<div dir="ltr"><br><div class="gmail_quote"><div dir="ltr" class="gmail_attr">---------- Forwarded message ---------<br>From: <strong class="gmail_sendername" dir="auto">The Geological Society of London</strong> <span dir="auto"><<a href="mailto:news@newsletters.geolsoc.org.uk">news@newsletters.geolsoc.org.uk</a>></span><br>Date: Mon, Oct 24, 2022 at 12:34 PM<br>Subject: Open Access Week from the Geological Society of London<br>To: Editorial team<br></div><br><br><div class="msg9056727982876441701"><u></u>
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<td align="left" style="font-family:'Trebuchet MS',Helvetica,Arial,sans-serif;font-size:14px;line-height:18px;color:#000000" width="100%"><span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">To mark International Open Access Week we have collated some of our new and popular Open Access content, as well as news related to Open Access. We hope you enjoy reading this diverse range of articles.</span><br>
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<span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">Kind regards, <br>
The Geological Society Publishing House</span></span></td>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTgIMSsE2tDU81H5xblRD" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/jgs2022-018.01.jpg?crop=385x207x84x201x180&size=170x0&w=BxyTqzZ94Tp_dC27eLItZKUEBm9I" style="display:block;border:none" width="170"></a>
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<td align="left" style="font-family:'Trebuchet MS',Helvetica,Arial,sans-serif;font-size:14px;line-height:18px;color:#000000;font-weight:normal" width="100%"><span style="padding:0;margin:0;font-size:14px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif"><span style="padding:0;margin:0;color:#c7a32b">Open Access </span></span></span><strong><span style="padding:0;margin:0;color:#000080"><span style="padding:0;margin:0;font-size:14px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">Arctic sediment routing during the Triassic: sinking the Arctic Atlantis</span></span></span></strong><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">By Albina Gilmullina, Tore Grane Klausen, Anthony George Doré, Hallgeir Sirevaag, Anna Suslova, and Christian Haug Eide<br>
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Opening of the Arctic Ocean has been the subject of much debate, and the placement of terranes in the Early Mesozoic remains a crucial part of this important discussion. Several continental terranes complicate the palaeogeographical reconstruction. One such terrane is Crockerland, which has been inferred to explain sediment distribution in the Arctic throughout the Mesozoic…<a href="http://geologicalsociety.msgfocus.com/c/14nTiOFtKwrIX0STwVCtozZ" style="font-weight:bold;text-decoration:none" target="_blank">read more</a></span></span></td>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTkUy52oQYg7DLmLHLril" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Content_images/petgeo2021-090.03_1_.jpg?crop=491x353x85x172x201&size=170x0&w=BPbn-FiDqGoXHX0djqjEz06-ELFk" style="display:block;border:none" width="170"></a>
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<td align="left" style="font-family:'Trebuchet MS',Helvetica,Arial,sans-serif;font-size:14px;line-height:18px;color:#000000;font-weight:normal" width="100%"><span style="padding:0;margin:0;font-size:14px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif"><span style="padding:0;margin:0;color:#c7a32b">Open Access </span><strong><span style="padding:0;margin:0;color:#000080">New insights into the structure, geology and hydrocarbon prospectivity along the central-northern Corona Ridge, Faroe–Shetland Basin</span></strong></span></span><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">By Lucinda K. Layfield, Nick Schofield, David W. Jolley, Simon P. Holford, Tudor-Remus Volintir, Ben A. Kilhams, David K. Muirhead, and Helen Cromie<br>
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The Faroe–Shetland Basin (FSB) is one of the only significant exploration frontiers remaining on the UK Continental Shelf. Over half of the basin's discovered reserves and resources lie along two intra-basinal highs, the Corona Ridge and the Rona Ridge. In contrast to the Rona Ridge, the central-northern Corona Ridge has received much less attention...<a href="http://geologicalsociety.msgfocus.com/c/14nTn0qGkhgdzeoDcBN3u0H" style="font-weight:bold;text-decoration:none" target="_blank">read more</a></span></span></td>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTo3mYYdsQdMM47wPHvmS" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Content_images/qjegh2022-022.01.jpg?crop=447x115x173x274x258&size=170x0&w=Bxh_dyeDHG0YLQFhr-Ht4a20KOP8" style="display:block;border:none" width="170"></a>
