Sediment Provenance of Shahejie Formation in Lixian Slope of Raoyang Depression Based on the Detrital Zircon Dating Analysis
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摘要: 为明确饶阳凹陷蠡县斜坡沙河街组沙一段物源组合与沉积体系配置关系，针对饶阳凹陷蠡县斜坡沉积缓坡带多物源供给的特征，结合传统物源研究方法，通过碎屑锆石年龄谱与物源区基岩年龄对比，精细刻画沙河街组沙一段物源体系.依据沙一段古地貌差异及钻井分布特征，将斜坡划分为A、B、C 3个区，对应3个物源体系，研究表明，西北部物源体系母岩为华北北缘及兴-蒙造山带晚古生代（Pz）火成岩，由古大清河水系自西北向斜坡A区供源；西部物源体系母岩为涞源地区中生代（Mz）火成岩、中-新元古界（Pt2+3）侵入岩、中-新太古代（Ar2+3）变质岩，由古唐河水系自西向斜坡B区供源；西南部物源体系母岩为五台地区古元古代（Pt1）滹沱系变质岩、中基性火成岩，由古大沙河水系自西南向斜坡C区供源.且碎屑锆石含量与流域面积成正相关关系.Abstract: The purpose of this study is to clarify the relationship between sediment provenance combination and sedimentary system of the Member 1 of Paleogene Shahejie Formation, Lixian county slope, Raoyang depression. According to the characteristics of sedimentary gentle slope in Raoyang sag, the distribution of the source systems and "Source-to-Sink" configuration of the Member 1 of Paleogene Shahejie Formation are discussed, based on the detrital zircon U-Pb dating and traditional method of provenance analysis in this study. According to the difference of paleo geomorphology and drilling distribution characteristics, the slope is divided into three areas, A, B and C, which correspond to three provenance systems respectively. More specifically, in terms of the northwest provenance system, the provenance is the Paleozoic igneous rocks from the Xing-Meng orogenic belt, carried by ancient Daqing river system from the northwest to the A district of theslope. As to the west provenance system, the provenance is the Mesozoicigneous rocks, the Meso-Neoproterozoicintrusive rocks, the Mesoproterozoic metamorphic rocks in Laiyuan district, carried by the ancient Tanghe river system from west to the B district of the slope. In the case of the southwest provenance system, the provenance is the Paleoproterozoic metamorphic rocks, carried by the ancient Dasha river system from the southwest to the C district of the slope. There is a positive correlation between detrital zircon content and drainage area.
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Key words:
- provenance system /
- bedrock types /
- zircon U-Pb dating /
- paleo-water system /
- Lixian slope /
- petroleum geology
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图 1 饶阳凹陷蠡县斜坡构造位置及古近系沙河街组层序充填序列
Fig. 1. Structural map of Lixian slope and generalized stratigraphic column of Paleogene Shahe Formation in Raoyang depression
图 3 饶阳凹陷蠡县斜坡古地貌及地震前积反射特征
Fig. 3. Paleo geomorphology and progradational reflections characteristics of Lixian slope in Raoyang depression
图 4 饶阳凹陷蠡县斜坡沙河街组沙一段岩石学特征
研究区外数据刘金龙等(2016)
Fig. 4. Petrological characteristics in the 1st member of Shahejie Formation of Lixian slope, Raoyang sag
图 5 饶阳凹陷蠡县斜坡高104井沙一段锆石阴极发光
Fig. 5. Zircon cathode luminescence plate of the 1st member of Shahejie Formation in Gao 104 well, Lixian slope, Raoyang sag
图 6 饶阳凹陷蠡县斜坡沙一段9口井碎屑锆石Th、U含量及Th/U比值
Fig. 6. Detrital zircon Th, U content and Th/U ratio of 9 wells in the 1st member of Shahejie Formation in Lixian slope, Raoyang sag
图 7 饶阳凹陷蠡县斜坡沙一段高29井、高108井及高30井碎屑锆石U-Pb年龄谐和曲线和频谱
Fig. 7. Detrital zicon U-Pb age harmonic curves and spectrogram of Gao 29, Gao 108 and Gao 30 wells in the 1st member of Shahejie Formation, Lixian sag, Raoyang depression
图 8 饶阳凹陷蠡县斜坡沙一段碎屑锆石U-Pb年龄频谱
井位见图 1b
Fig. 8. Age spectrum of detrital zircon U-Pb age in the 1st member of Shahejie Formation in Lixian slope, Raoyang sag
图 9 饶阳凹陷蠡县斜坡沙一段岩石物理参数关系
Fig. 9. The rock-physics relationships analysis of the 1st member of Shahejie Formation in Lixian slope, Raoyang sag
图 10 饶阳凹陷蠡县斜坡沙一段地层切片SS91(a)及其沉积综合解释(b)
Fig. 10. The RMS straigraphic slice 91 (a) and comprehensive interpretation of sedimentary facies (b) of the 1st member of Shahejie Formation in Lixian slope, Raoyang sag
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