CSEDI Collaborative Research: Integrating Seismological, Rheological and Petrological Studies of Melt Production and Transport in Subduction Zones

CSEDI 合作研究：整合俯冲带熔体产生和运输的地震学、流变学和岩石学研究

• 批准号: 1067974
• 负责人: Geoffrey Abers
• 金额: $ 21.71万
• 依托单位: Columbia University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-09-15 至 2014-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1067974&HistoricalAwards=false
• 关键词: CSEDI; Collaborative; Research; Integrating; Seismological

The most explosive, deadly volcanic eruptions occur in subduction zones. Their occurrence and explosivity is intimately tied to the transport of water and other volatiles to great depth, and its release into hot mantle or along the plate boundary. Yet, understanding how volatiles released from subducting plates produce melts within the mantle wedge of subduction zones remains a challenge. A series of recent seismic and petrologic projects in subduction zones and results from the laboratory have dramatically increased the available information on these processes, and preliminary analyses of these data have begun to place bounds on the extent and depths of melting, style of melt transport, and variations between sites. This proposal plans to take the next step, the integration of geophysical observations, geochemical measurements, and rheological models, to address fundamental problems regarding melting process in the mantle. We will compare recent results from the Nicaragua-Costa Rica subduction zone, which exhibits strong along-strike variations in geophysical and geochemical observations, with those from the Marianas where volcanoes sample across-strike from the arc front to active back-arc spreading center. Broadband imaging in Central America and the Marianas indicates a region of flowing hot mantle from seismic attenuation and P-wave velocities, mantle fabric from shear-wave splitting measurements, and the geometry of melt transport from Vp/Vs anomalies. These results also show clear along-strike variations in most parameters, interpretable as variations in slab hydration, melt transport, and mantle wedge H2O content. In both regions, extensive sampling and analysis of volcanic products has provided for the first time direct measurement of magmatic water content, which appears to vary in tandem with classic indicators of slab fluid/sediment in Central America, and with distance from the arc front in the Marianas. The integration of these observations will be made possible by advances in our understanding of mantle rheology in the presence of water and melt, including both experimental and theoretical breakthroughs, for example on the behavior of melt under shearing conditions and on the physical controls on grain size, and on quantitative parameterizations of melt fabric. Our approach will be to integrate all datasets in a consistent manner, then iteratively test theoretical predictions against them. Results should distinguish models of melt generation and transport, for example of vertical porous flow, inclined flow, or ascent of cold diapirs. Once calibrated, the relationships needed to make these comparisons will be made available to interpret structure in other subduction zones and regions of melt production globally. The integration of disparate observations is a key step in making them understandable to a wide audience, and this integrated multidisciplinary approach will be tested in undergraduate classrooms and graduate seminars. The calibration of relationships between seismic observables and thermodynamic melting parameters should be broadly applicable and serve to enhance infrastructure for research.

最具爆炸性和致命性的火山爆发发生在俯冲带。 它们的出现和爆发性与水和其他挥发分向深部的输送以及它们向热地幔或沿着板块边界的释放密切相关。 然而，了解俯冲板块释放的挥发物如何在俯冲带的地幔楔内产生熔体仍然是一个挑战。 一系列最近的地震和岩石学项目在俯冲带和实验室的结果，大大增加了这些过程的可用信息，这些数据的初步分析已经开始把边界的范围和深度的熔化，熔融运输的风格，和网站之间的变化。该提案计划采取下一步措施，整合地球物理观测，地球化学测量和流变学模型，以解决有关地幔熔融过程的基本问题。我们将比较尼加拉瓜-哥斯达黎加俯冲带的最新结果，该俯冲带在地球物理和地球化学观测中表现出强烈的沿走向变化，与马里亚纳群岛的火山样品从弧前到活跃的弧后扩张中心的横向走向。 在中美洲和马里亚纳群岛的宽带成像表明，从地震衰减和P波速度，地幔结构剪切波分裂测量的流动热地幔的区域，和熔融运输的Vp/Vs异常的几何形状。 这些结果也表明，在大多数参数，可解释为板水化，熔体输送，地幔楔H2O含量的变化，沿走向的变化。在这两个区域，对火山产物的广泛取样和分析首次提供了对岩浆水含量的直接测量，岩浆水含量似乎与中美洲板状流体/沉积物的经典指标以及与马里亚纳群岛弧前缘的距离同步变化。这些意见的整合将成为可能的地幔流变学的存在下，水和熔体，包括实验和理论上的突破，例如在剪切条件下的熔体的行为和粒度的物理控制，并对熔体结构的定量参数化的理解的进步。我们的方法是以一致的方式整合所有数据集，然后迭代地测试理论预测。结果应区分熔融生成和运输的模型，例如垂直多孔流，倾斜流，或冷底辟上升。一旦校准，进行这些比较所需的关系将可用于解释全球其他俯冲带和熔体生产区域的结构。整合不同的观察结果是使它们能够被广大受众理解的关键一步，这种综合的多学科方法将在本科生课堂和研究生研讨会上进行测试。对地震观测值和热力学熔化参数之间关系的校准应具有广泛的适用性，并有助于加强研究基础设施。