Geoscience Frontiers | |
Switching from advancing to retreating subduction in the Neoproterozoic Tarim Craton, NW China: Implications for Rodinia breakup | |
Wei Liu1  Yang Xiao2  Shuai Yang3  Xin Chen4  Zecheng Wang5  R. Damian Nance6  Guanghui Wu6  | |
[1] Corresponding author. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China.;Development, Beijing 100083, China;Southwest Petroleum University, Division of Key Laboratory of Carbonate Reservoirs, CNPC, Chengdu 610500, China;Department of Geological Sciences, 316 Clippinger Laboratories, Ohio University, Athens, OH 45701, USA;;PetroChina Research Institute of Petroleum Exploration &School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China; | |
关键词: Supercontinent breakup; Top-down tectonics; Rodinia; Subduction; U–Pb–Hf isotopes; | |
DOI : | |
来源: DOAJ |
【 摘 要 】
Geodynamic drivers for the supercontinent cycle are generally attributed to either top-down (subduction-related) or bottom-up (mantle-related) processes. Compiled geochemical data and U–Pb ages and Hf isotopic signatures for magmatic and detrital zircons from the Tarim Craton reveal a distinct change in subduction style during the Neoproterozoic. The subduction cycle is recorded in increasing and decreasing intensity of subduction-related magmatic rocks and time-equivalent sedimentary successions, and converse trends of εHf(t) values and corresponding changes in crustal incubation time. These trends are consistent with a switch from advancing to retreating subduction. The switch likely occurred at ca. 760 Ma when zircon εHf(t) values increase and crustal incubation times decrease following a transitional shift between 800 Ma and 760 Ma. A switch at this time is consistent with Rodinia breakup and may have resulted in the late Neoproterozoic Tarim rift basin. The long-lived (ca. 500 Ma) subduction recorded in the Tarim Craton suggests the predominance of a top-down process for Rodinia breakup on this part of its margin.
【 授权许可】
Unknown