Geochemistry of the Guadalupian—Lopingian carbonate rocks from the NE Sichuan Basin, China: implications for paleo-oceanic environment and provenance

IF 1.1 4区 地球科学 Q3 GEOLOGY
Shengyang Yao, Chuanlong Mou, Gang Zhou, Qiyu Wang, Xiuping Wang, Peng Ren, Bowen Zan
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Abstract

As the last part of the Hercynian cycle in the Yangtze region, the Dongwu Movement included the eruption of the Emeishan large igneous province (ELIP) and was an essential event between the Guadalupian and Lopingian, which had significant implications for the paleo-oceanic environment and paleoclimate of the area. To study the changes in the sedimentary environment in the Guadalupian and Lopingian, the Zhenba section was selected, and its trace elements and rare earth elements (REEs) were analyzed. From analysis of the trace elements and REEs in the Guadalupian, the limestone samples had prominent typical shallow-water seawater deposition characteristics and were less affected by terrigenous detritus, which was in an arid oxidation environment; Sr/Cu ranged from 4 to 1381, the Rb/Sr value was low, δCe < 1, Ceanom < −0.1, Er/Nd ranged from 0.1 to 0.27, and Y/Ho ranged from 44 to 72. However, in the Lopingian, the limestone samples were more affected by terrigenous detritus, which was in a humid climate with a weak oxidation‒reduction environment; the Sr/Cu ranged from 1 to 656, the Rb/Sr value was high, δCe ≅ 1, Ceanom ≥ −0.1, Er/Nd < 0.1, and Y/Ho ranged from 26 to 44. The geochemical diagrams of TiO2‒Al2O3, Al2O3‒REE, La‒Th‒Sc, Th‒Co‒Zr/10, Th‒Sc‒Zr/10 and 87Sr/86Sr of a sample indicated that the terrigenous detritus of the sample mainly came from the South Qinling active continental margin, rather than the weathering of Emeishan basalt. Acid bentonite came from the Paleo-Tethys island arc or the island arc formed by the subduction of the South China Plate beneath the North China Plate, rather than the ELIP. This evidence supported the view that the North China Plate potentially collided with the South China Plate in middle to late Wujiaping.

Abstract Image

中国四川盆地东北部瓜达卢佩-隆平带碳酸盐岩的地球化学:对古海洋环境和产地的影响
东吴运动是长江流域海西周期的最后一段,包括峨眉山大火成岩带的喷发,是瓜岛期和洛坪期之间的重要事件,对该地区的古海洋环境和古气候具有重要影响。为了研究瓜达卢佩期和洛坪期沉积环境的变化,我们选择了镇巴剖面,并对其微量元素和稀土元素(REEs)进行了分析。从瓜达鲁派的微量元素和稀土元素分析来看,石灰岩样品具有突出的典型浅水海水沉积特征,受土著碎屑影响较小,处于干旱氧化环境;Sr/Cu在4~1381之间,Rb/Sr值较低,δCe <1,Ceanom <-0.1,Er/Nd在0.但在罗平期,石灰岩样品受土著碎屑的影响较大,气候潮湿,氧化还原环境较弱,Sr/Cu 值在 1 至 656 之间,Rb/Sr 值较高,δCe ≅ 1,Ceanom ≥ -0.1,Er/Nd < 0.1,Y/Ho 在 26 至 44 之间。样品的 TiO2-Al2O3、Al2O3-RE、La-Th-Sc、Th-Co-Zr/10、Th-Sc-Zr/10 和 87Sr/86Sr 地球化学图表明,样品中的陆相碎屑岩主要来自南秦岭活动大陆边缘,而非峨眉山玄武岩的风化。酸性膨润土来自古特提斯岛弧或华南板块俯冲到华北板块之下形成的岛弧,而不是峨眉山板块。这一证据支持了华北板块可能在吴家坪中晚期与华南板块发生碰撞的观点。
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来源期刊
Carbonates and Evaporites
Carbonates and Evaporites 地学-地质学
CiteScore
2.80
自引率
14.30%
发文量
70
审稿时长
3 months
期刊介绍: Established in 1979, the international journal Carbonates and Evaporites provides a forum for the exchange of concepts, research and applications on all aspects of carbonate and evaporite geology. This includes the origin and stratigraphy of carbonate and evaporite rocks and issues unique to these rock types: weathering phenomena, notably karst; engineering and environmental issues; mining and minerals extraction; and caves and permeability. The journal publishes current information in the form of original peer-reviewed articles, invited papers, and reports from meetings, editorials, and book and software reviews. The target audience includes professional geologists, hydrogeologists, engineers, geochemists, and other researchers, libraries, and educational centers.
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