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Elemental and Sr-Nd isotopic compositions of Cenozoic sedimentary rocks from the Dongying Sag of Jiyang depression, North China Implications for provenance evolution
Cai, GQ (Cai, Guanqiang); Guo, F (Guo, Feng); Liu, XT (Liu, Xiantai); Sui, SL (Sui, Shuling)
刊名GEOCHEMICAL JOURNAL
2011
卷号45期号:1页码:33-55
关键词geochemistry Sr-Nd isotope provenance Dongying Sag Jiyang depression
ISSN号0016-7002
英文摘要Major, trace element and Sr-Nd isotopic compositions of Cenozoic sedimentary rocks from the Dongying Sag and the Zhanhua Sag, Jiyang Depression, provide evidence for provenance evolution and paleogeographic reconstruction. Compared with the average composition of post-Archean Australian shales (PAAS), the Paleogene sedimentary rocks of Shahejie formation (Es) from the Dongying Sag have similar SiO(2), Al(2)O(3) contents, lower K(2)O, Na(2)O contents with K(2)O/Na(2)O ranging from 0.18 to 4.58, relatively lower contents of V, Cr, Co, Ni, Nb, Ta, Y, Rb, and Cs, and higher contents of Sr, Ba, Zr and Hf. All samples show chondrite-normalized REE patterns similar to that of PAAS, with significant light REE enrichment, flat heavy REE and negative Eu anomalies (Eu/Eu* = 0.71-0.99, average of 0.80). The Sr-Nd isotopic compositions of the Pale)gene sedimentary rocks are different from those of the Neogene sedimentary rocks which generally have higher (87)Sr/(86)Si and lower (143)Nd/(144)Nd. In the geochemical discrimination diagrams (e.g., La/Th-Hf, La-Th-Sc, and Th-Hf-Co), the studied samples were plotted in the area of felsic rocks rather than mafic rocks, which indicated that the source rocks are mainly composed of post-Archean felsic igneous rocks and recycled sedimentary rocks. This is also supported by interelement ratios such as La/Co, La/Th, Th/Co, and Th/Cr. The Sr-Nd isotopic compositions vary from the Paleogene to Neogene sedimentary rocks further suggesting a change in provenance, during which contemporaneous volcanic lava supplied some clasts with higher (143)Nov (144)Nd and lower (87)Sr/(86)Sr ratios for deposition of Paleogene Es sedimentary rocks, whereas the contribution of volcanic detritus became much less during the Neogene time. The geochemistry of sedimentary rocks from the Jiyang depression possibly implies that the Paleozoic sedimentary rocks covering the old metamorphic crystalline basement rocks may not be totally denuded at the surrounding uplifts and highs during the Paleogenc time.
学科主题沉积学与沉积岩
WOS关键词PENNSYLVANIAN-PERMIAN AGE ; RARE-EARTH ELEMENT ; TRACE-ELEMENT ; CRUSTAL EVOLUTION ; MAJOR-ELEMENT ; SILICICLASTIC ROCKS ; VOLCANIC-ROCKS ; BOHAI BASIN ; GEOCHEMISTRY ; SANDSTONES
WOS研究方向Geochemistry & Geophysics
语种英语
出版者GEOCHEMICAL SOC JAPAN
WOS记录号WOS:000287890800004
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/39260]  
专题中国地质调查局
作者单位Geol Sci Res Inst Shengli Oilfield, Dongying 257015, Peoples R China
推荐引用方式
GB/T 7714
Cai, GQ ,Guo, F ,Liu, XT ,et al. Elemental and Sr-Nd isotopic compositions of Cenozoic sedimentary rocks from the Dongying Sag of Jiyang depression, North China Implications for provenance evolution[J]. GEOCHEMICAL JOURNAL,2011,45(1):33-55.
APA Cai, GQ ,Guo, F ,Liu, XT ,&Sui, SL .(2011).Elemental and Sr-Nd isotopic compositions of Cenozoic sedimentary rocks from the Dongying Sag of Jiyang depression, North China Implications for provenance evolution.GEOCHEMICAL JOURNAL,45(1),33-55.
MLA Cai, GQ ,et al."Elemental and Sr-Nd isotopic compositions of Cenozoic sedimentary rocks from the Dongying Sag of Jiyang depression, North China Implications for provenance evolution".GEOCHEMICAL JOURNAL 45.1(2011):33-55.
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