Je-S Combined
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Time Scales of Continental Rifting: Implications for Global Processes
spe500-11 1st pgs page 1 The Geological Society of America 18888 201320 Special Paper 500 2013 CELEBRATING ADVANCES IN GEOSCIENCE The time scales of continental rifting: Implications for global processes Cynthia J. Ebinger* Department of Earth Sciences, University of Rochester, Rochester, New York 14627, USA Jolante van Wijk* Department of Earth and Atmospheric Sciences, University of Houston, Houston, Texas 77204-5007, USA Derek Keir* National Oceanography Centre Southampton, University of Southampton, Southampton, UK ABSTRACT The rifting cycle initiates with stress buildup, release as earthquakes and/or magma intrusions/eruptions, and visco-elastic rebound, multiple episodes of which combine to produce the observed, time-averaged rift zone architecture. The aim of our synthesis of current research initiatives into continental rifting-to-rupture pro- cesses is to quantify the time and length scales of faulting and magmatism that pro- duce the time-averaged rift structures imaged in failed rifts and passive margins worldwide. We compare and contrast seismic and geodetic strain patterns during dis- crete, intense rifting episodes in magmatic and amagmatic sectors of the East African rift zone that span early- to late-stage rifting. We also examine the longer term rifting cycle and its relation to changing far-fi eld extension directions with examples from the Rio Grande rift zone and other cratonic rifts. Over time periods of millions of years, periods of rotating regional stress fi elds are marked by a lull in magmatic activity and a temporary halt to tectonic rift opening. Admittedly, rifting cycle comparisons are biased by the short time scale of global seismic and geodetic measurements, which span a small fraction of the 102–105 year rifting cycle. -
Deep Carbon Emissions from Volcanoes Michael R
Reviews in Mineralogy & Geochemistry Vol. 75 pp. 323-354, 2013 11 Copyright © Mineralogical Society of America Deep Carbon Emissions from Volcanoes Michael R. Burton Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy [email protected] Georgina M. Sawyer Laboratoire Magmas et Volcans, Université Blaise Pascal 5 rue Kessler, 63038 Clermont Ferrand, France and Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy Domenico Granieri Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy INTRODUCTION: VOLCANIC CO2 EMISSIONS IN THE GEOLOGICAL CARBON CYCLE Over long periods of time (~Ma), we may consider the oceans, atmosphere and biosphere as a single exospheric reservoir for CO2. The geological carbon cycle describes the inputs to this exosphere from mantle degassing, metamorphism of subducted carbonates and outputs from weathering of aluminosilicate rocks (Walker et al. 1981). A feedback mechanism relates the weathering rate with the amount of CO2 in the atmosphere via the greenhouse effect (e.g., Wang et al. 1976). An increase in atmospheric CO2 concentrations induces higher temperatures, leading to higher rates of weathering, which draw down atmospheric CO2 concentrations (Ber- ner 1991). Atmospheric CO2 concentrations are therefore stabilized over long timescales by this feedback mechanism (Zeebe and Caldeira 2008). This process may have played a role (Feulner et al. 2012) in stabilizing temperatures on Earth while solar radiation steadily increased due to stellar evolution (Bahcall et al. 2001). In this context the role of CO2 degassing from the Earth is clearly fundamental to the stability of the climate, and therefore to life on Earth. -
Inside Science
SPRING 2009 NEWS FROM THE ROYAL SOCIETY INSIDE SCIENCE YOUNG EXPLORERS TOUCHDOWN IN NEW ZEALAND International Expedition Prize is a ‘once in a lifetime experience’ SCIENCE TAKES TO THE STAGE The Royal Shakespeare Company premiers a new play on the emergence of modern science UPDATE FROM THE ROYAL SOCIETY This third issue of Inside Science contains early information DID YOU KNOW? about exciting plans for the Royal Society’s 350th Anniversary in 2010. The Anniversary is a marvellous STEADY FOOTING, opportunity to increase the profile of science, explore its SHAKY BRIDGE benefits and address the challenges it presents for society On its opening day, crowds