琼东南盆地陵南低凸起崖城组沉积物源的地球化学与碎屑锆石U-Pb年龄记录
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摘要
为研究琼东南盆地深水区陵南低凸起的LS33A井崖城沉积时期的物源特性,对其进行了地球化学和碎屑锆石U-Pb年龄分析。结果表明,崖城组碎屑锆石年龄为95.8～387.9 Ma,在频谱图上集中于95～106 Ma(燕山期)和214～237 Ma(印支期),相对简单的年龄组合揭示了崖城组沉积时期物源区范围相对有限;微量及稀土元素含量、分布特征和特征参数总体与上陆壳和中国浅海沉积物相近,说明其物源具有相似性。锆石U-Pb年龄记录还揭示崖城组受沉积分选和再循环作用影响不大,其物源主要为来自附近构造隆起的近源沉积,源岩为长英质岩石;物源区构造环境以大陆边缘弧环境为主,同时具有主动大陆边缘特征。结合矿物组合特征,认为琼东南盆地陵南低凸起周缘构造隆起受到了燕山期和印支期构造热事件的影响,形成的酸性岩浆岩为研究区提供了长英质物源,推测本区可能存在变质岩基底。
Geochemistry and detrital zircon U-Pb dating of sediments of the Yacheng Formation from the deep-water Well LS33 A drilled at the Lingnan Low Uplift, Qiongdongnan Basin have been conducted in this paper, in order to discuss the provenance characteristics of sediments of the Yacheng Formation during their sedimentation. Results show that U-Pb ages of detrital zircons from sediments of the Yacheng Formation range from 95.8 Ma to 387.9 Ma, with two major clusters of 95-106 Ma(Yanshanian) and 214-237 Ma(Indosinian). The relatively simple age groups reveal that sediments of the Yacheng Formation were derived from relatively limited sources during their sedimentation. The contents, distribution features, and characteristic parameters of trace elements and rare earth elements of the sediments are analogous to those of upper continental crust and of Chinese shallow-sea sediments, indicating the similarity in material provenances. The geochemistry and U-Pb ages of detrital zircons of the sediments show that sediments of the Yacheng Formation were limitedly influenced by sedimentary sorting and recycling processes, as they are mainly proximal deposits sourced from the felsic rocks in the adjacent tectonic uplift which are tectonically characterized with dominant continental margin arc and minor active continental margin. Combining with analysis of mineral association characteristics, it is shown that tectonic uplifts surrounding the Lingnan Low Uplift, Qiongdongnan Basin were influenced by Indosinian and Yanshanian tectonic hydrothermal events which produced acidic magmatic rocks for felsic provenance of the sediments in the study area and it is further inferred that the metamorphic rock basement could be existed in the study area.
Geochemistry and detrital zircon U-Pb dating of sediments of the Yacheng Formation from the deep-water Well LS33 A drilled at the Lingnan Low Uplift, Qiongdongnan Basin have been conducted in this paper, in order to discuss the provenance characteristics of sediments of the Yacheng Formation during their sedimentation. Results show that U-Pb ages of detrital zircons from sediments of the Yacheng Formation range from 95.8 Ma to 387.9 Ma, with two major clusters of 95-106 Ma(Yanshanian) and 214-237 Ma(Indosinian). The relatively simple age groups reveal that sediments of the Yacheng Formation were derived from relatively limited sources during their sedimentation. The contents, distribution features, and characteristic parameters of trace elements and rare earth elements of the sediments are analogous to those of upper continental crust and of Chinese shallow-sea sediments, indicating the similarity in material provenances. The geochemistry and U-Pb ages of detrital zircons of the sediments show that sediments of the Yacheng Formation were limitedly influenced by sedimentary sorting and recycling processes, as they are mainly proximal deposits sourced from the felsic rocks in the adjacent tectonic uplift which are tectonically characterized with dominant continental margin arc and minor active continental margin. Combining with analysis of mineral association characteristics, it is shown that tectonic uplifts surrounding the Lingnan Low Uplift, Qiongdongnan Basin were influenced by Indosinian and Yanshanian tectonic hydrothermal events which produced acidic magmatic rocks for felsic provenance of the sediments in the study area and it is further inferred that the metamorphic rock basement could be existed in the study area.
