Surface Elevation History of the Northern North America Cordillera as Constraint for Eocene Tectonic and Climatic Boundary Conditions

北美洲北部科迪勒拉地表高程历史作为始新世构造和气候边界条件的约束

• 批准号: 1450357
• 负责人: C. Page Chamberlain
• 金额: $ 28.38万
• 依托单位: Stanford University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2015
• 资助国家: 美国
• 起止时间: 2015-08-15 至 2022-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1450357&HistoricalAwards=false
• 关键词: Surface; Elevation; History; Northern; North

The development of large-scale regional topography during the development of mountain belts reflects fundamental tectonic processes that operate at deeper levels in the crust and mantle. Using a variety of geological and geochemical methods that act as proxies for paleoelevation, this researcher and colleagues suggested a broad high-standing plateau (4 to 5 km high) developed in the northern Rockies about 50 million years ago and grew southward into central Nevada by about 40 million years ago. Data from Nevada and California support this model, but data limited data are equivocal. This project aims to expand the collection of paleoelevation data to the northern regions (western Washington, Idaho, and Montana) to further test the model. Significant revisions to tectonic models of the building of the North American Cordillera could be required if the data do not support the southward growth idea. The project would advance desired societal outcomes through: 1) full participation of women and underrepresented minorities in STEM; (2) improved STEM education and educator development through teacher education and outreach to K-12 programs; (3) increased public scientific literacy and public engagement with STEM through public outreach; (4) development of a diverse, globally competitive STEM workforce through graduate and undergraduate student training; and (5) increased partnerships between through international collaboration that includes an international research opportunity for a graduate student. The research is supported by the Tectonics Program and NSF's International Science and Engineering program.Understanding the surface elevation history of mountain belts is central in placing critical constraints both on tectonic models and boundary conditions to global climate models. Previous work lead to an uplift model for the North American Cordillera that calls for north to south growth of an Eocene plateau with the northern Rockies reaching hypsometric mean heights of ~4 to 5 km first in British Columbia at ~50 Ma and sweeping southward into central Nevada at ~40 Ma. However, new geologic and geochemical evidence indicates that the surface elevation history north of the Snake River Plain contrasts markedly with its southern counterpart. For Nevada and California there is excellent evidence for a moderately high plateau in the Cretaceous that underwent another phase of surface uplift at ~40 Ma with rivers draining a low-relief highland west of the paleocontinental divide in Nevada and to the east across a high-relief landscape. To the north, however, an earlier phase of surface uplift at ~50 Ma is observed, but little evidence of a broad Eocene highland. If this evidence is correct, it will require substantial modification to surface elevation history models and would suggest other tectonic models for the northern North American Cordillera, such as piece-meal removal of the Farallon slab or the formation of a slab window. This project aims to obtain more data from basins in western Washington, Idaho, and Montana in order to test the nature of the connection between the southern region and regions farther north. The project would employ: (1) sedimentologic studies tied to geochronologic studies for age constraints; 2) stable isotopic studies from multiple proxies including volcanic glasses, calcite from paleosols, and clay minerals as well as clumped isotope temperatures; and 3) vapor transport models.

在造山带发展过程中，大尺度区域地形的发展反映了地壳和地幔更深层次的基本构造过程。利用各种地质和地球化学方法作为古海拔的替代物，这位研究人员和同事提出，大约5000万年前，北方落基山脉形成了一个广阔的高海拔高原（4至5公里高），大约4000万年前，该高原向南生长到内华达州中部。来自内华达州和加州的数据支持该模型，但数据有限的数据是模棱两可的。该项目旨在将古高程数据的收集扩展到北方地区（华盛顿西部、爱达荷州和蒙大拿州），以进一步测试该模型。如果数据不支持向南增长的想法，可能需要对北美科迪勒拉山脉的构造模型进行重大修改。该项目将通过以下方式推进预期的社会成果：（1）妇女和代表性不足的少数民族充分参与STEM;（2）通过教师教育和K-12计划的推广，改善STEM教育和教育工作者的发展;（3）通过公共宣传，提高公众的科学素养和公众对STEM的参与;（4）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;和（5）通过国际合作，包括为研究生提供国际研究机会，增加伙伴关系。这项研究得到了构造计划和NSF国际科学与工程计划的支持。了解山区的地表高程历史是对构造模型和全球气候模型边界条件施加关键约束的核心。以前的工作导致了北美科迪勒拉隆起模型，要求始新世高原由北向南生长，北方落基山脉在~50 Ma时首先在不列颠哥伦比亚省达到~4至5 km的测高平均高度，并在~40 Ma时向南扫入内华达州中部。然而，新的地质和地球化学证据表明，斯内克河平原北部的地表高程历史与南部形成鲜明对比。对于内华达州和加州州，有很好的证据表明，白垩纪有一个中等高度的高原，在~40 Ma时经历了另一个阶段的表面隆起，河流从内华达州古大陆分水岭以西的低地形高地流出，向东穿过高地形地貌。然而，在北部，在~50 Ma的早期阶段的表面隆起的观察，但没有证据表明广泛的始新世高地。如果这一证据是正确的，它将需要大量修改表面高程历史模型，并建议其他构造模型的北方北美科迪勒拉，如片状去除法拉隆板或板窗口的形成。该项目旨在从华盛顿西部、爱达荷州和蒙大拿州的盆地获得更多数据，以测试南部地区与更北部地区之间的联系性质。该项目将利用：（1）沉积学研究与年代学研究相结合，以限制年龄; 2）稳定同位素研究，包括火山玻璃、古土壤中的方解石、粘土矿物以及成团同位素温度; 3）蒸汽传输模型。