of but perhaps most important of all to inspire young minds pedestrians experienced unexpected with the excitement of scientific discovery. swaying as they walked across London’s Our policy work continues to address major scientific issues Millennium Bridge. Whilst pedestrians affecting the UK. In December we cautioned the Government on fondly nicknamed it the ‘wobbly bridge’, the levels of separated plutonium stockpiled in the UK – currently physicists were busy exploring the the highest in the world. With support from our Plutonium Working Group, the Society has reasons for the phenomenon. submitted detailed comment to the Nuclear Decommissioning Authority (NDA) for a report to The view was widely held that the Government on management options for the stockpile. ‘wobble’ was due to crowd loading and Late last year we ran an extremely successful MP-Scientist pairing scheme, helping to build pedestrians synchronising their footsteps bridges between parliamentarians and some of the best young scientists in the UK. -
Local Earthquake Magnitude Scale and B-Value for the Danakil Region of Northern Afar by Finnigan Illsley-Kemp, Derek Keir,* Jonathan M
Bulletin of the Seismological Society of America, Vol. 107, No. 2, pp. 521–531, April 2017, doi: 10.1785/0120150253 Ⓔ Local Earthquake Magnitude Scale and b-Value for the Danakil Region of Northern Afar by Finnigan Illsley-Kemp, Derek Keir,* Jonathan M. Bull, Atalay Ayele, James O. S. Hammond, J.-Michael Kendall, Ryan J. Gallacher, Thomas Gernon, and Berhe Goitom Abstract The Danakil region of northern Afar is an area of ongoing seismic and volcanic activity caused by the final stages of continental breakup. To improve the quantification of seismicity, we developed a calibrated local earthquake magnitude scale. The accurate calculation of earthquake magnitudes allows the estimation of b-values and maximum magnitudes, both of which are essential for seismic-hazard analysis. Earthquake data collected between February 2011 and February 2013 on 11 three-component broadband seismometers were analyzed. A total of 4275 earthquakes were recorded over hypocentral distances ranging from 0 to 400 km. A total of 32,904 zero-to-peak amplitude measurements (A) were measured on the seismometer’s horizontal components and were incorporated into a direct linear inversion that M solved for all individual local earthquake magnitudes ( L), 22 station correction fac- C n K M A− tors ( ), and 2 distance-dependent factors ( , ) in the equation L log log A0C. The resultant distance correction term is given by − log A0 1:274336 log r=17 − 0:000273 r − 172. This distance correction term suggests that attenuation in the upper and mid-crust of northern Afar is relatively high, con- sistent with the presence of magmatic intrusions and partial melt. -
My Main Research Interests Centre on the Science Behind Volcanoes and Volcanic Behaviour
PROF. TAMSIN A. MATHER Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. Tel.: +44 (0)1865 282125 [email protected] My main research interests centre on the science behind volcanoes and volcanic behaviour. My motivation is to understand volcanoes as (a) natural hazards, (b) a key planetary scale process throughout geological time, playing a key role in change but vital for maintaining habitability and (c) natural resources (e.g., geothermal power and the development of ore deposits). I use techniques including satellite Earth Observation, remote and direct measurements of volcanic gas/aerosol, field mapping and petrological and geochemical analysis. I have also studied the emissions from an oil depot fire (Buncefield 2005) and am generally interested in the global mercury cycle as well as other biogeochemical cycles. Post-doctoral employment (Maternity leave: June-December 2007 and January-July 2010) 2014–present: Professor of Earth Sciences, University of Oxford. 2006–2014: Lecturer/Academic Fellow in Physics & Chemistry of the Earth and Environment, Dept of Earth Sciences, University of Oxford & Fellow, University College. 2005–2009: Royal Society Dorothy Hodgkin research fellow, awarded at Cambridge and moved to Oxford (Volcanic volatile emissions: from lithosphere to atmosphere) 2005: NERC fellow Parliamentary Office of Science and Technology (Report title: Carbon capture and storage) Education and Qualifications 2001–2004: Ph.D., Dept of Earth Sciences, University of Cambridge, ‘Near-source chemistry of tropospheric volcanic plumes’. NERC funded. Awarded December 2004. 1999–2000: M.Phil. (History and Philosophy of Science), University of Cambridge. Distinction. 1995–1999: M.Sci. -
