Collaborative Research: Rear-arc Magmatism in the Northern Volcanic Zone of the Andes: Processes and Timescales in a Continental Rear-arc Setting

合作研究：安第斯山脉北部火山带的弧后岩浆作用：大陆弧后环境中的过程和时间尺度

• 批准号: 1019545
• 负责人: Kenneth Sims
• 金额: $ 10.95万
• 依托单位: University of Wyoming
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2010
• 资助国家: 美国
• 起止时间: 2010-08-15 至 2013-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1019545&HistoricalAwards=false
• 关键词: Collaborative; Research; Rear; arc; Magmatism

The overarching goal of this research is to investigate rear-arc petrogenetic processes in the Northern Volcanic Zone (NVZ) of the South American Andes. The NVZ is ideal for this study because it is similar in many ways to other well-studied arcs, yet it exhibits characteristics that are unique to the NVZ. This research is important because we have the opportunity to learn about the processes that mark the transition from dominantly subduction-influenced melting to the regime of MORB-type petrogenesis in South America. In addition to the primary objective, timescales will be evaluated for magma ascent and degassing in an active, calc-alkaline rear-arc volcano (El Reventador), which is important for constraining the timescales of magmagenesis in the rear-arc region. The new data set will be used to test existing models of rear-arc magmatism, while developing new models that can be applied to future arc research.The proposed research will comprise a regional, in-depth, geochemical study of Ecuadorian rear-arc volcanoes using a combination of field research, analytical work and geochemical modeling. Petrogenetic processes will be characterized using major and trace elements combined with radiogenic isotopes (Pb, Sr, Nd) and U-series on whole rocks and mineral separates. Special attention will be given to minerals in order to characterize melt inclusions and compositional variation that reveal fine-scale petrogenetic fingerprints. Timescales (i.e. crystallization and degassing rates, ages) will be determined by measuring 238U-, 230Th-, 226Ra, and 210Pb- and 210Po nuclides in mineral separates and whole rocks, using facilities at WHOI and the Universities of Wyoming and Iowa. Rigorous characterization of minerals and will be accomplished using electron microprobe and secondary ion mass spectrometry facilities at UCLA. These data will be used to evaluate contrasting models for melt formation.Intellectual Merit. This research is critical for understanding the nature of rear-arc processes in the Andean continental arc and arcs in general. The uniqueness of the NVZ lies in the compositional diversity of magmas (calc-alkaline and alkaline), the location of the rear-arc at the boundary of the South American craton, and the (possible) influence of the subducting Carnegie Ridge. Similarities to other rear-arc volcanoes provide a strong foundation for comparing our data and testing models. The application of U-series nuclides to igneous geochemistry has proven useful for determining melting and differentiation timescales in arc volcanoes, and more recently for identifying melting and differentiation processes. These currently active volcanoes in Ecuador present an opportunity to use U-series nuclides to investigate melting processes and magmatic timescales in a rear-arc setting.Broader Impacts. The Broader Impacts of this project include promoting geoscience to students, fostering international communication and emphasizing the importance of science to society. Incorporation of an interactive website as part of the field research, will bring the field experiences directly into classrooms in the U.S. and Ecuador, and provide students a sense of scientific discovery that could have a long lasting and positive impact on their lives. This project has the potential to strengthen the scientific foundation of K-12 students, with a large impact on minority students in a dominantly Hispanic community. Additionally, this funding will support a graduate student and provide funding for a junior faculty member at California State University, Los Angeles.--

本研究的首要目标是调查后弧岩石形成过程中的北方火山带（NVZ）的南美洲安第斯山脉。NVZ是这项研究的理想选择，因为它在许多方面与其他研究充分的弧相似，但它表现出NVZ独有的特征。这项研究是重要的，因为我们有机会了解的过程，标志着从主要俯冲影响熔融制度的MORB型岩石成因在南美洲的过渡。除了主要目标外，还将评估一个活跃的钙碱性弧后火山（El Reventador）的岩浆上升和脱气的时间尺度，这对限制弧后地区岩浆作用的时间尺度很重要。新的数据集将用于测试现有的弧后岩浆活动模型，同时开发可用于未来弧研究的新模型，拟议的研究将包括结合实地研究、分析工作和地球化学建模，对厄瓜多尔弧后火山进行区域性深入地球化学研究。将使用全岩和矿物分离物上的主要和微量元素以及放射性同位素（Pb、Sr、Nd）和U系列来表征成岩过程。将特别注意矿物，以表征熔融包裹体和成分变化，揭示精细尺度的成岩指纹。将使用WHOI和怀俄明州和爱荷华州大学的设施，通过测量矿物分离物和整个岩石中的238 U-、230 Th-、226 Ra、210 Pb-和210 Po核素来确定时间尺度（即结晶和脱气速率、年龄）。矿物的严格表征，并将在加州大学洛杉矶分校使用电子探针和二次离子质谱设备完成。这些数据将用于评估熔体形成的对比模型。这项研究对于了解安第斯大陆弧和一般弧的弧后过程的性质至关重要。NVZ的独特性在于岩浆成分的多样性（钙碱性和碱性），在南美克拉通的边界弧后的位置，和（可能）的影响，俯冲卡内基海岭。与其他弧后火山的相似性为比较我们的数据和测试模型提供了坚实的基础。铀系核素在火成岩地球化学中的应用已被证明有助于确定弧火山的熔融和分异时间尺度，最近还用于确定熔融和分异过程。这些目前在厄瓜多尔的活火山提供了一个机会，使用铀系列核素调查熔化过程和岩浆的时间尺度在弧后设置。该项目的更广泛影响包括向学生推广地球科学，促进国际交流，强调科学对社会的重要性。作为实地研究的一部分，一个互动网站的整合，将直接把实地经验带到美国和厄瓜多尔的课堂上，并为学生提供科学发现的感觉，这可能会对他们的生活产生持久和积极的影响。该项目有可能加强K-12学生的科学基础，对以西班牙裔为主的社区的少数民族学生产生重大影响。此外，这笔资金将支持一名研究生，并为洛杉矶的加州州立大学的一名初级教员提供资金。