Climate Change Data Portal
DOI | 10.1111/jmg.12735 |
Consistent garnet Lu-Hf and Sm-Nd ages indicate short-lived high-pressure metamorphism and rapid subduction in oceanic subduction belt: An example from the Changning-Menglian orogenic belt, southeastern Tibetan Plateau | |
Zhou, Ying; Cheng, Hao; Peng, Zhi-min; Dragovic, Besim; Fu, Yu-zhen; Du, Kai-Yang | |
发表日期 | 2023 |
ISSN | 0263-4929 |
EISSN | 1525-1314 |
起始页码 | 1031 |
结束页码 | 1047 |
卷号 | 41期号:8 |
英文摘要 | The integration of garnet-based petrologic constraints with multimineral geochronologic data in eclogites and blueschists allows the timing and rate of subduction zone metamorphism to be constrained. We present a combined garnet Lu-Hf/Sm-Nd and zircon/rutile U-Pb geochronology study on three eclogites, a garnet-bearing blueschist, and a micaschist from the Changning-Menglian orogenic belt, a newly discovered ultrahigh-pressure metamorphic belt in southeast Tibet, in order to characterize tectono-metamorphic events and determine the duration of Paleo-Tethys oceanic subduction. Integration of phase equilibrium modelling and conventional thermobarometry for the eclogites defines a clockwise P-T path evolving from blueschist facies conditions at similar to 1.4 GPa and similar to 505-530 degrees C to peak eclogite facies conditions at similar to 2.8 GPa and similar to 630-640 degrees C, followed by isothermal decompression to amphibolite facies at similar to 1.0 GPa and similar to 630-650 degrees C. The Lu-Hf ages of c. 239-236 Ma obtained for the eclogites and the blueschist are indistinguishable from the rutile U-Pb age of c. 239 Ma obtained for the eclogites and, combined with the observation of well-preserved Rayleigh-fractionation-style Mn and Lu zoning profiles in garnet, reflect the timing of early prograde garnet growth. The Sm-Nd ages of c. 242-236 Ma reflect a later period of garnet growth, evidenced by flat and/or M-shaped Sm zoning profiles. Each of the Sm-Nd ages overlaps, within uncertainty, with its corresponding Lu-Hf age (i.e., from the same garnet fraction). The consistency of the Lu-Hf and Sm-Nd ages indicates a short overall duration of garnet growth from blueschist to eclogite facies metamorphism, reflecting rapid subduction of the oceanic slab. The magmatic zircon U-Pb dates of c. 247 Ma constrain the protolith age of these metabasaltic rocks. The close protolith and the high-pressure metamorphic ages, together with the consistent garnet Lu-Hf and Sm-Nd ages and the overlapping youngest and oldest metamorphic ages of the oceanic-type and continental-type eclogites, respectively, suggest a fast tectonic transition from divergence to convergence highlighted by rapid oceanic subduction, continuous transition from oceanic to continental subduction, and a rapid cooling of the subduction interface. |
关键词 | eclogiteLu-HfSm-NdsubductionTibet |
英文关键词 | ARC/BACK-ARC ASSEMBLAGES; PALEO-TETHYS OROGEN; QIANGTANG TERRANE; TECTONIC CYCLE; SUTURE ZONE; PB; ZIRCON; ECLOGITES; GEOCHEMISTRY; BEARING |
WOS研究方向 | Geology |
WOS记录号 | WOS:001003367200001 |
来源期刊 | JOURNAL OF METAMORPHIC GEOLOGY |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/283420 |
作者单位 | Tongji University; China Geological Survey; University of South Carolina System; University of South Carolina Columbia; Chengdu University of Technology |
推荐引用方式 GB/T 7714 | Zhou, Ying,Cheng, Hao,Peng, Zhi-min,et al. Consistent garnet Lu-Hf and Sm-Nd ages indicate short-lived high-pressure metamorphism and rapid subduction in oceanic subduction belt: An example from the Changning-Menglian orogenic belt, southeastern Tibetan Plateau[J],2023,41(8). |
APA | Zhou, Ying,Cheng, Hao,Peng, Zhi-min,Dragovic, Besim,Fu, Yu-zhen,&Du, Kai-Yang.(2023).Consistent garnet Lu-Hf and Sm-Nd ages indicate short-lived high-pressure metamorphism and rapid subduction in oceanic subduction belt: An example from the Changning-Menglian orogenic belt, southeastern Tibetan Plateau.JOURNAL OF METAMORPHIC GEOLOGY,41(8). |
MLA | Zhou, Ying,et al."Consistent garnet Lu-Hf and Sm-Nd ages indicate short-lived high-pressure metamorphism and rapid subduction in oceanic subduction belt: An example from the Changning-Menglian orogenic belt, southeastern Tibetan Plateau".JOURNAL OF METAMORPHIC GEOLOGY 41.8(2023). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。