南秦岭北缘淅川地区泥盆纪地层的物源及构造背景

徐大良; 彭练红; 刘浩; 邓新; 魏运许; 张维峰

doi:10.3799/dqkx.2018.591

南秦岭北缘淅川地区泥盆纪地层的物源及构造背景

doi: 10.3799/dqkx.2018.591

中国地质调查局武汉地质调查中心, 湖北武汉 430205

基金项目:

中国地质调查局项目 12120113067900

中国地质调查局项目 121201009000150013

详细信息

作者简介:
徐大良(1983-), 男, 助理研究员, 主要从事基础地质调查与研究工作

中图分类号: P547
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出版历程
- 收稿日期: 2017-10-31
- 刊出日期: 2018-07-15

Provenance and Tectonic Settings of Devonian Sedimentary Strata in Xichuan Area, Northern Margin of South Qinling Block

Wuhan Center of China Geological Survey, Wuhan 430205, China

摘要

摘要: 造山带内广泛发育的泥盆纪地层是揭示秦岭造山带古生代中期洋陆演化、地块构造属性和大地构造背景的良好载体.对南秦岭内部淅川地区泥盆系砂岩进行了岩石地球化学和锆石U-Pb定年，结果显示泥盆系碎屑岩具有中等的成分成熟度及一定程度的沉积再旋回特征，源区物质成分以上地壳长英质岩石为主；碎屑锆石的年龄区间主要集中在新元古代晚期-古生代（0.40~0.63 Ga）、新元古代（0.7~0.9 Ga）和中元古代（1.0~1.6 Ga）三个区间，并存在少量古元古代和中-晚太古代年龄.综合分析，淅川地区泥盆系主要形成于被动大陆边缘环境，其物源可能主要为南秦岭自身隆升的基底和构造高地，并未接受来自于北秦岭的物质，沿商丹洋的俯冲增生事件可能未影响到南秦岭内部.
- 南秦岭 /
- 碎屑锆石年代学 /
- 泥盆系 /
- 物源分析 /
- 大地构造属性 /
- 地球化学
Abstract: The Devonian sedimentary strata, widely developed in the Qinling orogenic belt, are good vehicles to reveal the ocean-continent transition, tectonic attributes and tectonic settings of the Qinling orogenic belt in the Middle Paleozoic. This study presents new geochemical and zircon U-Pb isotopic data for the Devonian sedimentary rocks in Xichuan area. Geochemical data show that the Devonian clastic rocks are characterized by moderate compositional maturity, and a higher portion of sediment recycling, and are likely to have been derived predominantly from felsic igneous rocks within upper-continental-crust. The detrital zircon ages are mainly concentrated in Late Neoproterozoic-Paleozoic (0.40-0.63 Ga), Neoproterozoic (0.7-0.9 Ga) and Mesoproterozoic (1.0-1.6 Ga), with a small amount of ages in Paleoproterozoic and Middle-Late Archean. Comprehensive analysis suggests that the Devonian basin in Xichuan area has beea formed in passive continental margin, and its provenance may be mainly the uplift basement and tectonic highland of the South Qinling, not from the North Qinling. The subduction accretion event along the Shangdan Ocean probably did not affect the interior of South Qinling.
- South Qingling /
- detrital zircon geochronology /
- Devonian /
- provenance analysis /
- tectonic affinity /
- geochemistry

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图 1 研究区地质简图

F₁.洛南-栾川断裂带；F₂.商南-丹凤断裂带；F₃.山阳-凤镇断裂带；F₄.安康-竹山断裂带；F₅.襄樊-广济断裂带

Fig. 1. Geological sketch of the study area

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图 2 淅川地区泥盆纪地层特征

Fig. 2. Stratigraphic column of the Devonian strata in Xichuan area

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图 3 淅川盆地泥盆纪地层野外和镜下特征

a.泥盆系白山沟组与志留系张湾组平行不整合接触；b.王冠沟组珊瑚化石；c.葫芦山组砂岩中发育交错层理；d.白山沟组紫红色砂岩中发育不对称波痕(样品D151)；e.王冠沟组岩屑砂岩(样品D152)；f.白山沟组紫红色粉砂岩(样品D155)；g~h.砂岩镜下特征(正交偏光)；i.砂岩镜下特征(单偏光).Qm.石英；P.长石；Ms.云母；Lc.碳酸盐岩岩屑；Lf.化石碎屑

Fig. 3. Field photographs and micro-photos for the Devonian succession in the Xichuan basin

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图 4 淅川地区泥盆系砂岩中碎屑锆石的阴极发光图像

Fig. 4. Cathodoluminescence (CL) images of detrital zircons from Devonian rocks in Xichuan area

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图 5 淅川地区泥盆系样品碎屑锆石U-Pb年龄谐和图和频谱直方图

Fig. 5. Concordia and probability density diagrams for the detrital zircons of the Devonian samples in Xichuan area

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图 6 淅川地区泥盆纪碎屑岩稀土元素球粒陨石标准化配分模式图

球粒陨石标准值据Sun and McDonouch(1989)；代表性构造环境碎屑沉积岩平均值据Bhatia and Crook(1986)

Fig. 6. Chondrite-normalized REE patterns of Devonian sandstones in Xichuan area

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图 7 淅川地区泥盆纪碎屑岩源区物质组成图解

a.F₁-F₂主量元素判别函数图解，据Roser and Korsch(1988)；b.Zr/Sc-Th/Sc判别图解，据Bhatia and Crook(1986)；c.La/Sc-Co/Th判别图解，据Bhatia and Crook(1986).刘岭群数据来自Yan et al.(2012)

Fig. 7. The characteristics of source composition discrimination diagrams for clastic rocks of Denvoian from Xichuan area

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图 8 碎屑锆石年龄频谱对比

刘岭群数据来自Dong et al.(2013)、Liao et al.(2017)；武关群数据来自Yan et al.(2016)

Fig. 8. Relative probability diagrams of U-Pb detrital zircon age distributions

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图 9 淅川盆地泥盆纪砂岩构造环境判别图

a.(TFe₂O₃+MgO)-TiO₂图解，据Bahtia(1983)；b.构造环境判别函数图解，据Bahtia(1983)；c.La/Sc-Ti/Zr图解，据Bhatia and Crook(1986)；d.La-Th-Sc和Th-Sc-Zr/10三角图解，据Bhatia and Crook(1986).刘岭群数据来自Yan et al.(2012)

Fig. 9. Tectonic discrimination diagrams for the Devonian sandstones in Xichuan area

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