Sponsored student reportsMany organisations, including the GSA Specialist Groups andDivisions, sponsored students to attend the 34th IGC. Thankyou to all the groups that sponsored students. Here’s whatsome students had to say about their experiences.Johannes HammerliThanks to the support by the Specialist Group in Geochemistry,Mineralogy and Petrology (GSA) (SGGMP), I was able to attendthe IGC in Brisbane in early August. As my PhD project focuseson trace element behaviour and Nd, Sr and O isotope systematicson prograde metamorphism, I was particularly interested in thesessions ‘Understanding migmatites’ and ‘Accessory phases andtrace elements in metamorphic processes’.The keynote presentation by Ed Sawyer ‘Composition andmicrostructure in understanding migmatites’ was definitely one<strong>of</strong> the many highlights <strong>of</strong> the conference. All talks in the abovesessions were very well attended and I was given the opportunityto present my research ‘In-situ Nd and Sr isotope measurementson accessory minerals from a prograde LP/HT sequence — Insightsinto isotope equilibration during metamorphism’ in the lattersession.There was plenty <strong>of</strong> time for discussions during the breaks(on the almost non-ending route to find some c<strong>of</strong>fee) — andthese have already led to fruitful collaborations. Within thescientific program there was time to socialise with a few refreshments,for instance at the BBQ organised by the EconomicGeology Research Unit (EGRU) <strong>of</strong> James Cook University. Thewhole conference was very well organised … but if only therewas beer at the poster sessions ...JOHANNES HAMMERLISchool <strong>of</strong> Earth and Environmental SciencesJames Cook University, TownsvilleArticle based on SGGMP Newsletter September 2012: articleused with permission.Gisela CobenasI am pleased to have attended the IGC and I am very thankful tothe SGGMP for their financial support. This conference hasbenefited my research immensely. I had the opportunity topresent at the ‘SW Pacific Magmatism’ special session. My talkwas entitled ‘Metal evolution during differentiation <strong>of</strong>calc-alkaline magmas (Hunter Ridge, SW Pacific)’. The feedbackI was given was very positive and it was great to discuss my resultsand findings with other key researchers in my field.I also attended the sessions on ‘Footprints <strong>of</strong> mineralisedsystems: new concepts and data for exploration’, ‘Orogen todistrict-scale structural and tectonic controls on porphyryand epithermal deposits’, ‘Giant and super giant orebodies’,‘Magmatism in extensional environments (continental rifts andMORB)’ and ‘Origin and evolution <strong>of</strong> marsupials’. I found all thesesessions very interesting, well structured and informative.Finally, as I intend to become a researcher after completingmy PhD, attending the conference was an important opportunityto meet potential sponsors to help me develop my career — andundoubtedly has helped me to expand my network.GISELA COBENASPhD student ARC Centre <strong>of</strong> Excellence in Ore Deposits (CODES)University <strong>of</strong> Tasmania, HobartArticle based on SGGMP Newsletter September 2012: articleused with permission.Ed SaundersI recently received sponsorship from the SGGMP group <strong>of</strong> GSA toattend the ICG, where I presented some results from my PhDresearch. My project focuses on the gold geochemistry in theupper mantle, and I have been using in situ analytical techniquesto measure the sulfide chemistry from mantle xenoliths tounderstand how gold behaves during mantle processes. At theIGC, I presented results from xenoliths from Svalbard, NorthAtlantic, which show a relationship between silicate and sulfidemetasomatism, and how these metasomatic events alter theAu concentration within the mantle.I attended a wide array <strong>of</strong> sessions at IGC, all <strong>of</strong> which werevery interesting. Several talks stood out as highlights. The sessionon the global sulfur cycle and its impact on metallogenesis wasparticularly interesting. The keynote by Cin-Ty Lee in this sessiondiscussing the use <strong>of</strong> Cu systematics in understandingcrust–mantle differentiation was fascinating. The follow-upinvited talk by Iain Pitcairn looking into constraints on themobility <strong>of</strong> gold during metamorphism was also extremelyrelevant. This session in particular, and the conference in general,definitely gave me a new perspective on my research, and newavenues that I can use my data to explore.ED SAUNDERSPhD student, Macquarie UniversityArticle based on SGGMP Newsletter September 2012: articleused with permission.Kieran MeaneyAs an Honours student in geology, fresh out <strong>of</strong> my undergraduatedegree and halfway through my research project, being <strong>of</strong>feredthe opportunity to attend such a large event as the IGC was quitespecial. I ended up spending a week in Brisbane with some <strong>of</strong> myfellow students and academic mentors, and was able to learn somany new ideas and concepts in geology, many <strong>of</strong> which werevery relevant to my own project. It was fantastic to see the peoplewho had taught me over the years present some <strong>of</strong> their work onan international stage. Even simple things, such as just being ableto put some faces to the names I had seen so <strong>of</strong>ten attached topublished works, made the whole experience very interesting.In addition to all the lectures and presentations, I attended apr<strong>of</strong>essional development workshop on how to communicategeoscience to the general public. So at the very least I cannow better explain to my family and friends what it is thatI actually do!<strong>TAG</strong> December 2012| 41