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<td align="left" style="font-family:'Trebuchet MS',Helvetica,Arial,sans-serif;font-size:14px;line-height:18px;color:#000000;font-weight:normal" width="100%"><span style="padding:0;margin:0;font-size:14px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif"><span style="padding:0;margin:0;color:#c7a32b">Open Access </span><strong><span style="padding:0;margin:0;color:#000080">High-resolution 3D geological modelling of heterogeneity in poorly exposed glacial deposits using sedimentary and glaciotectonic architectural element analysis: a case example from Sellafield in west Cumbria, UK</span></strong></span></span><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">By Nicholas T. Smith, Jonathan W. Merritt, and Emrys R. Phillips<br>
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Three-dimensional modelling of superficial geology is challenging, particularly for complex industrial sites such as the Sellafield nuclear site, Cumbria, UK. A lithostratigraphic approach is sufficient to show distribution of key units where only a general understanding of hydrogeology is required…<a href="http://geologicalsociety.msgfocus.com/c/14nTq9fAg5S5wTwVXmUZy5e" style="font-weight:bold;text-decoration:none" target="_blank">read more</a></span></span></td>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTrcbSU24IbrUmShXDzrp" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Content_images/esss-02-10054-g003.jpg?crop=1072x33x445x627x555&size=170x0&w=BFyJKfm0RFlqiGzqsT3ieHrbXaOU" style="display:block;border:none" width="170"></a>
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<td align="left" style="font-family:'Trebuchet MS',Helvetica,Arial,sans-serif;font-size:14px;line-height:18px;color:#000000;font-weight:normal" width="100%"><span style="padding:0;margin:0;font-size:14px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif"><span style="padding:0;margin:0;color:#c7a32b">Open Access </span><strong><span style="padding:0;margin:0;color:#000080">Time Zero for Net Zero: A Coal Mine Baseline for Decarbonising Heat</span></strong></span></span><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">By <span style="padding:0;margin:0;background:white">Alison A. Monaghan, </span>Luke Bateson, Adrian J. Boyce, <span style="padding:0;margin:0;background:white">Neil M. Burnside, Rebecca Chambers, </span>Julia R. de Rezende, Eilidh Dunnet, Paul A. Everett, Stuart M. V. Gilfillan, Muhammad S. Jibrin, Gareth Johnson<span style="padding:0;margin:0;background:white"><span style="padding:0;margin:0;font-variant-ligatures:normal"><span style="padding:0;margin:0;font-variant-caps:normal"><span style="padding:0;margin:0"><span style="padding:0;margin:0"><span style="padding:0;margin:0"><span style="padding:0;margin:0;text-decoration-style:initial"><span style="padding:0;margin:0;text-decoration-color:initial"><span style="padding:0;margin:0;float:none"><span style="padding:0;margin:0;word-spacing:0px">, </span></span></span></span></span></span></span></span></span>Richard Luckett</span>, <span style="padding:0;margin:0;background:white">Donald John MacAllister, </span>Alan M. MacDonald, John W. Moreau, Laura Newsome, Alessandro Novellino, Barbara Palumbo-Roe, Ryan Pereira, Douglas Smith, <span style="padding:0;margin:0;background:white">Mike J. Spence, </span>Vanessa Starcher, Helen Taylor-Curran, Christopher H. Vane, Thomas Wagner<span style="padding:0;margin:0;background:white"><span style="padding:0;margin:0;font-variant-ligatures:normal"><span style="padding:0;margin:0;font-variant-caps:normal"><span style="padding:0;margin:0"><span style="padding:0;margin:0"><span style="padding:0;margin:0"><span style="padding:0;margin:0;text-decoration-style:initial"><span style="padding:0;margin:0;text-decoration-color:initial"><span style="padding:0;margin:0;float:none"><span style="padding:0;margin:0;word-spacing:0px"> and </span></span></span></span></span></span></span></span></span>David B. Walls</span></span></span></td>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTul0MPQGA972FD35zDvW" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Content_images/jgs2022-022.03.jpg?crop=1015x3x560x355x373&size=170x0&w=B67sFL8OUuusw_8u98_VOICEyYGs" style="display:block;border:none" width="170"></a>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">By Xiujuan Bao, Hanqing Zhao, Shihong Zhang, Xinlei Li, Wengang Tan, Chao Li, Huaichun Wu, Haiyan Li, and Tianshui Yang<br>
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Length of day (LOD) varies throughout Earth history, dictated in the long term by the retreat of the Moon and growth of Earth's core. Reconstruction of LOD in deep time has greatly benefited from analyses of the orbital cycle from geological records. The Precambrian database, however, is very limited…<a href="http://geologicalsociety.msgfocus.com/c/14nTxtPGLFis6MaYnOdvHAt" style="font-weight:bold;text-decoration:none" target="_blank">read more</a></span></span><br>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTywLZpBv4LkypiJg9IWE" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Random_Images/OA.png?size=100x0&w=BbX8d910DrV7kbYe6DGuzA2MIjA8" style="display:block;border:none" width="100"></a>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">The Geological Society’s open access read and publish agreements provide seamless and unlimited open access publishing for corresponding authors at participating institutions – including UK, Germany, Australia, New Zealand, and others.</span></span>
