2016 Geochemistry of Mineral Deposits GRC

2016年矿床地球化学戈登研究会议（GRC）将汇集一批不同的科学家，他们专注于确保编织成现代社会结构的金属的可持续供应。与会者包括来自学术界、各政府机构和实验室以及采矿业和地热业的代表，他们为小组带来了他们在需要切实解决的紧迫问题方面的经验和专门知识。该会议是具有不同经验水平的国际研究人员聚集和讨论有关自然环境中金属运输和沉积地球化学问题的主要场所之一。该提案将使科学家能够展示研究成果，并与来自世界各地的科学家进行交流，这些科学家专注于我们不断发展的社会中矿石矿物的演变和可持续性。GRC是一个小型会议，最多有180名与会者，鼓励所有与会者积极参与讨论。所有与会者共同进餐，会议的形式提供了一个理想的机会，与科学家在研究领域的不同观点，也对新方法的应用进行互动。这是一个理想的场所，为早期职业研究人员与学术和工业界的高级成员进行互动，并获得他们的想法反馈。GRC将讨论的主题包括高分辨率勘探战略，岩浆和热液过程，活动热液系统，地幔楔和氧化还原过程中的交代作用和硫循环，锆石中记录的矿化系统的化学特征，各种尺度下矿石成因的动力学过程，气候变化与风化和表生矿床形成之间的关系，沉积型铜、铀矿床中的流体流动、稀土元素系统以及地质微生物学在成矿系统中的作用。

The 2016 Geochemistry of Mineral Deposits Gordon Research Conference (GRC) will bring together a diverse group of scientists who are focused on ensuring a sustainable supply of metals that are woven into the fabric of modern society. Participants include representatives from academia and various government agencies and laboratories, as well as from the mining and geothermal industries, who bring to the group their experience and expertise concerning immediate problems requiring practical solutions. The conference serves as one of the premier venues for international researchers with differing levels of experience to gather and discuss issues concerning the geochemistry of metal transportation and deposition in the natural environment. This proposal will allow scientists to present research and engage with scientists from around the world who are focused on the evolution and sustainability of ore minerals for our growing society. The GRC is a small meeting, with a maximum of 180 participants, and all participants are encouraged to actively participate in the discussions. All participants share meals together and the format of the meeting provides an ideal opportunity to interact with scientists with different perspectives in the field of research and also on applications of new methods. This is an ideal venue for early-career researchers to interact with senior members of the academic and industrial communities and to get feedback on their ideas. Topics to be discussed at the GRC will include high-resolution exploration strategies, magmatic and hydrothermal processes, active hydrothermal systems, metasomatism and sulfur cycling in the mantle wedge and redox processes, chemical signatures of mineralizing systems recorded in zircon, dynamic processes involved in ore genesis at a variety of scales, the relationship between climate change and weathering and formation of supergene deposits, fluid flow in sedimentary copper and uranium deposits, and rare earth element systems, and the role of geomicrobiology in mineralizing systems.