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古地理学报 ›› 2026, Vol. 28 ›› Issue (1): 245-263. doi: 10.7605/gdlxb.2025.077

• 岩相古地理学及沉积学 • 上一篇    下一篇

北羌塘坳陷夏里组碎屑岩地球化学特征及其对风化、物源与构造背景的启示*

戚俊1,2(), 王忠伟1,2(), 王剑1,2, 隋博雨1,2, 李磊1,2   

  1. 1 西南石油大学地球科学与技术学院,四川成都 610500
    2 西南石油大学羌塘盆地研究院,四川成都 610500
  • 收稿日期:2024-12-20 修回日期:2025-03-10 出版日期:2026-02-01 发布日期:2026-02-09
  • 通讯作者: 王忠伟,男,1990年生,西南石油大学副教授,主要从事中生代羌塘盆地演化与油气资源评价研究。E-mail: wzwcdg@sina.com
  • 作者简介:

    戚俊,男,2001年生,西南石油大学硕士研究生,主要从事沉积学研究工作。E-mail:

  • 基金资助:
    *国家自然科学基金项目(42241202); 国家自然科学基金项目(42372129); 四川省自然科学基金项目(2024NSFSC0833)

Geochemical characteristics of clastic rocks from the Xiali Formation in North Qiangtang Depression and their implications for weathering,provenance and tectonic setting

QI Jun1,2(), WANG Zhongwei1,2(), WANG Jian1,2, SUI Boyu1,2, LI Lei1,2   

  1. 1 School of Geoscience and Technology,Southwest Petroleum University,Chengdu 610500,China
    2 Qiangtang Institute of Sedimentary Basin,Southwest Petroleum University,Chengdu 610500,China
  • Received:2024-12-20 Revised:2025-03-10 Online:2026-02-01 Published:2026-02-09
  • Contact: WANG Zhongwei,born in 1990,is an associate professor in Southwest Petroleum University. He is engaged in researches on the evolution of the Mesozoic Qiangtang Basin and the evaluation of oil and gas resources. E-mail: wzwcdg@sina.com.
  • About author:

    QI Jun,born in 2001,masteral degree candidate,is mainly engaged in research on sedimentology. E-mail: .

  • Supported by:
    National Natural Science Foundation of China(42241202); National Natural Science Foundation of China(42372129); Natural Science Foundation of Sichuan Province(2024NSFSC0833)

摘要:

北羌塘坳陷中侏罗世夏里组沉积期发生了一次大规模海退,发育大量含膏碎屑岩。本研究以北羌塘坳陷胜利河西剖面和羌科1井夏里组碎屑岩岩石学及元素地球化学资料为基础,分析其物源区化学风化强度、沉积物源属性及大地构造背景,明确其对侏罗纪盆地演化及成盐响应的意义。 结果表明: (1)研究区夏里组碎屑岩化学风化指数(CIA)受颗粒大小与分选性影响较大,且基本不受沉积旋回的影响,故泥页岩样品的CIA值能够较真实地反映物源区的化学风化强度。羌科1井夏里组泥页岩CIA值波动较大(60~77),基本不受钾交代作用影响,表明羌科1井物源区总体上经历了中等—弱的化学风化作用。胜利河西剖面夏里组泥页岩样品的CIA值受钾交代作用影响较大,经钾校正后的泥页岩样品CIA值(CIAcorr)为80~85,表明胜利河西剖面物源区经历了强烈的化学风化作用。(2)依据La/Th vs. HfCo/Th vs. La/ScLa/Yb vs. 􀰐REEA-CN-K等判别图解,结合显著的Eu负异常,推测夏里组物源主要来自长英质岩石。其中, 北羌塘坳陷西部胜利河和中部羌科1井地区夏里组碎屑岩主体形成于碰撞型构造背景,而东部沱沱河地区夏里组主体形成于岛弧构造背景,这一结论与北羌塘坳陷侏罗纪中期的构造体制一致, 即侏罗纪中期北羌塘中、西部为陆内弱挤压前陆盆地,而东部可能为班公湖—怒江新特提斯洋俯冲消减诱发的弧后前陆盆地。(3)侏罗纪早、中期北羌塘地区多期次海侵—海退、相对干旱的古气候条件及局限的古地理背景为夏里组膏盐岩形成奠定了有利条件。

关键词: 化学风化, 物源, 碰撞型背景, 夏里组, 羌塘盆地

Abstract:

A large-scale marine regression occurred during the depositional period of the Middle Jurassic Xiali Formation in the North Qiangtang Depression,accompanied by the widespread deposition of gypsum-bearing clastic sediments. Based on integrated petrological characteristics and elemental geochemical analyses of clastic rocks from the Xiali Formation in the Shenglihexi section and Well QK-1,we systematically analyzed the intensity of chemical weathering,provenance characteristics,and tectonic setting of these sediments,which is critical for understanding the evolutionary history and evaporite response of the Jurassic basin system. The results indicate that the Chemical Index of Alteration(CIA)values of these clastic rocks are significantly influenced by grain size and sediment sorting,but minimally affected by sedimentary recycling;thus,the CIA values of mudstone samples reflect the intensity of chemical weathering in the source region. Mudstones from the Xiali Formation in Well QK-1 exhibit considerable variation in CIA values(60-77),with negligible influence from potassium metasomatism,indicating that the source area underwent generally moderate to weak chemical weathering. In contrast,mudstones from the Shenglihexi section show significant effects of potassium metasomatism;after correction for this influence(CIAcorr),their values range from 80 to 85,suggesting intense chemical weathering in the corresponding source region. Discriminant diagrams based on La/Th vs. Hf,Co/Th vs. La/Sc,La/Yb vs. 􀰐REE,and A-CN-K plots,along with pronounced negative Eu anomalies,collectively indicate a predominantly felsic rock provenance for these clastic deposits. Clastic sediments from the western and central segments of the North Qiangtang Depression were deposited in a continental collision setting,whereas those from the eastern segment were formed in an arc-related tectonic environment. This interpretation aligns well with the established tectonic framework of the North Qiangtang Depression during the Middle Jurassic. During this period,the central and western regions functioned as a weakly magmatic intracontinental foreland basin,while the eastern region likely developed as a back-arc foreland basin,induced by southward subduction of the Bangonghu-Nujiang Tethys Ocean. Multiple transgressive-regressive cycles,combined with a relatively arid palaeoclimate and restricted paleogeographic conditions in the North Qiangtang Depression during the Early to Middle Jurassic,may have created favorable conditions for the formation of extensive gypsum-rich evaporites within the Xiali Formation.

Key words: chemical weathering, provenance, collision setting, Xiali Formation, Qiangtang Basin

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