Detrital Zircon U-Pb Geochronology of the Dazhuyuan Formation in Northern Guizhou: Implications for Bauxite Mineralization

Zhi ZHAO; Deng-hong WANG; Pei-gang LI; Zhi-yuan LEI

Rock and Mineral Analysis > 2013 > 32(1): 166-173.

Zhi ZHAO, Deng-hong WANG, Pei-gang LI, Zhi-yuan LEI. Detrital Zircon U-Pb Geochronology of the Dazhuyuan Formation in Northern Guizhou: Implications for Bauxite Mineralization[J]. Rock and Mineral Analysis, 2013, 32(1): 166-173.

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Detrital Zircon U-Pb Geochronology of the Dazhuyuan Formation in Northern Guizhou: Implications for Bauxite Mineralization

1.
Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Land and Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
No.106 Geological Team of Guizhou, Zunyi 563000, China

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Received Date: December 02, 2012
Accepted Date: December 03, 2012
Published Date: January 31, 2013

Abstract

ABSTRACT

The Late Carboniferous Dazhuyuan Formation, an important bauxite bearing bed, lies along the Northern Guizhou-Southern Chongqing formation. For tracing the material source of the bauxite, U-Pb dates on detrital zircon of aluminous from Dazhuyuan bauxite deposit using Laser Ablation-Multicollector Inductively Coupled Plasma-Mass Spectrometry (LA-MC-ICPMS) have been determined. The results show that 84 groups of concordant age are distributed over a wide range, varying from 447 to 2825 Ma, with the main populations ranging from 505-660 Ma (n=5), 714-794 Ma (n=13), 900-1302 Ma (n=42) and 2473-2500 Ma (n=5). Compared with the detrital zircon age spectrum of Paleozoic Clastic of South China, the result lacks the data from about 440-400 Ma, which belongs to the middle-upper Devonian, more similar to a detrital zircon age spectrum of the Ordovician-Lower Devonian. Combined with the regional geological characteristics, it is postulated that (1) the detrital zircons of the aluminous come from the Hanjiadian group (S₁hj), which is the important metallogenic parent rocks of the bauxite. (2) The Caledonian orogeny made the collision between the Cathaysian block and the Yangtze block, implying that the Cathaysia block uplifted rapidly and suffered from erosion in the Silurian, which made a foundation providing a large amount of metallogenic material for the formation of the bauxite.
- Dazhuyuan Formation,
- detrital zircon,
- mineralization,
- bauxite,
- Northern Guizhou

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References (35)

References

章柏盛.微量元素对比在铝土矿成矿物质来源上的应用[J].轻金属,1987(3): 1-4. http://www.cnki.com.cn/Article/CJFDTOTAL-QJSS198703000.htm

卢静文,彭晓蕾,徐丽杰.山西铝土矿床成矿物质来源[J].长春地质学院学报,1997,27(2): 147-151. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ702.004.htm

刘平.八论贵州之铝土矿——黔中-渝南铝土矿成矿背景及成因探讨[J].贵州地质,2001,18(4): 238-243. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ200104005.htm

Bruguier O, Lancelet J R. U-Pb dating on single detrital zircon grains from the Triassic Songpan-Ganzeflysch (Central China): Provenance and tectonic correlations[J]. Earth and Planetary Science Letters,1997,152: 217-231. doi: 10.1016/S0012-821X(97)00138-6

刘长龄.中国石炭纪铝土矿的地质特征与成因[J].沉积学报,1988,6(3): 1-10. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198803000.htm

刘平.黔北务-正-道地区铝土矿地质概要[J].地质与勘探,2007,43(5): 29-33. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200705007.htm

雷志远,廖友常.黔北大竹园铝土矿床地质特征及成因浅析[J].西部探矿工程,2007(9): 94-97. http://www.cnki.com.cn/Article/CJFDTOTAL-XBTK200709036.htm

刘平.初论贵州之铝土矿[J].贵州地质,1987,4(10): 1-12. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ198701000.htm

刘平.三论贵州之铝土矿——黔北铝土矿成矿时代、物质来源及成矿模式[J].贵州地质,1993,10(2): 105-113. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199302001.htm

刘平.论黔北-川南石炭系大竹园组[J].中国区域地质,1996(2): 123-130. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD602.003.htm

刘平.六论贵州之铝土矿——铝土矿矿床成因类型划分意见[J].贵州地质,1996,13(1): 45-60. http://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ601.006.htm

刘平.黔北务正道地区铝土矿地质概要[J].地质与勘探,2007,43(5): 29-33. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKT200705007.htm

殷科华.黔北务正道铝土矿的成矿作用及成矿模式[J].沉积学报,2009,27(3): 452-457. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200903009.htm

侯可军,李延河,田有荣. LA-MC-ICPMS锆石微区原位U-Pb定年技术[J].矿床地质,2009,28(4): 481-492. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGKD201104001484.htm

佘振兵.中上扬子上元古界-中生界碎屑锆石年代学研究[D].武汉:中国地质大学(武汉),2007.