引文
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Bhatia M R, Taylor S R. 1981. Trace-element geochemistry and sedimentary provinces: A study from the Tasman geosyncline, Australia. Chemical Geology, 33(1-4): 115-125
Bhatia M R. 1983. Plate tectonics and geochemical composition of sandstones. The Journal of Geology, 91(6): 611-627
Cullers R L. 1994. The chemical signature of source rocks in size fractions of Holocene stream sediment derived from metamorphic rocks in the wet mountains region, Colorado, U.S.A. Chemical Geology, 113(3-4): 327-343
Haskin L A, Frey F A, Schmitt R A, Smith R H. 1966. Meteoritic, solar and terrestrial rare-earth distributions. Physics and Chemistry of the Earth, 7: 167-321
Hu B, Wang L S, Yan W B, Liu S W, Cai D S, Zhang G C, Zhong K, Pei J X, Sun B. 2013. The tectonic evolution of the Qiongdongnan Basin in the northern margin of the South China Sea. Journal of Asian Earth Sciences, 77: 163-182
Jackson S E, Pearson N J, Griffin W L, Belousova E. 2004. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology, 211(1-2): 47-69
Li X H, Li Z X, Li W X, Wang Y J. 2006. Initiation of the Indosinian orogeny in south China: Evidence for a Permian magmatic arc on Hainan Island. The Journal of Geology, 114(3): 341-353
Liu X F, Zhang D J, Zhai S K, Liu X Y, Chen H Y, Luo W, Li N, Xiu C. 2015. A heavy mineral viewpoint on sediment provenance and environment in the Qiongdongnan Basin. Acta Oceanologica Sinica, 34(4): 41-55
Liu Y S, Hu Z C, Gao S, Günther D, Xu J, Gao C G, Chen H H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1-2): 34-43
Ludwig K R. 2003. User's manual for Isoplot 3.0: A geochronological toolkit for Microsoft Excel. Berkely: Berkely Geochronology Center Special Publication, 4: 1-71
Mao J R, Ye H M, Liu K, Li Z L, Takahashi Y, Zhao X L, Kee W S. 2013. The Indosinian collision-extension event between the South China Block and the Palaeo-Pacific plate: Evidence from Indosinian alkaline granitic rocks in Dashuang, eastern Zhejiang, South China. Lithos, 172-173: 81-97
Mclennan S M, Hemming S, Mcdaniel D K, Hanson G N. 1993. Geochemical approaches to sedimentation, provenance, and tectonics. Geological Society of America Special Papers, 284: 21-40
Mclennan S M, Taylor S R. 1980. Th and U in sedimentary rocks: Crustal evolution and sedimentary recycling. Nature, 285(5767): 621-624
Mclennan S M, Taylor S R. 1991. Sedimentary rocks and crustal evolution: Tectonic setting and secular trends. The Journal of Geology, 99(1): 1-21
Mclennan S M. 1989. Rare earth elements in sedimentary rocks: Influence of provenance and sedimentary processes. Reviews in Mineralogy and Geochemistry, 21: 169-200
Nasdala L, Hofmeister W, Norberg N, Martinson J M, Corfu F, D?rr W, Kamo S L, Kennedy A, Kronz A, Reiners P W, Frei D, Kosler J, Wan Y S, G?tze J, H?ger T, Kr?ner A, Valley J W. 2008. Zircon M257-a homogeneous natural reference material for the ion microprobe U-Pb analysis of zircon. Geostandards and Geoanalytical Research, 32(3): 247-265
Nesbitt H W, Markovics G, Price R C. 1980. Chemical processes affecting alkalis and alkaline earths during continental weathering. Geochimica et Cosmochimica Acta, 44(11): 1659-1666
Prokopiev A V, Toro J, Miller E L, Gehrels G E. 2008. The paleo-Lena River-200 m.y. of transcontinental zircon transport in Siberia. Geology, 36(9): 699-702
Rudnick R L, Gao S. 2003. Composition of the continental crust. Treatise on Geochemistry, 3: 1-64
Sewell R J, Davis D W, Campbell S D G. 2012. High precision U-Pb zircon ages for Mesozoic igneous rocks from Hong Kong. Journal of Asian Earth Sciences, 43(1): 164-175
Sircombe K N. 1999. Tracing provenance through the isotope ages of littoral and sedimentary detrital zircon, eastern Australia. Sedimentary Geology, 124(1-4): 47-67
Sun W D, Ding X, Hu Y H, Li X H. 2007. The golden transformation of the Cretaceous plate subduction in the west Pacific. Earth and Planetary Science Letters, 262(3-4): 533-542
Taylor S R, Mclennan S M. 1985. The Continental Crust: Its Composition and Evolution. London: Blackwell Scientific Publications
Turekian K K, Wedepohl K H. 1961. Distribution of the elements in some major units of the earth's crust. Geological Society of America Bulletin, 72(2): 175-192
Wang Y J, Fan W M, Zhang G W, Zhang Y H. 2013. Phanerozoic tectonics of the South China Block: Key observations and controversies. Gondwana Research, 23(4): 1273-1305
Ye H M, Mao J R, Zhao X L, Liu K, Chen D D. 2013. Revisiting Early-Middle Jurassic igneous activity in the Nanling Mountains, South China: Geochemistry and implications for regional geodynamics. Journal of Asian Earth Sciences, 72: 108-117
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