青藏高原安多地区晚三叠世沉积环境与锆英石来源分析:对中特提斯洋演化的影响

IF 2.6 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Shiyao Gao , Zhongjie Xu , Chaoming Xie , Zainaibai Ma , Peizhao Deng , Haoxuan Liu
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引用次数: 0

摘要

中特提斯洋中生代早期演化的某些方面仍不确定,而非晶质锆石出处分析可能有助于制约该地区的发展。本文描述了青藏高原图门格拉地层(南羌塘盆地)和曲哈拉地层(安多弧后盆地)的晚三叠世沉积面、岩相学、地球化学和非晶锆石UPb地质年代。在晚三叠世,南羌塘盆地的特征是邻近蒸发平台的海洋三角洲环境,而安多弧后盆地的特征是由潮汐影响的三角洲环绕的浅海陆架;在这两个盆地中,海洋古环境先加深后变浅。通过分析冈瓦纳北缘各微大陆的非铁质锆石UPb年龄谱特征,并结合之前已发表的数据,我们推断南北羌塘地块在晚三叠世时合并,并与拉萨地块被宽阔的中特提斯洋分隔开来。三叠纪晚期,中特提斯洋开始俯冲,南羌塘地块南缘发育为活跃的大陆边缘。在中特提斯洋俯冲过程中,奎哈拉地层堆积于安多微大陆的弧后盆地,奎哈拉地层第2层最上部的年代不早于早侏罗世。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Late Triassic sedimentary environments and detrital zircon provenance analysis in the Amdo area of the Tibetan Plateau: Implications for the evolution of the Meso-Tethys Ocean
Aspects of the early Mesozoic evolution of the Meso-Tethys Ocean remain uncertain, and detrital zircon provenance analyses may be useful for constraining the development of this region. In this paper, we describe Late Triassic sedimentary facies, petrography, geochemistry, and detrital zircon UPb geochronology for the Tumengela Formation (South Qiangtang Basin) and the Quehala Formation (Amdo back-arc basin) in the Tibetan Plateau. In Late Triassic times, the South Qiangtang Basin was characterized by marine deltaic environments adjacent to an evaporative platform, whereas the Amdo back-arc basin was characterized by a shallow marine shelf fringed by tidally-influenced deltas; in both basins, marine palaeoenvironments first deepened and then shallowed. By analyzing the characteristics of detrital zircon UPb age spectra for each microcontinent on the northern margin of Gondwana, and combining them with previously published data, we infer that the North and South Qiangtang Terranes amalgamated in Late Triassic times, and were separated from the Lhasa Terrane by the wide Meso-Tethys Ocean. During the Late Triassic, the Meso-Tethys Ocean began to be subducted, and the southern edge of the South Qiangtang Terrane developed as an active continental margin. The Quehala Formation accumulated in the back-arc basin of the Amdo microcontinent during subduction of the Meso-Tethys Ocean, and the uppermost part of Member 2 of the Quehala Formation is dated as no older than Early Jurassic.
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来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
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