U.S.-China Cooperative Research: Mechanisms of Pluton Emplacement; Study of East China and North America Batholiths

美中合作研究：岩体侵位机制；

• 批准号: 9507687
• 负责人: Christian Teyssier
• 金额: $ 2.86万
• 依托单位: University of Minnesota-Twin Cities
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1995
• 资助国家: 美国
• 起止时间: 1995-08-01 至 2000-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9507687&HistoricalAwards=false
• 关键词: U.S.; China; Cooperative; Research; Mechanisms

9507687 Teyssier This award supports collaboration between Christian Teyssier, University of Minnesota, and Wen TianFang, China University of Geosciences on Mechanisms of pluton emplacement. The PI's core research is focused on testing the hypothesis that granitoid plutons are emplaced in the upper crust in tensional bridges between crustal-scale fractures. This research is presently being conducted in the Sierra Nevada batholith, a major continental arc in the Circum-Pacific. The aim of the proposed project is to extend the analysis of pluton-emplacement mechanism to East China in areas that underwent similar tectonic processes as the Sierra Nevada. The methods used in the Sierra Nevada involve structural analysis in the field and in the laboratory, and the analysis of anisotropy of magnetic susceptibility of granitoid rocks in order to retrieve information about magma flow during emplacement. In East China, it will be possible to add a new component to this project, the gravity-anomaly analysis of plutons, in order to define their three-dimensional shape. This technique is difficult to apply successfully within the Sierra Nevada because the rugged topography induces large errors. In contrast, the plutons of East China are exposed in areas of smooth topography, ensuring that this analysis will provide a useful signal above the background noise. Defining the three-dimensional shape of plutons, and particularly the root zones of plutons, is a key element in the hypothesis to be tested. The Chinese group, led by Professor Wan, has corresponded with the PI regularly in the past two years on the methods of pluton emplacement analysis. The two study areas in Eastern China were carefully chosen - in terms of tectonic similarity to the Sierra Nevada, good field exposure, and gentle topography - to insure meaningful results from the analyses and thereby test different models of granitoid emplacement effectively. The Chinese group brings their knowledge of the regional geology and their experience in the field. The American group brings techniques of rock magnetism and gravimetry applied to plutons. All stages of the work, from field analysis to laboratory measurements, will be conducted jointly, and the results will be written collaboratively.

9507687泰西尔 该奖项支持明尼苏达大学的Christian Teyssier和中国地质大学的温天芳在岩体侵位机制方面的合作。 PI的核心研究集中在测试假设，花岗岩类岩体侵位在地壳规模的裂缝之间的张性桥梁的上地壳。 这项研究目前正在内华达州岩基进行，这是环太平洋的一个主要大陆弧。 该项目的目的是将对岩浆侵位机制的分析扩展到中国东部经历了与内华达州山脉相似构造过程的地区。 在内华达州使用的方法包括野外和实验室的结构分析，以及花岗岩类岩石磁化率各向异性的分析，以检索有关侵位期间岩浆流动的信息。 在中国东部，将有可能为这一项目增加一个新的组成部分，即岩体的重力异常分析，以确定其三维形状。 这种技术很难在内华达州山脉内成功应用，因为崎岖的地形会导致很大的误差。 相比之下，中国东部的岩体暴露在地形平坦的地区，确保这种分析将提供高于背景噪音的有用信号。 确定岩体的三维形状，特别是岩体的根区，是有待检验的假设的一个关键要素。 在过去的两年里，由万教授领导的中国小组定期与PI就岩体定位分析方法进行通信。 中国东部的两个研究区是精心挑选的--在构造上与内华达州相似，野外暴露良好，地形平缓--以确保分析结果有意义，从而有效地检验花岗岩类侵位的不同模型。 中国小组带来了他们的区域地质知识和在该领域的经验。 美国小组带来了应用于岩体的岩石磁学和重力测量技术。 从现场分析到实验室测量的所有阶段的工作都将联合进行，结果将由合作编写。