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<td align="left" style="font-family:'Trebuchet MS',Helvetica,Arial,sans-serif;font-size:14px;line-height:18px;color:#000000" width="100%"><span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">Under the terms, any article submitted by a corresponding author to a hybrid Geological Society publication in the Lyell Collection through 2022, which goes on to be accepted, will be published on an open access basis and the fee waived i.e. no charge to the author.</span></span><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">This is an easy route to compliance under the UKRI open access policy, which came into effect on 1 April 2022.</span></span><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">If your institution is not currently signed-up to a transformative read and publish agreement but might be interested to do so, please do share details with your librarian or reach out to your contact at GSL Publishing House.</span></span><br>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">View the <a href="http://geologicalsociety.msgfocus.com/c/14nTACEAHtUk4rjh8zlrLF0" style="font-weight:bold;text-decoration:none" target="_blank">list of participating institutions</a></span></span><br>
<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif"><a href="http://geologicalsociety.msgfocus.com/c/14nTBFATlq6WIZGI3uo5N1b" style="font-weight:bold;text-decoration:none" target="_blank">Find out more here</a></span></span></td>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">The hybrid journals published by the Society have Transformative Journal status. These are journals that demonstrate an active commitment to transitioning to a fully Open Access journal through a gradual increase in published Open Access content. Authors are generally allowed to use their funding to pay for APCs in these journals and comply with their funders’ Open Access policy even if their institution is not signed up to a transformative read and publish agreement.<br>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTCIxbZmjzny48YpqJOnm" style="font-weight:bold;text-decoration:none" target="_blank">Find out more about the Geological Society Open Access policy</a></span></span></td>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTDLtuDiwc26rzTktnPJx" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Random_Images/membership_card_2022.jpg?crop=954x0x0x669x597&size=100x0&w=BpXgWK_ZFQRvv9PPmcDXTrGoZZMs" style="display:block;border:none" width="100"></a>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">Fellows have access to a discounted Open Access Article Processing Charge for Geological Society owned journals (where the corresponding author or at least half the authors are Fellows or student members). <a href="http://geologicalsociety.msgfocus.com/c/14nTEOpNheIOGEP0Ofw1R5I" style="font-weight:bold;text-decoration:none" target="_blank">Find out more</a></span></span>
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<a href="http://geologicalsociety.msgfocus.com/c/14nTFRm5VaVrldcrJayFSrT" style="font-weight:bold;display:block;text-decoration:none" target="_blank"><img alt="" border="0" src="http://geologicalsociety.msgfocus.com/i/amf_geolsoc/project_204/Journal/es3_cover_jpeg.jpg?size=100x0&w=BwgTElHDlOyF4DCKbvShmEoMnTXk" style="display:block;border:none" width="100"></a>
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<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">ES³ is the Geological Society's full open access journal. The journal’s scope covers the broad spectrum of Earth science, and is headed up by Chief Editor Dr Kathryn Goodenough (British Geological Survey).<br>
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The journal provides authors with a dedicated route to Open Access publication, and welcomes engagement from both new and previous contributors.<br>
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To read the papers head to the <a href="http://geologicalsociety.msgfocus.com/c/14nTJ0aZQZxjiSkKtVGBWwq" style="font-weight:bold;text-decoration:none" target="_blank">ES³ website</a>.</span></span><br>
<span style="padding:0;margin:0;font-size:12px"><span style="padding:0;margin:0;font-family:Trebuchet MS,Helvetica,sans-serif">Submit your paper, for review, on the <a href="http://geologicalsociety.msgfocus.com/c/14nTK37iuVJVXqIboQJfXSB" style="font-weight:bold;text-decoration:none" target="_blank"><span style="padding:0;margin:0;color:null">ES<sup>3 </sup></span>website</a></span></span>
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