Textures and Tectonics of Metamorphic Crystallization

变质结晶的结构和构造

• 批准号: 0510300
• 负责人: Donna Whitney
• 金额: $ 20.09万
• 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: 2005
• 资助国家: 美国
• 起止时间: 2005-08-01 至 2009-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0510300&HistoricalAwards=false
• 关键词: Textures; Tectonics; Metamorphic; Crystallization

A general aim of this project is understanding the dynamics of metamorphic textures by integrating mineral chemical and microstructural data: reconciling geometric and chemical aspects of metamorphic textures for petrologic and structural applications. These data are obtained and integrated using a variety of approaches: electron back-scattered diffraction to determine crystallographic orietnation, electron microprobe analysis to document mineral composition and zoning, X-ray computed tomography and serial sectioning/image analysis to obtain 3-dimensional views of textures, and modeling methods to explore crystal growth in the context of deformation (e.g., Elle microstructural modeling). This investigation focuses on the growth of garnet, an important metamorphic mineral for recording pressure, temperature, time, fluid, and deformation information during metamorphism, and the basis for many studies of metamorphic crystallization processes. Specific questions being studied are: What does the presence of high-angle misorientation boundaries in morphologically coherent crystals of garnet indicate about garnet nucleation and growth? And, because these boundaries are rare in other porphyroblasts: Do garnets grow by different mechanisms than other porphyroblasts? A hypothesis to be tested is that the boundaried form during early coalescence of garnets that grow prior to development of growth zoning, and that the boundaries represent special low energy orientations.This project represents part of the Ph.D. thesis of a University of Minnesota graduate student, Eric Goergen, and involve international collaboration with Dr. Mark Jessell (Toulouse). The research also involves undergraduate research assistants at Minnesota and summer interns from other institutions as part of an NSF-REU site. Results are being incorporated into a new teaching module that focuses on the Dutchess County, NY, Barrovian sequence; the module is distributed through the Teaching Petrology website.

该项目的总体目标是通过整合矿物化学和显微结构数据来了解变质结构的动力学：协调岩石学和结构应用中变质结构的几何和化学方面。这些数据是使用各种方法获得和整合的：电子背散射衍射以确定晶体学取向，电子探针分析以记录矿物成分和分区，X射线计算机断层扫描和连续切片/图像分析以获得纹理的三维视图，以及建模方法以探索变形背景下的晶体生长（例如，Elle微观结构建模）。石榴石是记录变质作用过程中压力、温度、时间、流体和变形信息的重要变质矿物，也是许多变质结晶过程研究的基础。正在研究的具体问题是：什么是存在的高角度的取向差边界在形态连贯的晶体石榴石表明石榴石形核和生长？而且，因为这些边界在其他成斑晶中很少见：石榴石的生长机制与其他成斑晶不同吗？一个有待检验的假设是，在石榴石的早期聚结过程中，在生长分区的发展之前生长的边界形式，并且边界代表特殊的低能取向。这是明尼苏达大学研究生Eric Goergen的毕业论文，涉及与Mark Schuell博士（图卢兹）的国际合作。这项研究还涉及明尼苏达州的本科研究助理和来自其他机构的暑期实习生，作为NSF-REU网站的一部分。结果被纳入一个新的教学模块，重点是达奇斯县，纽约州，巴罗维序列;该模块是通过教学岩石学网站分发。