The Role of Melt Composition on Aqueous Fluid Vs. Silicate Melt
The role of melt composition on aqueous fluid vs. silicate melt partitioning of bromine in magmas Anita Cadoux, Giada Iacono-Marziano, Bruno Scaillet, Alessandro Aiuppa, Tamsin Mather, David Pyle, Étienne Deloule, Emanuela Gennaro, Antonio Paonita To cite this version: Anita Cadoux, Giada Iacono-Marziano, Bruno Scaillet, Alessandro Aiuppa, Tamsin Mather, et al.. The role of melt composition on aqueous fluid vs. silicate melt partitioning of bromine in magmas. Earth and Planetary Science Letters, Elsevier, 2018, 498, pp.450-463. 10.1016/j.epsl.2018.06.038. insu-01856882 HAL Id: insu-01856882 https://hal-insu.archives-ouvertes.fr/insu-01856882 Submitted on 13 Aug 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License *Manuscript Click here to view linked References 1 2 The role of melt composition on aqueous fluid vs. silicate melt 3 partitioning of bromine in magmas 4 5 Anita Cadouxa,b,c,d, Giada Iacono-Marzianoa,b,c, Bruno Scailleta,b,c, Alessandro Aiuppae,f, 6 Tamsin A. Matherg, David M. Pyleg, Etienne Delouleh, Emanuela Gennaroa,b,c,f, Antonio 7 Paonitae 8 9 10 a Université d’Orléans, ISTO, UMR 7327, 45071, Orléans, France 11 b CNRS, ISTO, UMR 7327, 45071 Orléans, France 12 c BRGM, ISTO, UMR 7327, BP 36009, 45060 Orléans, France 13 d GEOPS, Univ. -
TRAINING REVAMPED John Underhill on the Role of Doctoral Training in Addressing 21St Century Challenges
SCIENTISTVOLUME 29 No. 08 ◆ SEPTEMBER 2019 ◆ WWW.GEOLSOC.ORG.UK/GEOSCIENTIST GEOThe Fellowship Magazine of the Geological Society of London @geoscientistmag A fresh look at geoscience education TRAINING REVAMPED John Underhill on the role of doctoral training in addressing 21st Century challenges GEOSCIENTISTS WANTED! FUTURE RESOURCES STATE OF PLAY To steward the transition Building a The worrying decline of UK to clean energy multidisciplinary community geoscience education WWW.GEOLSOC.ORG.UK/GEOSCIENTIST | SEPTEMBER 2019 | 1 WHERE IS YOUR The Geological Society FUTURE IN MINING? Career and Industry Days 2019/20 Wednesday 6 November 2019 JOIN DIGBEE AND FIND OUT... Venue: BGS, Keyworth, Nottingham, UK Wednesday 4 December 2019 Venue: Our Dynamic Earth, Edinburgh, UK Wednesday 19 February 2020 World's first expert network for mining professionals Venue: The Geological Society of London, Burlington House, London, UK www.geolsoc.org.uk/Education-and-Careers/ Free access to data from thousands of mining projects Careers-Information/Careers-Days Earn recurring income by writing geological summaries The Geological Society Career & Industry Day is an essential meeting place for geoscience students and the geoscience industry, and is the most recognised geoscience from technical feasibility studies (coming Q4 2019) careers focused forum in the country. The day will include short career and industry presentations covering different areas Free to join of geology and academia, and there will be an exhibition consisting of industry and professional bodies, and higher education institutions promoting MSc and PhD programmes. There will also be a CV and careers workshop running alongside the talks. For more info: Registration thedigbee.com/geologist This event is free to attend but there are limited numbers so pre-booking is recommended. -
Support to National and Local Resilience Building
