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DOI | 10.1130/B35378.1 |
Extreme thermal metamorphism associated with Gondwana assembly: Evidence from sapphirine-bearing granulites of Rajapalayam, southern India | |
Li S.S.; Palin R.M.; Santosh M.; Shaji E.; Tsunogae T. | |
发表日期 | 2020 |
ISSN | 167606 |
起始页码 | 1013 |
结束页码 | 1030 |
卷号 | 132期号:2021-05-06 |
英文摘要 | The Madurai block is the largest composite crustal block in the Southern Granulite terrane of India, where granulite-facies rocks metamorphosed at ultrahigh-temperature (UHT) conditions occur in several localities. Here, we investigated UHT rocks from Rajapalayam, in the southern domain of the Southern Granulite terrane, using integrated thermobarometry and in situ monazite geochronology to precisely constrain the nature and timing of this extreme metamorphism and its implications for regional tectonics. Conventional thermobarometry and petrological phase equilibrium modeling reveal prograde pressure-temperature (P-T) conditions at 0.75-1.2 GPa and <900 °C, followed by peak/postpeak UHT metamorphism at 0.72-0.82 GPa and 1025-1050 °C, and retrograde reequilibration at 0.72-0.80 GPa and 875-895 °C. The granulites thus record a clockwise P-T path defining geothermal gradients of 1200-1500 °C/GPa at peak metamorphism, indicating the presence of an extreme thermal perturbation in the middle to lower continental crust. In situ monazite dating indicates prograde metamorphism at 607-585 Ma, peak metamorphism at 546-543 Ma, and retrograde cooling and exhumation at 539-483 Ma. As such, the entire tectonothermal cycle was complete within ~120 m.y., although temperatures exceeding 900 °C were likely sustained for at least 30 m.y. Such extreme thermal events preserved in geological terranes worldwide are commonly associated with lithospheric extension, although our data show that prolonged heating can occur during continental convergence instead, supporting inferences made by thermomechanical models. Thus, supercontinent formation may act as a driver for spatially distributed UHT tectonometamorphism, as shown by the episodic records in geological history. The age of peak metamorphism constrained here was synchronous with UHT metamorphism in other localities in the Southern Granulite terrane, Sri Lanka, Madagascar, and Antarctica, indicating their correlation with the final amalgamation of eastern Gondwana at ca. 550 Ma. |
语种 | 英语 |
来源期刊 | Bulletin of the Geological Society of America |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/184797 |
作者单位 | School of Earth Sciences and Resources, China University of Geosciences-Beijing, 29 Xueyuan Road, Beijing, 100083, China; Department of Geology and Geological Engineering, Colorado School of Mines, Golden, Colorado 80401, United States; Centre for Tectonics, Exploration and Research, University of Adelaide, Adelaide, SA 5005, Australia; Yonsei Frontier Laboratory, Yonsei University, Seoul, 03722, South Korea; Department of Geology, University of Kerala, Kariyavattom Campus, Trivandrum, 695 581, India; Graduate School of Life and Environmental Sciences, University of Tsukuba, Ibaraki, 305-8572, Japan; Department of Geology, University of Johannesburg, Auckland Park, 2006, South Africa; School of Earth Sciences and Resources, China University of Geosciences-Beijing, 29 Xueyuan Road, Beijing, 100083, China |
推荐引用方式 GB/T 7714 | Li S.S.,Palin R.M.,Santosh M.,et al. Extreme thermal metamorphism associated with Gondwana assembly: Evidence from sapphirine-bearing granulites of Rajapalayam, southern India[J],2020,132(2021-05-06). |
APA | Li S.S.,Palin R.M.,Santosh M.,Shaji E.,&Tsunogae T..(2020).Extreme thermal metamorphism associated with Gondwana assembly: Evidence from sapphirine-bearing granulites of Rajapalayam, southern India.Bulletin of the Geological Society of America,132(2021-05-06). |
MLA | Li S.S.,et al."Extreme thermal metamorphism associated with Gondwana assembly: Evidence from sapphirine-bearing granulites of Rajapalayam, southern India".Bulletin of the Geological Society of America 132.2021-05-06(2020). |
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