Johannes Hammerli. Imagecourtesy Johannes Hammerli.Gisela Cobenas at Cape Hauy in the Tasmanpeninsula, where the dolerite columnformations are spectacular. Image courtesyFrancisco Testa.Ed Saunders on an undergraduate fieldtripto the Ormiston Gorge in the NorthernTerritory, which he attended as a tutor.Image courtesy Charmaine Thomas.Kieran Meaney with hisposter at the 34th IGC.Image courtesy KieranMeaney.The most exciting and rewarding moment <strong>of</strong> all, however, wasthe chance to display a poster <strong>of</strong> my own work and the resultsfrom my project so far. It was a great feeling to have otherresearchers see my work, ask questions with genuine interest anddiscuss what affect my work might have on theirs. In momentslike these there is a great feeling <strong>of</strong> accomplishment, and not thekind that I was expecting to feel throughout my Honours year.I would like to thank everyone who supported me, andespecially my supervisor, Alan Collins, for putting me up to thechallenge <strong>of</strong> presenting. I would also like to thank the South<strong>Australia</strong>n Division <strong>of</strong> the GSA for their generous financialsponsorship, without which I may not have been able to attend.KIERAN MEANEYHonours student, University <strong>of</strong> AdelaideNick LyonsThe ICG was a fantastic opportunity for a young geologist likeme to meet and interact with the global geological communityfor the first time. I feel very fortunate to have attended.There were many, many highlights <strong>of</strong> the conference, butthree specifically come to mind.The first was the chance to present a poster about some <strong>of</strong>the work I had completed from my 2012 Honours thesis Evidence<strong>of</strong> magmatic hydrothermal mineralisation at Kanmantoo Au–Cudeposit, South <strong>Australia</strong>. Some <strong>of</strong> the insightful feedbackI received about my work I will carry through the remainder <strong>of</strong>my geological career. The chance to ‘talk rocks’ with geologistsfrom around the world will always be a great memory.The second highlight was the chance to listen to some <strong>of</strong> thevery insightful, ground-breaking research that is currently beingundertaken on some <strong>of</strong> the largest ore deposits around the world.Presentations on the porphyry deposits <strong>of</strong> South America andepithermal deposits <strong>of</strong> the Indonesian archipelago, the modelsfor formation and challenges when exploring for them wereintriguing.The third highlight was seeing the quality <strong>of</strong> representationfrom <strong>Australia</strong>, and the immense interest in <strong>Australia</strong>n geologyfrom the international community. The research and development<strong>of</strong> iron-oxide–copper–gold (IOCG) deposits in <strong>Australia</strong> and thecontribution that <strong>Australia</strong> is making towards these uniquedeposits was encouraging to see. Contributions from <strong>Australia</strong>nresearchers to the supercontinent cycle and global tectonics werealso <strong>of</strong> great interest, as was the pride shown towards the<strong>Australia</strong>n geological community.I would like to thank the GSA SA Division, and the scholarshipthat I received, without which I would not have been able toattend and be involved in this once-in-a-lifetime experience.Rock on GSA SA!!NICK LYONSHonours student, University <strong>of</strong> AdelaideYuan MeiI would like to acknowledge the SGGMP and the South <strong>Australia</strong>Division <strong>of</strong> the GSA for sponsoring my registration to attend IGCthis year.I gave an oral presentation in the session ‘Global sulfur cycleand impact on metallogenesis’ with the title ‘Speciation andthermodynamic properties <strong>of</strong> d 10 transition metals: insights fromab-initio molecular dynamics simulations’. In this talk, I sharedthe idea <strong>of</strong> applying computational chemistry methods to get amolecular-level insight into the physical and chemical factorsthat affect ore transport and deposition over a wide range <strong>of</strong>conditions. In particular, I presented my recent studies that showhow molecular dynamics simulation helps us to understand thecoordination chemistry and structural properties <strong>of</strong> metalcomplexation, how to derive the thermodynamic properties andbuild metal transport-deposition models, and to predict the metalspeciation for experimentally unknown systems.42 |<strong>TAG</strong> December 2012