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《Acta Sedimentologica Sinica》 2005-04
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Rare Earth Elemental Characteristics of Ordovician-Jurassic Mudstone in Tabei Uplift, Tarim Basin

ZHANG Pei ZHENG Jian-ping ZHANG Rui-sheng YU Chun-mei(State Key Laboratory of Geological Processes and Mineral Resources, Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074)  
Rare earth element (REE) abundance of Ordovician, Triassic and Jurassic mudstone in the Tabei uplift, Tarim basin has been analysed. All the mudstones show the characteristics of high LREE content, uniform HREE and negative Eu anomaly. The ratios such as ∑LREE/∑HREE, La_N/Yb_N, (La/Yb)_ UCC , Eu/Eu* and Ce/Ce*, however, are obviously different among them, and thus reflecting the different sources and environments when they were formed. The mudstones formed in different ages display variable degrees of REE differentiation and negative Eu anomaly. The Ordovician mudstones have high ratios of ∑LREE/∑HREE and LaN/YbN (12.1 and 19.8) and significant negative Eu anomaly (Eu/Eu*=0.59). The Triassic mudstones, however, show unusual low ratios of ∑LREE/∑HREE and LaN/YbN (5.9 and 7.7) and small negative Eu anomaly (Eu/Eu*=0.78). The Jurassic mudstones are similar to the Ordovician samples except less negative Eu anomaly (Eu/Eu*=0.72). Similarly, UCC-normalized REE patterns of samples also show significant changes within different ages. In general, the Ordovician and Jurassic mudstones show slight enrichment of LREE relative to UCC, whereas the Triassic ones show strong LREE depletion. These characteristics indicate that the Ordovician mudstones were formed under a relatively stable sedimentary environment. The sources should be the upper continental crust with high maturity. During Permian-Triassic times, the north of the Tarim basin was tectonic and volcanic, which provide abundant volcanic materials. It stepped into the stable sinking period in Jurssic. The REE difference among mudstones has indicating significance for studying the formation and evolution of the Tarim basin and surrounding orogenic belt.
【Fund】: 国家‘973’项目(G1999043303);; 国家自然科学基金项目(批准号:40273001)资助
【CateGory Index】: P595
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