Collaborative Research: Clockwise block rotation in the Pacific Northwest and sinistral movement on the Lewis & Clark zone

合作研究：太平洋西北地区的顺时针旋转和刘易斯河的左旋运动

• 批准号: 2317912
• 负责人: Bernard Housen
• 金额: $ 40.15万
• 依托单位: Western Washington University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-08-01 至 2026-07-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2317912&HistoricalAwards=false
• 关键词: Collaborative; Research; Clockwise; block; rotation

GeneralThe western portion of the North American continent was assembled by collision of large blocks of crust over the past 200 million years. These collisions are likely responsible for the formation of mountain belts, significant igneous activity, and production of mineral deposits throughout the western United States. This project will gather data from rocks in Idaho and Montana to test new ideas to explain the timing and origin of the mountain building events in the northern Rocky Mountains and Pacific Northwest. The ideas to be tested include the type of crustal movement, the timing of those crustal movements, and the deformation of rocks associated with it. Predictions resulting from these ideas include the existence of clockwise rotation of large portions of Idaho, Oregon, and Montana. The Lewis & Clark zone of Idaho and Montana - a large-scale strike-slip fault - may have resulted from these clockwise rotations. The work conducted for this project will include collection of samples to measure the direction of the Earth’s magnetic field recorded when the rocks formed, and to analyze minerals in these rocks to determine their age. This data will test predictions for the timing of deformation and of associated igneous activity. The work will be done by a team of faculty at two universities, three graduate students, and several undergraduate students.The proposal is a straightforward paleomagnetic test of whether the Blue Mountains and Adjacent Laurentia – the region of eastern Oregon, southeastern Washington, central Idaho, and possibly southwestern Montana – rotated ~30° clockwise as a coherent block in the Late Cretaceous-Paleogene. A series of paleomagnetic analyses will be conducted on different locations to test whether the clockwise rotation happened and, if so, what is the spatial extent of the crustal block. Paleomagnetic analyses of different ages of rocks will test when the clockwise rotation occurred, to correlate it to motions along the western margin of Laurentia and contractional deformation in the continental interior. The implications are three-fold. First, clockwise rotation could provide independent evidence for dextral terrane translation along the western margin of the Pacific Northwest. Second, the clockwise rotation may explain the activation of the Lewis and Clark line, a major strike-slip system that is oblique to the plate margin. The timing of clockwise rotation should act as a guide to the history of left-lateral vs. right-lateral movement on that structure. Third, the rotation of the Blue Mountains- Adjacent Laurentia block may be spatially and temporally correlated with Laramide-style deformation in its type locality, it could inform questions about foreland deformation. The work will support three graduate students from Western Washington University and the University of Wisconsin-Madison. It will also support undergraduate student research and a capstone experience for undergraduate students at each university.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

北美洲大陆西部是在过去2亿年中由大块地壳碰撞而成的。这些碰撞可能是负责形成山脉带，显着的火成岩活动，并在整个美国西部的矿床生产。该项目将从爱达荷州和蒙大拿州的岩石中收集数据，以测试新的想法，来解释北方落基山脉和太平洋西北部造山事件的时间和起源。 这些观点包括地壳运动的类型、地壳运动的时间以及与之相关的岩石变形，并由此预测了爱达荷州、俄勒冈州和蒙大拿州的大部分地区存在顺时针旋转。 爱达荷州和蒙大拿州的刘易斯克拉克带--一个大规模的走滑断层--可能就是这些顺时针旋转的结果。 为该项目进行的工作将包括收集样本，以测量岩石形成时记录的地球磁场方向，并分析这些岩石中的矿物以确定其年龄。 这些数据将测试对变形时间和相关火成活动时间的预测。 这项工作将由两所大学的一个教师团队、三名研究生和几名本科生完成，该计划是一个简单的古地磁测试，以确定蓝山和邻近的劳伦蒂亚地区--俄勒冈州东部、华盛顿东南部、爱达荷州中部，可能还有蒙大拿州西南部--是否在晚白垩纪-古近纪顺时针旋转了约30°，成为一个连贯的块体。 将在不同地点进行一系列古地磁分析，以测试是否发生了顺时针旋转，如果发生了，地壳块体的空间范围是什么。 对不同年代岩石的古地磁分析将测试顺时针旋转发生的时间，以将其与劳伦大陆西缘沿着的运动和大陆内部的收缩变形相关联。 其影响有三个方面。 首先，顺时针旋转可以提供独立的证据，右西平移沿着太平洋西北缘。 第二，顺时针旋转可以解释刘易斯和克拉克线的激活，一个主要的走滑系统，是斜向板块边缘。 顺时针旋转的时间应该作为该结构上左侧运动与右侧运动的历史的指导。 第三，蓝山-邻近劳伦地块的旋转可能与其模式产地的Laramide式变形在空间和时间上相关，它可以为前陆变形问题提供信息。 这项工作将支持来自西华盛顿大学和威斯康星大学麦迪逊分校的三名研究生。 该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。