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

CSEDI 合作研究：整合俯冲带熔体生产的地震学、流变学和岩石学研究

• 批准号: 1067689
• 负责人: Karen Fischer
• 金额: $ 4.01万
• 依托单位: Brown University
• 依托单位国家: 美国
• 项目类别: Continuing 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=1067689&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、最致命的火山喷发发生在俯冲带。 它们的出现和爆炸与水和其他挥发物向深处的输送以及其释放到热地幔或沿着板块边界密切相关。 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。 最近在俯冲带进行的一系列地震和岩石学项目以及实验室的结果极大地增加了有关这些过程的可用信息，并且对这些数据的初步分析已经开始对熔化的范围和深度、熔化运输的方式、以及站点之间的差异。该提案计划下一步，整合地球物理观测、地球化学测量和流变模型，解决地幔熔化过程的基本问题。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，与马里亚纳群岛的结果进行比较，马里亚纳群岛的火山从弧前到活跃的弧后扩张中心进行跨走向采样。 中美洲和马里亚纳群岛的宽带成像根据地震衰减和 P 波速度显示了流动的热地幔区域，根据剪切波分裂测量显示了地幔结构，并根据 Vp/Vs 异常显示了熔体传输的几何形状。 这些结果还显示了大多数参数明显的沿走向变化，可以解释为板片水化、熔体传输和地幔楔 H2O 含量的变化。在这两个地区，对火山产物的广泛采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片流体/沉积物的经典指标以及与弧前的距离同步变化。马里亚纳群岛。通过我们对存在水和熔体的地幔流变学的理解的进步，包括实验和理论的突破，例如在剪切条件下熔体的行为以及对晶粒尺寸的物理控制方面的突破，这些观察的整合将成为可能，以及熔体织物的定量参数化。我们的方法将以一致的方式整合所有数据集，然后针对它们迭代测试理论预测。结果应区分熔体产生和传输的模型，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让广大受众理解它们的关键一步，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。地震观测值与热力学熔化参数之间关系的校准应广泛适用，并有助于加强研究基础设施。