Collaborative Research: Determining the 3D Kinematic Evolution of the Wyoming Laramide, Implications for Processes of Foreland Deformation

合作研究：确定怀俄明州拉拉酰胺的 3D 运动学演化，对前陆变形过程的影响

• 批准号: 0948692
• 负责人: W.A. Yonkee
• 金额: $ 10.05万
• 依托单位: Weber State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2010
• 资助国家: 美国
• 起止时间: 2010-04-15 至 2014-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0948692&HistoricalAwards=false
• 关键词: Collaborative; Research; Determining; 3D; Kinematic

First-order outstanding questions regarding foreland deformation center on geodynamic processes that form diverse orientations of basement arches, mechanisms of basement deformation and its transfer to the sedimentary cover, and relationships to plate margin stresses. This project will integrate structural, anisotropy of magnetic susceptibility (AMS), and paleomagnetic studies of Laramide structures in Wyoming to test various tectonic models of foreland deformation. Testable models include, temporal changes in stress directions (possibly associated with flat-slab subduction), spatial variations in stress and fault orientations (potentially associated with basement anisotropy), and varying components of shear along differently oriented structures. Results of this project will further provide data on structural traps, fracture systems, and fault patterns within the Wyoming foreland, which will improve understanding of hydrocarbon reservoirs and potential sites for carbon dioxide sequestration. Finally, this collaborative investigation will be merged with ongoing paleomagnetic and structural studies of other orogens to compare processes of mountain building in different settings, and will generate large data sets for statistical comparisons of various strain and paleostress methods used in kinematic and mechanical analysis.The focus of this investigation will be on key structures that display a range of trends and deformation styles in the Wyoming foreland, and on two stratigraphic levels (Triassic redbeds and Jurassic limestone) that are well exposed, carry primary remanent magnetizations, and contain multiple strain markers. Characteristics of minor fault systems will be measured and analyzed to estimate paleostress patterns, strain orientations will be estimated from AMS fabrics and calcite twin analysis, and oriented cores will be drilled for paleomagnetic analysis to quantify timing and magnitudes of vertical-axis rotations. Characteristics of fracture patterns will be quantified for selected well-exposed surfaces to test relationships to fold and fault mechanics. By integrating multiple data sets, limitations of each set will be reduced. Critically, paleomagnetic data will be combined with deformation fabrics (minor faults, AMS, calcite twins, and fractures) and cross sections/3-D restorations to quantify both vertical-axis rotations and spatial-temporal changes in paleostress/strain. This project will provide an expansive data base, building on previous studies, in order to critically test kinematic models and mechanical processes of Laramide foreland deformation.

关于前陆变形的一阶突出问题集中在形成基底拱的不同方向的地球动力学过程、基底变形的机制及其向沉积盖层的转移以及与板块边缘应力的关系。该项目将整合怀俄明州Laramide构造的构造、磁化率各向异性（AMS）和古地磁研究，以测试前陆变形的各种构造模型。 可测试的模型包括应力方向的时间变化（可能与平板俯冲有关）、应力和断层方向的空间变化（可能与基底各向异性有关）以及沿沿着不同方向结构的剪切分量的变化。该项目的结果将进一步提供怀俄明州前陆内的构造圈闭、断裂系统和断层模式的数据，这将提高对油气藏和二氧化碳封存潜在地点的理解。最后，这项合作调查将与正在进行的其他造山带的古地磁和构造研究相结合，以比较不同环境下的造山过程，并将产生大量数据集，用于运动学和力学分析中使用的各种应变和古应力方法的统计比较。这项调查的重点将是怀俄明州前陆显示一系列趋势和变形样式的关键结构，和两个地层水平（三叠纪红层和侏罗纪灰岩），它们暴露良好，带有原始的反射磁化，并包含多个应变标志。将测量和分析小断层系统的特征，以估计古应力模式，将从AMS组构和方解石双晶分析中估计应变方向，并将钻取定向岩心进行古地磁分析，以量化垂直轴旋转的时间和幅度。将对选定的暴露良好的表面的断裂模式的特征进行量化，以测试与褶皱和断层力学的关系。通过整合多个数据集，将减少每个数据集的局限性。重要的是，古地磁数据将与变形组构（小断层，AMS，方解石双晶和裂缝）和横截面/3-D解释相结合，以量化古应力/应变的垂直轴旋转和时空变化。该项目将提供一个广阔的数据库，建立在以前的研究，以严格测试运动学模型和力学过程的Laramide前陆变形。