谢士稳,高山,柳小明,高日胜.扬子克拉通南华纪碎屑锆石U-Pb年龄、Hf同位素对华南新元古代岩浆事件的指示[J].地球科学——中国地质大学学报,2009,34(1): 117-126. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200901012.htm

于津海, O’Reilly S Y,王丽娟, Griffin W L,蒋少涌,王汝成,徐夕生.华夏地块古老物质的发现和前寒武纪地壳的形成[J].科学通报,2007,52(1): 11-18. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB200701001.htm

李青,段瑞春,凌文黎,胡明安,张军波,杨振.桂东早古生代地层碎屑锆石U-Pb同位素年代学及其对华夏陆块加里东期构造事件性质的约束[J].地球科学——中国地质大学学报,2009,34(1): 189-202. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200901019.htm

于津海,王丽娟,周新民,蒋少涌,王汝成,徐夕生,邱检生.粤东北基底变质岩的组成和形成时代[J].地球科学——中国地质大学学报,2006,31(1): 38-48. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200601006.htm

于津海,王丽娟,魏震洋,孙涛,舒良树.华夏地块显生宙的变质作用期次和特征[J].高校地质学报,2007,13(3): 474-483. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200703011.htm

王丽娟,于津海,O’Reilly S Y,Griffin W L,孙涛,魏震洋,舒良树,蒋少涌.华夏南部可能存在Grenville期造山作用: 来自基底变质岩中锆石U-Pb定年及Lu-Hf同位素信息[J].科学通报,2008,53(14): 1680-1692. doi: 10.3321/j.issn:0023-074X.2008.14.009

于津海,沈渭洲.南岭地区基低变质岩的组成和形成时代[M]//周新民主编.南岭地区晚中生代花岗岩成因与岩石圈动力学演化.北京: 科学出版社,2007:23-37.

向磊,舒良树.华南东段前泥盆纪构造演化: 来自碎屑锆石的证据[J].中国科学: 地球科学,2010,40(10): 1377-1388. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201010008.htm

陈旭,戎嘉余,Rowley D B,张进,张元动,詹仁斌.对华南早古生代板溪洋的质疑[J].地质论评,1995,41(5): 389-400. http://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199505000.htm

许效松,刘伟,周棣康 ,王国司,张海全,石国山.黔中-黔东南地区下志留统沉积相[J].古地理学报,2009,21(3): 13-20. http://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200901005.htm

毛建仁,厉子龙,赵希林,叶海敏,陈荣,曾庆涛.赣南上犹岩体的锆石 SHRIMP定年和地球化学特征及其构造意义[J].矿物岩石地球化学通报,2007,26(Z1): 18-20. doi: 10.3969/j.issn.1007-2802.2007.z1.010

赵芝,陈振宇,陈郑辉,侯可军,赵正,许建祥,张家菁,曾载淋.赣南加里东期阳埠(垇子下)岩体的锆石年龄、构造背景及含矿性评价[J].岩矿测试,2012,31(3): 530-535. http://www.cnki.com.cn/Article/CJFDTOTAL-YKCS201203030.htm

段亮.南秦岭与扬子地体西北缘志留-泥盆系碎屑锆石物源分析及构造意义[D].西安:西北大学,2010.

沈渭洲,张芳荣,舒良树,王丽娟,向磊.江西宁冈岩体的形成时代、地球化学特征及其构造意义[J].岩石学报,2008,24(10): 2244-2254. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200810006.htm

张芳荣,沈渭洲,舒良树,向磊.江西省早古生代晚期花岗岩的地球化学特征及其地质意义[J].岩石学报,2010,26(12): 3456-3468. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201012003.htm

马昌前,明厚利,杨坤光.大别山北麓的奥陶纪岩浆弧:侵入岩年代学和地球化学证据[J].岩石学报,2004,20(3): 393-402. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200403003.htm

李伍平,王涛,王晓霞.北秦岭灰池子花岗质复式岩体的源岩讨论——元素-同位素地球化学制约[J].地球科学: 中国地质大学学报,2001,26(3): 269-278. http://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200103008.htm

牟传龙,许效松.华南地区早古生代沉积演化与油气地质条件[J].沉积与特提斯地质,2010,30(3): 24-29. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD201003004.htm

Li Z X. Tectonic history of the major East Asian litho-spheric blocks since the mid-Proterozoic: A Synthesis [M]//Flower M F J, Chung S L, Lo C H, eds. Mantle Dynamics and Plate Interactions in East Asia. Washington D C: American Geophysics Union, 1998: 221-243.

Wang D H, Li P G, Qu W J, Yin L J, Zhao Z, Lei Z Y, Wen S F. Discovery and preliminary study of the high tungsten and lithium contents in the Dazhuyuan bauxite deposit, Guizhou, China [J]. Science China: Earth Sciences, 2012, 55(1): 1-8. doi: 10.1007/s11430-011-4320-0

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