Support of an AGU Chapman Conference: Fifth International Orogenic Lherzolite Conference: Shallow Mantle Composition and Dynamics, September 22-26, 2008, Mount Shasta Resort, CA

AGU Chapman 会议的支持：第五届国际造山二辉橄榄岩会议：浅地幔成分和动力学，2008 年 9 月 22-26 日，加利福尼亚州沙斯塔山度假村

• 批准号: 0822430
• 负责人: Henry Dick
• 金额: $ 2.31万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2008
• 资助国家: 美国
• 起止时间: 2008-08-01 至 2009-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0822430&HistoricalAwards=false
• 关键词: Support; AGU; Chapman; Conference; Fifth

Intellectual merit. This proposal requests support for travel and meeting costs for an American Geophysical Union Chapman Conference on Shallow Mantle Composition and Dynamics to be held September 22 to 26, 2008, at the Mount Shasta Resort, Mount Shasta, California (http://www.agu.org/meetings/chapman/2008/ccall/). This will be the fifth International Orogenic Lherzolite Conference, with previous conferences held near the peridotite massifs of Lanzo (N Italy, 1990), Ronda (Spain, 1995), Finero (N Italy, 1999), and Horoman (Japan, 2002). The year 2008 marks the 31st anniversary of the 1977 Chapman Conference on Partial Melting in the Earth?s Upper Mantle held in the Josephine peridotite, one of two field trip locales for the current meeting. This venue was selected as a result of unanimous request of the participants at the previous Conference in this series.Broader impacts. The overall objective of these meetings is to assemble specialists in studies of peridotite massifs and upper mantle processes for a field conference, where recent results and key outcrops can be discussed in a group setting. This conference will incorporate a broader range of topics than previously, and includes influential scientists in rock mechanics and low-temperature alteration processes in the organizing committee to ensure that this is a success. Topics to be covered will include melting processes, melt transport, metasomatism, localized and regional deformation, formation and nature of plate boundaries, mechanisms of intermediate depth earthquakes, and both geochemistry and physical processes of low temperature alteration. An attendance of between 80 and 120 international scientists is anticipated, including ~20% graduate students and post doctoral researchers.

智力优点。该提案要求为2008年9月22日至26日在加利福尼亚州沙斯塔山（http://wwwww.agu.org.org.org.org.org.org/meetings/chapman/2008/2008/ccall//）举行的美国地球物质组成和动态的美国地球物理联盟查普曼会议的旅行和满足费用支持。这将是第五届国际造山赖唑群会会议，以前的会议在兰佐（Nitaly，1990年），朗达（Spain，1995），芬罗（1995），芬罗（Nitaly）（Nitaly，1999）和霍曼（Horoman）和霍曼（Horoman）（日本，2002年）举行。 2008年是1977年查普曼（Chapman）大会31周年，该会议在地球上的层矿山上的地幔中举行，在约瑟芬橄榄石（Josephine Peridotite）举行，这是当前会议的两个实地考察地区之一。由于参与者在本系列的上一次会议上的一致要求，因此选择了该场所。这些会议的总体目的是在田野会议的橄榄岩地层和上地幔过程中组装专家，在该研究中，可以在小组环境中讨论最近的结果和关键露头。该会议将比以前更广泛的主题纳入更广泛的主题，并包括组织委员会的摇滚力学和低温改变过程的有影响力的科学家，以确保这是成功的。要涵盖的主题将包括熔化过程，熔体运输，交代，局部和区域变形，板边界的形成和性质，中间深度地震的机制以及低温改变的地球化学和物理过程。预计将有80至120名国际科学家的出席率，其中包括约20％的研究生和博士后研究人员。