Ramsburg and Pennell, 2002 surfactant–alcohol flushing combination 63.5 × 38 × 1.4 glass trichloroethene...
Journal Article
Journal: Economic Geology
Published: 01 January 2002
Economic Geology (2002) 97 (1): 73–91.
... et al., (1998) . It is also in concert with observations at the Silvermines and Tynagh SEDEX deposits (e.g., Russell, 1975 ; Taylor and Andrew, 1978 ; Boyce et al., 1983b , 1999 ; Banks, 1985 ). Our conclusion that a deep-seated Caledonoid structure (or suite of structures) was one...
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Journal Article
Journal: Geology
Published: 01 July 2004
Geology (2004) 32 (7): 557–560.
... and Scherer, 2004 ). These contain ∼60% centrics, well above that of true diatomaceous muds ( Fig. 3B ; Table 2 ). The diamicton of PC31 on the Pennell Bank (diamicton I), which is characterized by high diatom abundance with a strong (presumably locally derived) middle Miocene component, contains ∼70...
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