Collaborative Research: Intracontinental Deformation and Surface Uplift: Geodynamic Evolution of the Hangay Dome, Mongolia, Central Asia

大陆上常见的大而高海拔且低起伏的表面。这种隆起通过影响排水网络和沉积物供应对地质记录产生重大影响，通过改变大气环流对气候产生重大影响，对生物地理学和生物群产生重大影响。地球动力学研究表明，这种隆起相当于地幔动力学的一个明显特征。因此，它们提供了一种方法来区分关于大陆岩石圈和更深地幔如何通过导致大陆内部隆起和质量转移的过程相互作用的假设。蒙古中部的杭盖圆顶提供了一个优秀且方便的实验室来研究这些过程，并确定地幔上升、镁铁质底板、岩石圈沉没或羽流活动在其隆升过程中发挥重要作用的程度。这个为期五年的项目计划利用 HangayDome 作为这样一个实验室，协调对岩石圈和岩石圈下地幔的结构和状态以及地表隆起和地貌演化历史的研究。该项目将涉及使用宽带地震学、玄武岩和捕虏体岩石学和地球化学、40Ar/39古年代学、稳定同位素和泡状玄武岩古温度测定、地貌学和10Be地质年代学、不同鱼类种群的分子遗传学以及U-Th/He和4He/3He热年代学进行的观测和测量。 杭爱圆顶广泛暴露的玄武岩熔岩在过去 30 Ma 的大范围海拔范围内喷发，这将是整合所有这些数据的关键。 玄武岩的测年将使有关玄武岩成因和杭爱圆顶地幔性质的岩石学数据与使用熔岩作为记录地貌演化和地表隆起历史的时间标记的研究联系起来。

Large relatively high-elevation surfaces with low relief are common onthe continents. Such uplifts have a significant impact on the geological record by influencing drainage networks and sediment supply, on climate by modifyingatmospheric circulation, and on biogeography and the biota. Work in geodynamics hasshown that such uplifts amount to a telling signature of mantle dynamics. Thus, theyprovide a means to discriminate among hypotheses about how the continental lithosphereand the deeper mantle interact through processes that result in uplift and mass transfer incontinental interiors. The Hangay Dome in central Mongolia provides an excellent andaccessible laboratory to investigate these processes and determine the degree to whichmantle upwelling, mafic underplating, lithospheric foundering or plume activity havebeen important agents in its uplift. This five-year project proposes to use the HangayDome as such a laboratory to coordinate studies of both the structure and state of thelithosphere and the sublithospheric mantle as well as the history of surface uplift andlandscape evolution. The project will involve observations and measurements made usingbroadband seismology, basalt and xenolith petrology and geochemistry, 40Ar/39Argeochronology, stable-isotope and vesicular-basalt paleoaltimetry, geomorphology and10Be geochronology, molecular genetics of divergent fish populations, and U-Th/He and4He/3He thermochronology. The Hangay Dome?s widespread exposures of basaltic lavas,which were erupted over the past 30 Ma across a broad range of elevations, will be key tothe integration of all these data. Dating of the basalts will enable linkage of petrologic databearing on basalt genesis and the nature of the Hangay-Dome mantle with studies thatuse the lavas as time markers for documenting landscape evolution and the history ofsurface uplift.