How do Continental Plateaus Grow? Mantle to Surface Dynamics of the Anatolian and Andean Plateaus

大陆高原如何生长？

• 批准号: RGPIN-2015-04695
• 负责人: Schoenbohm, Lindsay
• 金额: $ 1.97万
• 依托单位: University of Toronto
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2017
• 资助国家: 加拿大
• 起止时间: 2017-01-01 至 2018-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=633776
• 关键词: How; do; Continental; Plateaus; Grow

My research group will investigate the formation of continental plateaus – regions where mountain ranges swell to great widths, with relatively flat tops. We focus on two key locations: (1) the Central Anatolian Plateau in Turkey; and (2) the southern part of the Central Andean Plateau, the Puna Plateau, in northwest Argentina. We are interested in the processes that shape the plateau from the deepest levels to the surface, including: detachment and formation of tears in the subducting oceanic plate; loss of the lower part of the tectonic plate to delamination or dripping; flow of the weak lower crust; shortening of the crust in an organized or disorganized manner; and the influence of climate and erosion on the redistribution of mass. My team uses a combination of field and GIS (computer) based mapping and dating to measure deformation, subsidence and uplift of the plateau in order to constrain the various influences on plateau growth. Specifically, in Argentina, a PhD student will map the interior of the southern Puna Plateau, three Master’s students will map key basins around the margins of the plateau, and five undergraduates will measure features of mountain ranges on and around the plateau to constrain the history of deformation. In Turkey, a PhD student will map and measure movement rates along the Central Anatolian fault zone and other active faults, and two Master’s students will constrain uplift by measuring the incision of a major river into the plateau.

我的研究小组将研究大陆高原的形成--山脉膨胀到很宽的区域，顶部相对平坦。我们关注两个关键地点：（1）土耳其的安纳托利亚高原中部;（2）阿根廷西北部的安第斯高原中部南部，普纳高原。我们感兴趣的是高原从最深处到表面的形成过程，包括：俯冲洋板块的分离和裂缝的形成;构造板块下部因分层或滴水而丧失;脆弱的下地壳的流动;地壳有组织或无组织地缩短;气候和侵蚀对物质重新分布的影响。我的团队使用野外和基于GIS（计算机）的测绘和测年相结合的方法来测量高原的变形、沉降和隆起，以限制对高原生长的各种影响。具体来说，在阿根廷，一名博士生将绘制南部普纳高原的内部地图，三名硕士生将绘制高原边缘的关键盆地，五名本科生将测量高原上和周围的山脉特征，以限制变形的历史。在土耳其，一名博士生将绘制和测量沿着安纳托利亚中部断层带和其他活动断层的运动速率，两名硕士生将通过测量一条主要河流进入高原的切口来限制隆起。