EAPSI:EAPSI: Integrating English and Chinese-Language Literature on the India-Asia Collision to Better Understand the Formation and Evolution of Subduction Complexes

EAPSI:EAPSI:整合有关印亚碰撞的英汉文献,更好地理解俯冲杂岩的形成和演化

基本信息

  • 批准号:
    1614206
  • 负责人:
  • 金额:
    $ 0.54万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Fellowship Award
  • 财政年份:
    2016
  • 资助国家:
    美国
  • 起止时间:
    2016-06-01 至 2017-05-31
  • 项目状态:
    已结题

项目摘要

Before India and Asia collided, forming the Himalayas, the oceanic plate between the continents was subducted beneath Asia. The material scraped off from the oceanic plate during subduction, called a subduction complex, is one of the few records of the material that entered the subduction zone. Most of the material is subducted into the mantle and lost to the geologic record. Integrating data from Chinese-language and English-language sources will provide a holistic understanding of the subduction complex in southern Tibet. This project will analyze and compile maps and data available only in China with those from English-language publications and new data generated in the United States and China. This research will be conducted at the Institute of Tibetan Plateau Research in collaboration with Professor Ding Lin and his students, who have worked extensively on the subduction complex in southern Tibet. The collaboration could lead to the discovery of new continental fragments that were subducted and a new model for how subduction complexes develop. This project will integrate the extent, deformation style, and provenance of the subduction complex in southern Tibet. Primary data will be maps, unit descriptions, U-Pb detrital zircon geochronology, and sedimentary provenance. The subduction complex in southern Tibet is a complicated, little-studied unit that records the source and deformation of materials entering the subduction zone and that is composed almost entirely of block-in-matrix mélange, far thicker and more mixed than any other documented subduction complex. This block-in-matrix style of deformation over kilometers width in a few millions of years is unexplained by current subduction zone models. This award under the East Asia and Pacific Summer Institutes program supports summer research by a U.S. graduate student and is jointly funded by NSF and the Ministry of Science and Technology of China.
在印度和亚洲碰撞形成喜马拉雅山之前,大陆之间的海洋板块被俯冲到亚洲之下。在俯冲过程中从大洋板块上刮下来的物质,称为俯冲复合体,是进入俯冲带的物质的少数记录之一。大部分物质被俯冲到地幔中,并消失在地质记录中。整合来自中文和英文来源的数据将提供对藏南俯冲杂岩的全面了解。该项目将分析和汇编仅在中国可用的地图和数据,以及来自英语出版物的地图和数据以及在美国和中国生成的新数据。这项研究将在青藏高原研究所与丁林教授及其学生合作进行,他们对西藏南部的俯冲复合体进行了广泛的研究。这项合作可能会导致发现新的大陆板块,并为俯冲复合体的发展提供新的模式。该项目将整合藏南俯冲杂岩的范围、变形样式和物源。主要数据将是地图、单元描述、U-Pb碎屑锆石年代学和沉积物源。藏南的俯冲杂岩是一个复杂的、很少被研究的单元,它记录了进入俯冲带的物质的来源和变形,几乎完全由块体-基质混杂岩组成,比任何其他有记载的俯冲杂岩都要厚得多,也更混杂。这种在数百万年内超过千米宽的块体-基质变形方式是目前的俯冲带模型无法解释的。该奖项属于东亚和太平洋夏季研究所计划,支持美国研究生的夏季研究,由NSF和中国科技部共同资助。

项目成果

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Kathryn Metcalf其他文献

Kathryn Metcalf的其他文献

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{{ truncateString('Kathryn Metcalf', 18)}}的其他基金

Collaborative Research: Evaluating the evolution of the southern Himalayan-Tibetan orogeny: What happened during Paleocene-Eocene time?
合作研究:评估南喜马拉雅-西藏造山运动的演化:古新世-始新世期间发生了什么?
  • 批准号:
    2020457
  • 财政年份:
    2021
  • 资助金额:
    $ 0.54万
  • 项目类别:
    Standard Grant

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