Detrital Zircon U-Pb Geochronology of the Es2 Sandstones of Lvda 29-1 Structure of the Eastern Bohai Sea, and Its Implication for Provenance
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摘要: 为示踪辽东凹陷LD29-1构造沙二段(Es2)砂岩沉积,对LD29-1-1、LD29-1-1Sa及LD29-1-2等3口井的沙二段砂岩6个岩屑样品进行了碎屑锆石U-Pb定年和锆石阴极发光(CL)图像分析。结果表明:LD29-1-1井样品中白垩纪(K)锆石含量高达41.2%,具有108 Ma峰值年龄,锆石柱状晶形完整,并且棱角明显;而LD29-1-1Sa及LD29-1-2井样品的中元古代(Pt2)锆石含量高达74%~75%,中生代(Mz)锆石含量少,具有~1.5 Ga和~1.8 Ga双峰值特征,锆石晶体明显小于LD29-1-1井沉积物,并且晶形不完整、边缘均被磨圆。因此,认为LD29-1-1井沙二段砂岩为近源沉积,母岩为长兴岛凸起斜坡带中生界碎屑岩,而LD29-1-1Sa及LD29-1-2井沙二段砂体为远源沉积,母岩以辽东半岛西部复州地区广泛分布的中、上元古界沉积岩为主,在搬运至斜坡带时才混入少量中生界碎屑岩。
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关键词:
- 旅大29-1构造 /
- 物源示踪 /
- 碎屑锆石U-Pb年龄 /
- 中元古界 /
- 上元古界
Abstract: To trace the sedimentary source-to-sink systems of the Lvda 29-1 structure in the eastern Bohai Sea, six sandstone cuttings of the second Member of Shahejie Formation (Es2) were collected from LD29-1-1, LD29-1-1Sa and LD29-1-2 for detrital zircon U-Pb dating and cathodoluminescence (CL) image analysis. The results showed that the sandstones of LD29-1-1 contained 41.2% Cretaceous (K) zircons and featured a 108 Ma peak, and the columnar crystals were characterized by sharp edges. The LD29-1-1Sa and LD29-1-2 sandstones contained 74%-75% Mesoproterozoic (Pt2) zircons with peaks at ~1.5 Ga and ~1.8 Ga, and the broken crystals were well rounded. We concluded that the Es2 sandstones of LD29-1-1 were near-source deposited, and the provenance was the Mesozoic sedimentary rocks along the slope of the Changxingdao Uplift; the Es2 sandstones of LD29-1-1Sa and LD29-1-2 were distal from the source area and were dominated by the widespread Mesoproterozoic and Neoproterozoic sedimentary rocks exposed in Fuzhou on the western Liaodong Peninsula, with only a slight influence of Mesozoic sedimentary rocks from the slope of the Changxingdao Uplift.-
Key words:
- Lvda 29-1 Structure /
- provenance /
- detrital zircon U-Pb ages /
- Mesoproterozoic /
- Neoproterozoic
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