United Nations Development Programme Country: Eritrea Programme Document Programme Title Eritrea-Support to national and local resilience building initiatives Outcome 5: Strengthened national and sectoral resilience building and climate risk management SPCF Outcome Outcome 6: Poor and vulnerable households have improved access to, and utilization of quality food and enhanced livelihood opportunities. Outcome 7: Eritrea is on track towards the achievement of MDG targets for environmental sustainability. UNDP CP output 3 of SPCF outcome 7: Community resilience to climate change Expected Country increased Programme Output UNDP CP Output 4 SPCF outcome 7: Capacity of national institutions to undertake adaptive and mitigation assessments enhanced. 1. An enabling environment for resilience-building established at national level Expected Results: 2. Sustainable livelihoods opportunities enhanced for vulnerable communities in Southern and Northern Red Sea Region and other drought affected regions 3. Enhanced community resilience to disasters, shocks and stresses Implementing Partner: Ministry of Agriculture and Ministry of Labor and Human Welfare Brief Description Eritrea is in the Horn of Africa region and within the Great East African Rift Valley. These regions are very well known to be prone to natural disaster such as drought, earthquakes, volcanic eruptions, etc. Drought is the most common hazard affecting large areas particularly the Arid and Semi-Arid Lands that cover an important part of the country’s landscape and hosts approximately 30% of the population and more than 60% of livestock population. Over the years, drought has continued to damage key livelihood activities including agriculture, livestock, water and natural resources, biodiversity among others often triggering acute food insecurity, conflict over resources and placing a heavy strain on both the local and national economy. -
A View from the City
UNIVERSITY COLLEGE OXFORD ISSUE 3 SUMMER 2015 A VIEW FROM THE CITY LEIGH INNES (1994) AND LIFE IN THE MARKETPLACE ALSO IN THIS ISSUE GEORGE CAWKWELL CELEBRATES 65 YEARS AT UNIV LOUISE TAYLOR (2011) ON THE PURSUIT OF PERFECTION ELECTION NIGHT SPECIAL WITH SIR IVOR CREWE THE MAGNA CARTA AT UNIV JOHN RADCLIFFE’S MEDICAL LEGACY FROM THE EDITOR University College Oxford OX1 4BH elcome to the Summer 2015 issue of The Martlet, the magazine for www.univ.ox.ac.uk Members and Friends of University College Oxford. I would like to Wexpress my sincere thanks to those Old Members, students, Fellows, staff www.facebook.com/univalumni and Friends of the College who contributed to this issue. [email protected] I would also like to take this opportunity to thank our extended Univ team – © University College, Oxford, 2015 Charles New and Andrew Boyle at B&M Design & Advertising Limited, who produce the magazine; Clare Holt and the team at Nice Tree Films who worked tirelessly on Produced by B&M Design & Advertising our recent videos – in particular the Election Night Special, for which they stayed www.bm-group.co.uk up well past their bedtimes! Michelle Enoch and the team at h2o creative for their splendid design concepts for the 1249 Society, and our unofficial ‘in-house’ designer Rob Moss and photographer Rachel Harrison for all their hard work on our event If you would like to share your thoughts or programmes and College photography. comments about The Martlet, please e-mail: [email protected] Enormous thanks also to Dr Robin Darwall-Smith and Frances Lawrence for their invaluable help with the In Memoriam section of the magazine. -
Glaciovolcanism at Volcán Sollipulli, Southern Chile: Lithofacies Analysis and Interpretation
Journal of Volcanology and Geothermal Research 303 (2015) 59–78 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Glaciovolcanism at Volcán Sollipulli, southern Chile: Lithofacies analysis and interpretation Stefan M. Lachowycz a,⁎, David M. Pyle a, Jennie S. Gilbert b, Tamsin A. Mather a,KatyMeec, José A. Naranjo d, Laura K. Hobbs b a Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom b Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom c British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, United Kingdom d Servicio Nacional de Geología y Minería, Avenida Santa María 0104, Santiago, Chile article info abstract Article history: Magma–ice–meltwater interactions produce diverse landforms and lithofacies, reflecting the multitude of factors Received 18 December 2014 that influence glaciovolcanism, including both magmatic (e.g., composition, eruption rate) and glacial (e.g., ice Accepted 20 June 2015 thickness, thermal regime) conditions. This is exemplified by the walls of the partly ice-filled summit caldera Available online 3 July 2015 of Volcán Sollipulli, a stratovolcano in southern Chile, which include lithofacies from eruptions of a wide range of magma compositions beneath or in contact with ice. Here we analyse these lithofacies and hence propose Keywords: new interpretations of the eruptive and glacial history of Sollipulli. The facies include a thick, laterally extensive Volcano–ice interaction fi Glaciovolcanic lithofacies sequence of fragmental glaciovolcanic deposits, comprising massive, ma c lava pillow-bearing hyaloclastite Hyaloclastite overlain by sills and then hyaloclastic debris flow deposits (similar to Dalsheidi-type sequences). -
