Paleomagnetism of Neoproterozoic to Lower Paleozoic Rocks on Microcontinents of Central Asia: Implications for the Precambrian Glacial Paradox and Amalgamation of Eurasia

中亚微大陆新元古代至下古生界岩石的古地磁：对前寒武纪冰川悖论和欧亚大陆合并的启示

• 批准号: 0508597
• 负责人: Joseph Meert
• 金额: $ 26.75万
• 依托单位: University of Florida
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2005
• 资助国家: 美国
• 起止时间: 2005-07-15 至 2009-06-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0508597&HistoricalAwards=false
• 关键词: Paleomagnetism; Neoproterozoic; Lower; Paleozoic; Rocks

The microcontinents that make up Eurasia were amalgamated over a protracted period beginning in the Cambrian Period (~520 million years ago). The rocks that lie on these microcontinents contain older (Precambrian-age) igneous and sedimentary rocks that formed, at least in part, during a period of time thought to be characterized by extreme swings in global climate. These episodes of severe climate change are dubbed the "Snowball Earth" epochs. Both the location of these microcontinents prior to their incorporation into Eurasia and the exact age of the glacial events preserved on the microcontinents are poorly known. This work focuses on obtaining paleomagnetic and geochronologic data from various microcontinents now located in Mongolia, Khazakhstan and Kyrgystan. The data collected in this study allow the investigators to better constrain the position of these microcontinents prior to their amalgamation into Eurasia. The data also supply researchers with important paleolatitudinal and geochronologic constraints on the glacial sediments preserved on the microcontinents. Since the Snowball Earth hypothesis posits near global synchroneity of glaciation across the planet, these data provide a critical test of the Snowball Earth hypothesis as well as a test of other competing explanations for this ancient ice age. Lastly, the data obtained in the study impose strong constraints on the general style of tectonic evolution for the Ural-Mongol fold belt that developed as a result of collisions between the microcontinental blocks and the closure of an ancient ocean.Support for the project is provide by the Tectonics Program and by the Russia and Eurasia Group of the Office of International Science and Engineering.

构成欧亚大陆的微大陆在寒武纪（约5.2亿年前）开始的漫长时期内合并。 位于这些微大陆上的岩石包含更古老的（前寒武纪时代）火成岩和沉积岩，这些岩石至少部分形成于被认为具有全球气候极端波动特征的时期。 这些严重的气候变化被称为“雪球地球”时代。 这些微大陆在并入欧亚大陆之前的位置和保存在微大陆上的冰川事件的确切年龄都知之甚少。 这项工作的重点是获得古地磁和地质年代学数据，从各种微大陆现在位于蒙古，哈萨克斯坦和吉尔吉斯斯坦。 这项研究收集的数据使研究人员能够更好地限制这些微大陆在合并成欧亚大陆之前的位置。 这些数据也为研究人员提供了保存在微大陆上的冰川沉积物的重要古纬度和年代学约束。 由于雪球假说假设地球上的冰川作用几乎是全球同步的，因此这些数据提供了对雪球假说的关键检验，以及对这个古老冰河时代的其他竞争性解释的检验。 最后，研究中获得的数据对乌拉尔-蒙古褶皱带的构造演化的一般方式施加了强有力的约束，该褶皱带是由于微大陆块体之间的碰撞和古海洋闭合而形成的。该项目得到了构造计划和国际科学与工程办公室俄罗斯和欧亚集团的支持。