Collaborative Research: Investigating Mesozoic Deformation in the Pamir: Implications for Crustal Thickening in the Pamir and the Evolution of the Tibetan Orogen

这一建议的目的是了解作为喜马拉雅-西藏造山带西端的帕米尔中南部地区发生的中生代地壳缩短的时间和强度。喜马拉雅-青藏造山带是印度板块和欧亚板块汇聚形成的陆-陆碰撞造山带的典型代表。常规的地质解释表明，大部分隆升发生在新生代。相反，主要研究人员假设，该地区岩石记录的大部分地壳缩短和增厚发生在晚侏罗世至白垩纪中期。为了验证这一假设，PIS将进行一项多学科调查，其中将涉及地质和构造制图、地层分析、地质年代学和热年代学测年。该项目的研究成果将为理解喜马拉雅-藏期造山带帕米尔地区的构造演化提供新的思路。除了研究的科学目标外，该项目还有助于培养研究生和本科生从事地球科学的前沿研究，地球科学是STEM的一个重要学科。该项目将有助于扩大代表性不足群体对地球科学的参与，这是一项重要的社会成果。该项目将促进美国、意大利和塔吉克斯坦的研究人员之间的国际合作，并将在两所美国大学之间建立重要的机构合作。该项目将包括为杜尚别大学的学生举办的帕米尔高原地质学讲座和讲习班等外联工作，以促进这个发展中国家的地球科学教育和科学素养。这项研究的结果将发表在同行评议的科学文献和专业学会会议上的报告中；同位素和地球化学数据将在基于网络的社区数据库中存档。过去十年来，越来越多的证据表明，青藏高原的大部分地壳缩短和增厚的年龄是白垩纪，早于印度和亚洲之间的新生代碰撞。然而，尚不清楚整个造山带的前新生代缩短和加厚在横向上有多广泛，或在空间上有多大的变化。这项研究将提供青藏造山带西部广大地区地壳缩短的时间和强度的重要信息，并解决青藏造山带前新生代变形沿走向连续性的重要问题。此外，虽然帕米尔地区的新生代地壳在中新世到最近的片麻岩穹隆有记录在案，但早期对上地壳缩短幅度的计算被证明是严重高估的，这引发了关于新生代地壳增厚机制的重要问题(即逆冲作用与纯剪切增厚作用)。这一结果还将为理解帕米尔地区地壳增厚的机制提供新的信息。这项研究的具体目的是检验这样一种假说，即帕米尔中南部的大部分地壳缩短和增厚是中生代的(而不是以前解释的新生代)，代表了西藏记录的晚侏罗世-中白垩世大规模地壳缩短和增厚的沿线延续。该项目将包括：详细的地质填图和构造分析，以评估帕米尔地区的地壳缩短；对该地区各地发现的粗陆源矿床进行地层学分析，以评估其是否与区域缩短构造有关；进行粗陆源矿床的地质年代学(碎屑U-Pb锆石)和热年代学(碎屑白云母40Ar/39Ar测年，以及碎屑AFT/AHE双重测年)分析，以确定沉积年龄，以评估区域缩短的时间；对参与区域缩短的基底地体进行热年代学分析，以评估与折返有关的缩短时间。

The objective of this proposal is to understand the timing and magnitude of Mesozoic crustal shortening that has occurred within the Central and Southern Pamir region as the western end of the Himalayan-Tibetan orogenic belt. The Himalayan-Tibetan orogen is the classic example of a mountain belt that has formed by continent-continent collision due to the convergence of the Indian and Eurasian tectonic plates. Conventional geologic understanding suggest that most of the uplift is occurred during the Cenozoic. In contrast, the principal investigators hypothesize that much of the crustal shortening and thickening recorded by rocks in this area occurred during Late Jurassic to middle Cretaceous time. To test this hypothesis, the PIs will conduct a multidisciplinary investigation that will involve geologic and structural mapping, stratigraphic analysis, geochronologic and and thermochronologic dating. The results of this project will provide new insights in to the understanding of the tectonic evolution of the Pamir region of the Himalayan-Tibetan orogenic belt. In addition to the scientific goals of the research, the project is contributing to the training of graduate and undergraduate students in cutting-edge research in the geosciences, an important STEM discipline. The project will contribute to the broadening of participation of underrepresented groups in the geosciences, which is an important societal outcome. The project will facilitate international collaboration between researchers at U.S., Italy, and Tajikistan, and will build important institutional collaborations between two U.S. universities. The project will include outreach efforts that include lectures and workshops on the Geology of the Pamir for students at the University of Dushanbe in order to promote geoscience education and science literacy in this developing country. The outcomes of the research will be published in peer-reviewed scientific literature and presentations at professional society meetings; isotopic and geochemical data will be archived in web-based community databases.Over the last decade, increased evidence has shown that much of the crustal shortening and thickening in the Tibetan plateau is Cretaceous in age, pre-dating the Cenozoic collision between India and Asia. However, it is still unclear how laterally extensive, or spatially variable, pre-Cenozoic shortening and thickening is across the entire orogen. This study will provide important information on the timing and magnitude of crustal shortening over a broad region of the western portion of the Tibetan orogen and address important questions regarding the along-strike continuity of pre-Cenozoic deformation in the Tibetan orogen. Further, while significant Cenozoic crustal thickening in the Pamir has been documented in Miocene to Recent gneiss domes, early calculations of the magnitude of upper crustal shortening have been shown to be significantly overestimated, raising important questions regarding the mechanism of Cenozoic crustal thickening (i.e. underthrusting vs. pure shear thickening). The results of this will also provide new information in understanding the mechanisms of crustal thickening in the Pamir region. The specific goal of this study involves testing the hypothesis that much of the crustal shortening and thickening in the Central and Southern Pamir is Mesozoic in age (rather than Cenozoic, as previously interpreted) and represents the along-strike continuation of extensive Late Jurassic-middle Cretaceous crustal shortening and thickening documented in Tibet. The project will include detailed geologic mapping and structural analysis to evaluate crustal shortening in the Pamir; stratigraphic analyses of coarse terrigenous deposits found throughout the region to evaluate whether the deposits are syntectonic with regional shortening structures; geochronologic (detrital U-Pb zircon) and thermochronologic (detrital muscovite 40Ar/39Ar dating, and detrital AFT/AHe double dating) analyses of coarse terrigenous deposits to determine the age of deposition in order to evaluate timing of regional shortening; thermochronologic analyses of basement terranes involved in regional shortening to evaluate timing of shortening related exhumation.