Termination of the Paleo-Asian Ocean in the Beishan orogen, NW China: Constraints from detrital zircon U-Pb age and Hf isotope analysis of turbidites

GSA Bulletin Pub Date : 2022-11-14 DOI:10.1130/b36455.1
Q. Guo, Sun‐Lin Chung, Hao-Yang Lee, W. Xiao, Quanlin Hou
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Abstract

The termination of the Paleo-Asian Ocean, including duration and architecture, is controversial and has led to different reconstructions of the Central Asian orogenic belt. Deep-marine turbidites are of great significance in constraining the evolution of the oceanic basin. The youngest marine turbidites in the Beishan orogen in the central part of the southern Central Asian orogenic belt are separated by the Liuyuan mélange into two sections, the South turbidites and North turbidites. Detrital zircon grains from South turbidites yielded a maximum depositional age of 255 Ma. Those from North turbidites yielded a maximum depositional age of 254 Ma. Most of the Precambrian zircons of South turbidites have concentrated εHf(t) values (−6 to −2.6), whereas those of North turbidites range from −12.6 to +10.4, indicating different provenances. The North turbidites also have more positive whole-rock εNd(t) values (−0.5 to +1.1) than the South turbidites (−4.2 to −2.4), suggesting more juvenile or less evolved crustal components in the source. Detailed comparison of the detrital zircon ages and Hf-Nd isotopic characteristics with igneous and metamorphic rocks in the south Beishan area distinguishes two sources. These findings constrain the Liuyuan suture as the latest suture in the Beishan region, occurring no earlier than 254 Ma. The youngest peak age of detrital zircons of the youngest marine sedimentary rocks in the southern Central Asian orogenic belt becomes younger eastward from 288 Ma to 247 Ma, characterizing the closure duration of the Paleo-Asian Ocean from west to east in ∼40 m.y. This study finds that the youngest turbidites in the Beishan orogen not only record sedimentary processes in response to the final episode of orogenic evolution in the southern Central Asian orogenic belt, but they also constrain how and when an archipelago-type accretionary orogen terminated.
北山造山带古亚洲洋的终结:碎屑锆石U-Pb年龄和浊积岩Hf同位素分析的约束
古亚洲洋的终结,包括持续时间和结构,是有争议的,并导致了中亚造山带的不同重建。深海浊积岩对制约洋盆演化具有重要意义。南中亚造山带中部北山造山带最年轻的海相浊积岩被柳源沟分隔为南浊积岩和北浊积岩两段。南浊积岩碎屑锆石颗粒的最大沉积年龄为255 Ma。北浊积岩的最大沉积年龄为254 Ma。南浊积岩大部分前寒武纪锆石εHf(t)值集中在−6 ~−2.6之间,而北浊积岩的εHf(t)值集中在−12.6 ~ +10.4之间,说明其物源不同。北浊积岩的全岩εNd(t)值(- 0.5 ~ +1.1)高于南浊积岩(- 4.2 ~ - 2.4),说明烃源岩中地壳成分多为幼代或演化程度较低。通过对北山南部火成岩和变质岩碎屑锆石年龄和Hf-Nd同位素特征的详细对比,可以区分出两种来源。这些发现约束了柳源缝合线是北山地区最晚的缝合线,发生时间不早于254 Ma。南中亚造山带最年轻海相沉积岩碎屑锆石的最年轻峰值年龄在288 Ma ~ 247 Ma之间向东变年轻,表征了古亚洲洋自西向东的闭合时间为~ 40 Ma。研究发现,北山造山带最年轻浊积岩不仅记录了南中亚造山带造山演化最后阶段的沉积过程;但它们也限制了群岛型增生造山带如何以及何时终止。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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