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DOI | 10.1126/science.abf1876 |
Orogenic quiescence in Earth's middle age | |
Tang M.; Chu X.; Hao J.; Shen B. | |
发表日期 | 2021 |
ISSN | 0036-8075 |
起始页码 | 728 |
结束页码 | 731 |
卷号 | 371期号:6530 |
英文摘要 | Mountain belts modulate denudation flux and hydrologic processes and are thus fundamental to nutrient cycling on Earth's surface. We used europium anomalies in detrital zircons to track mountain-building processes over Earth's history. We show that the average thickness of active continental crust varied on billion-year time scales, with the thickest crust formed in the Archean and Phanerozoic. By contrast, the Proterozoic witnessed continuously decreasing crustal thickness, leaving the continents devoid of high mountains until the end of the eon. We link this gradually diminished orogenesis to the long-lived Nuna-Rodinia supercontinent, which altered the mantle thermal structure and weakened the continental lithosphere. This prolonged orogenic quiescence may have resulted in a persistent famine in the oceans and stalled life's evolution in Earth's middle age. Copyright © 2021 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works |
英文关键词 | zirconium; Archean; continental crust; continental lithosphere; crustal thickness; orogeny; Phanerozoic; supercontinent; thermal structure; Archean; Article; astronomy; compression; crustal thickness; mantle thermal structure; Middle Ages; orogenic quiescence; Phanerozoic; sea; tectonic compression; thermal analysis; thickness; trend study; water cycle; weathering |
语种 | 英语 |
来源期刊 | Science |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/245704 |
作者单位 | Key Laboratory of Orogenic Belt and Crustal Evolution, MOE, Beijing, 100871, China; School of Earth and Space Science, Peking University, Beijing, 100871, China; Department of Earth Sciences, University of Toronto, Toronto, ON M5S 3B1, Canada; Department of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ 08901, United States; CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China |
推荐引用方式 GB/T 7714 | Tang M.,Chu X.,Hao J.,et al. Orogenic quiescence in Earth's middle age[J],2021,371(6530). |
APA | Tang M.,Chu X.,Hao J.,&Shen B..(2021).Orogenic quiescence in Earth's middle age.Science,371(6530). |
MLA | Tang M.,et al."Orogenic quiescence in Earth's middle age".Science 371.6530(2021). |
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