Collaborative Research: Fold Form, Strain, and Mechanics at the Whaleback Anticline: New Approaches to a Classic Field Locality

合作研究：鲸背背斜的褶皱形式、应变和力学：经典野外地点的新方法

• 批准号: 1523909
• 负责人: Juliet Crider
• 金额: $ 15.98万
• 依托单位: University of Washington
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2015
• 资助国家: 美国
• 起止时间: 2015-09-01 至 2019-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1523909&HistoricalAwards=false
• 关键词: Collaborative; Research; Fold; Form; Strain

Folded rock layers are among the most fundamental, instructive and charismatic geologic structures. Folds are studied to investigate mountain building, to understand the engineering properties of rock, to predict the underground movement of water or hydrocarbons, and to give insight into the fundamental processes of folding itself. These applications rely on the accurate interpretation of rock deformation within a fold. Various conceptual and mathematical models predict fold-related deformation. To assess the capabilities of such predictive models, data from natural examples are required. This can be challenging, because most geologic folds at Earth's surface are only partially exposed, with major portions of the fold either buried underground or eroded away. The Whaleback Anticline in Bear Valley, east-central Pennsylvania, is a unique locale where a complete large-scale fold is exposed; strip mining for coal early in the last century revealed it in exquisite detail. This outstanding exposure permits observation of the complete three-dimensional form of the folded surface and provides a highly detailed record of deformation across the fold. This project will use cutting-edge digital imaging techniques and traditional geologic fieldwork to produce a comprehensive data set against which to test hypotheses about folding. In addition to the scientific goals of the project, the research is contributing to achievement of societally relevant outcomes in the areas of science, technology, engineering, and mathematics (STEM) education, including the development of a diverse, globally competitive STEM workforce through graduate and undergraduate student training; the development of research infrastructure of three universities; the broadening of participation of underrepresented groups in science; and increased public scientific literacy and public engagement with science and technology. The Whaleback Anticline is an important educational field trip location for dozens of university geology departments throughout the eastern United States, and it is a well-used recreation site for the local community. As part of this proposed project we will preserve, expand and curate geological observations from the Whaleback, for use by researchers, educators and the community. Deformation associated with folding is recorded by distributed strain and discrete secondary structures. These features are of fundamental importance to understanding mechanisms and sequence of fold evolution and are of practical importance as records and hosts for fluid migration in and around folds. Incomplete data from natural examples limits the ability to evaluate geometric and physics-based models of folding. Recent advances in digital imaging and analysis now make it possible to produce quantitative three-dimensional descriptions of noncylindrical folds and evaluate the relationships of these forms to the distribution and evolution of fold-related strain. This project has the following objectives: 1) to produce a high-resolution digital surface model of an iconic fold, the Whaleback Anticline in Bear Valley, east-central Pennsylvania; 2) to document the spatial variability of strain around the fold with new observations of grain-scale strain, anisotropy of magnetic susceptibility, and detailed mapping of mesoscale structures in the folded layer; 3) to test the hypothesis that surface curvature controls the spatial variation and style of observed strain around a fold; 4) to evaluate stratigraphic and rheological influences on fold strain, through finite element analysis; 5) to demonstrate the utility of structure-from-motion photogrammetry as a tool for structural geology research and 6) to produce educational resources that will preserve and expand access to a world-class field locality and engage the local community.

褶皱岩层是最基本、最有指导意义和最具魅力的地质构造之一。研究褶皱是为了调查造山运动，了解岩石的工程特性，预测水或碳氢化合物的地下运动，并深入了解褶皱本身的基本过程。 这些应用依赖于对褶皱内岩石变形的准确解释。 各种概念和数学模型预测褶皱相关的变形。 为了评估这种预测模型的能力，需要来自自然实例的数据。 这可能是具有挑战性的，因为地球表面的大多数地质褶皱只是部分暴露，褶皱的主要部分要么埋在地下，要么被侵蚀掉。 宾夕法尼亚州中东部熊谷的鲸背背斜是一个独特的地方，那里有一个完整的大规模褶皱暴露出来;上个世纪早期的露天采煤以精美的细节揭示了它。 这种出色的曝光允许观察折叠表面的完整三维形式，并提供了跨折叠变形的非常详细的记录。 该项目将使用先进的数字成像技术和传统的地质实地考察，以产生一个全面的数据集，以测试有关折叠的假设。 除了该项目的科学目标外，该研究还有助于实现科学，技术，工程和数学（STEM）教育领域的社会相关成果，包括通过研究生和本科生培训发展多元化，具有全球竞争力的STEM劳动力;三所大学的研究基础设施的发展;扩大代表性不足的群体对科学的参与;提高公众的科学素养和公众对科学和技术的参与。鲸背背斜是美国东部数十所大学地质系的重要教育实地考察地点，也是当地社区使用良好的娱乐场所。作为这个拟议项目的一部分，我们将保护，扩大和策划从鲸背的地质观测，供研究人员，教育工作者和社区使用。变形与折叠记录的分布应变和离散的二级结构。 这些特征对认识褶皱的演化机制和演化序列具有重要意义，同时也是褶皱及其周围流体运移的记录和宿主。 来自自然实例的不完整数据限制了评估基于几何和物理的折叠模型的能力。 数字成像和分析的最新进展，现在有可能产生定量的三维描述的非圆柱形褶皱，并评估这些形式的分布和演变的褶皱相关的应变的关系。该项目有以下目标：1）制作一个标志性褶皱（宾夕法尼亚州中东部熊谷的鲸背背斜）的高分辨率数字表面模型; 2）记录褶皱周围应变的空间变化，包括对颗粒尺度应变、磁化率各向异性的新观测，以及褶皱层中尺度结构的详细测绘;（3）验证地表曲率控制褶皱周围应变空间变化和样式的假设：（4）通过有限元分析评价地层和流变对褶皱应变的影响; 5）展示运动恢复结构摄影测量作为结构地质学研究工具的实用性; 6）制作教育资源，以保护和扩大进入世界级实地的机会，并参与当地社区。