CAUGHT: Central Andean Uplift and the Geodynamics of High Topography

发现：安第斯中部隆起和高地形的地球动力学

• 批准号: 0908858
• 负责人: Carmala Garzione
• 金额: $ 29.27万
• 依托单位: University of Rochester
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2009
• 资助国家: 美国
• 起止时间: 2009-07-01 至 2015-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0908858&HistoricalAwards=false
• 关键词: CAUGHT; Central; Andean; Uplift; Geodynamics

This is an ambitious project that has the potential to fill in important gaps in the overall picture of orogenesis in the central Andes, and of convergent-margin tectonism in general. The project is constructed around a well defined basic-science question, did the Andes rise in a rapid pulse, or did they rise gradually? Producing elevations and crustal thicknesses of the magnitude found in this study area remains a key problem in continental tectonics.This question provides a foundation from which the PIs develop a variety of linked projects, including: 3-D structural analysis of fold-thrust belt shortening in the Andes, testing of new methods of paleo-elevation analysis, use of seismic studies to characterize the roots of the range (both in the deep crust and in the underlying mantle), creative use of petrologic and isotopic data to constrain thickened crust at times in the past. The project has the potential to address 3-D mass balance issues during orogeny, as well as the impact of a rising mountain belt on continent-scale weather systems. Of note, to put the analysis of orographic weather studies in context, the PIs will also undertake a broader paleo-climate study. All of the questions to be studied are current and important, and are of interest across traditional disciplinary boundaries and, the research strategy as outlined has a high potential to answer the questions that it poses.

这是一个雄心勃勃的项目，有可能填补中央安第斯山脉造型的整体形象以及总体上收敛碎片构造的重要空白。该项目是围绕一个明确定义的基本科学问题构建的，安第斯山脉迅速脉动上升，还是逐渐上升？ Producing elevations and crustal thicknesses of the magnitude found in this study area remains a key problem in continental tectonics.This question provides a foundation from which the PIs develop a variety of linked projects, including: 3-D structural analysis of fold-thrust belt shortening in the Andes, testing of new methods of paleo-elevation analysis, use of seismic studies to characterize the roots of the range (both in the deep crust and in the underlying地幔），对质和同位素数据的创造性使用有时会限制外壳增厚。该项目有可能在造山基因期间解决3D质量平衡问题，以及山带对大陆尺度天气系统的影响。值得注意的是，为了对地形天气研究进行分析，PI还将进行更广泛的古气候研究。 所有要研究的问题都是当前和重要的，并且在传统的纪律界限中引起了人们的关注，并且所概述的研究策略具有很高的潜力来回答其提出的问题。