How the Variety of Satellite Remote Sensing Data Over Volcanoes Can Assist Hazard Monitoring Efforts: the 2011 Eruption of Nabro Volcano T
Remote Sensing of Environment 236 (2020) 111426 Contents lists available at ScienceDirect Remote Sensing of Environment journal homepage: www.elsevier.com/locate/rse How the variety of satellite remote sensing data over volcanoes can assist hazard monitoring efforts: The 2011 eruption of Nabro volcano T ∗ Gaetana Ganci , Annalisa Cappello, Giuseppe Bilotta, Ciro Del Negro Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, Catania, Italy ARTICLE INFO ABSTRACT Keywords: Satellite remote sensing is becoming an increasingly essential component of volcano monitoring, especially at Lav@Hazard little-known and remote volcanoes where in-situ measurements are unavailable and/or impractical. Moreover HOTSAT the synoptic view captured by satellite imagery over volcanoes can benefit hazard monitoring efforts. By MAGFLOW monitoring, we mean both following the changing styles and intensities of the eruption once it has started, as Satellite remote sensing well as nowcasting and eventually forecasting the areas potentially threatened by hazardous phenomena in an Numerical modelling eruptive scenario. Here we demonstrate how the diversity of remote sensing data over volcanoes and the mutual interconnection between satellite observations and numerical simulations can improve lava flow hazard mon- itoring in response to effusive eruption. Time-averaged discharge rates (TADRs) obtained from low spatial/high temporal resolution satellite data (e.g. MODIS, SEVIRI) are complemented, compared and fine-tuned with de- tailed maps of volcanic deposits with the aim of constraining the conversion from satellite-derived radiant heat flux to TADR. Maps of volcanic deposits include the time-varying evolution of lava flow emplacement derived from multispectral satellite data (e.g. EO-ALI, Landsat, Sentinel-2, ASTER), as well as the flow thickness var- iations, retrieved from the topographic monitoring by using stereo or tri-stereo optical data (e.g. -
Glaciovolcanism at Volcán Sollipulli, Southern Chile: Lithofacies Analysis and Interpretation
Journal of Volcanology and Geothermal Research 303 (2015) 59–78 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Glaciovolcanism at Volcán Sollipulli, southern Chile: Lithofacies analysis and interpretation Stefan M. Lachowycz a,⁎, David M. Pyle a, Jennie S. Gilbert b, Tamsin A. Mather a,KatyMeec, José A. Naranjo d, Laura K. Hobbs b a Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom b Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom c British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, United Kingdom d Servicio Nacional de Geología y Minería, Avenida Santa María 0104, Santiago, Chile article info abstract Article history: Magma–ice–meltwater interactions produce diverse landforms and lithofacies, reflecting the multitude of factors Received 18 December 2014 that influence glaciovolcanism, including both magmatic (e.g., composition, eruption rate) and glacial (e.g., ice Accepted 20 June 2015 thickness, thermal regime) conditions. This is exemplified by the walls of the partly ice-filled summit caldera Available online 3 July 2015 of Volcán Sollipulli, a stratovolcano in southern Chile, which include lithofacies from eruptions of a wide range of magma compositions beneath or in contact with ice. Here we analyse these lithofacies and hence propose Keywords: new interpretations of the eruptive and glacial history of Sollipulli. The facies include a thick, laterally extensive Volcano–ice interaction fi Glaciovolcanic lithofacies sequence of fragmental glaciovolcanic deposits, comprising massive, ma c lava pillow-bearing hyaloclastite Hyaloclastite overlain by sills and then hyaloclastic debris flow deposits (similar to Dalsheidi-type sequences).