Collaborative Research: Erosion History and Sediment Provenance of East Antarctica from Multi-method Detrital Geo- and Thermochronology

该奖项是根据2009年《美国复苏和再投资法案》(公法111-5)提供资金的。东南极基岩年代学的大部分目录，以及其侵蚀历史的记录，都保存在其边缘的新生代沉积物中。该项目旨在利用这些沉积物，通过测量单个碎屑晶体和碎屑碎屑中多个晶体的多个地质和热年龄(锆石和磷灰石的U/Pb、裂变径迹和(U-Th)/He年龄，以及角闪石、云母和长石的40Ar/39Ar年龄)，来了解它们的冰下物源和盾体的侵蚀历史。单一颗粒和碎屑中的多个测年组合提供了强大的基岩来源指纹，使我们能够通过边缘周围的第四纪直径追踪始新世河流相砂岩的物源。同一颗粒和碎屑中的多个温度计时(冷却)年龄也使我们能够解释这些基岩来源的侵蚀时间和速率。描绘基岩年龄单位的分布、它们在新生代的泥沙运移联系以及它们的侵蚀历史，反过来将使我们能够检验构造模型，这些模型涉及：(1)甘布尔采夫冰下山脉的起源，(2)河流和地形演变，以及(3)冰川生长和侵蚀的历史。

This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5). Much of the inventory of East Antarctic bedrock geochronology, as well as a record of its erosional history, is preserved in Cenozoic sediments around its margin. This project is to use these sediments to understand their sub-ice provenance and the erosional history of the shield by measuring ages of multiple geo- and thermochronometers on single detrital crystals and on multiple crystals in detrital clasts (U/Pb, fission-track, and (U-Th)/He dating of zircon and apatite, and 40Ar/39Ar dating of hornblende, mica, and feldspar). The combination of multi-chronometer ages in single grains and clasts provides a powerful fingerprint of bedrock sources, allowing us to trace provenance in Eocene fluvial sandstones through Quaternary diamicts around the margin. Multiple thermochronometric (cooling) ages in the same grains and clasts also allows us to interpret the timing and rates of erosion from these bedrock sources. Delineating a distribution of bedrock age units, their sediment transport connections, and their erosional histories over the Cenozoic, will in turn allow us to test tectonic models bearing on: (1) the origin of the Gamburtsev Subglacial Mountains, (2) fluvial and topographic evolution, and (3) the history of glacial growth and erosion.