2016 Geochemistry of Mineral Deposits GRC

2016年矿床地球化学戈登研究会议（GRC）将汇集不同群体的科学家，他们专注于确保金属的可持续供应，这些金属被编织到现代社会的结构中。与会者包括来自学术界和各政府机构和实验室的代表，以及来自采矿和地热工业的代表，他们为小组带来了他们对需要实际解决的紧迫问题的经验和专门知识。会议为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的地球化学问题提供了一个主要场所。这项提案将使科学家们能够展示研究成果，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的进化和可持续性。GRC是一个小型会议，最多180人参加，鼓励所有与会者积极参与讨论。所有参与者一起用餐，会议的形式提供了一个理想的机会，与在研究领域和新方法应用方面具有不同观点的科学家进行互动。这是一个理想的场所，早期职业研究人员与学术界和工业界的资深成员进行互动，并获得他们的想法反馈。会议将讨论高分辨率勘探策略、岩浆和热液过程、活动热液系统、地幔楔中的交代作用和硫循环以及氧化还原过程、锆石中记录的矿化系统的化学特征、各种尺度的成矿动力学过程、气候变化与风化的关系以及表生矿床的形成。沉积型铜铀矿床的流体流动与稀土元素系统，以及地球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.