鄂西恩施地区孤峰组岩石地球化学特征及含矿性分析GEOCHEMISTRY AND ORE POTENTIAL OF THE GUFENG FORMATION,ENSHI,WESTERN HUBEI PROVINCE
李朋,胡正祥,宗维,周峰,杜小锋,吴龙
摘要(Abstract):
鄂西恩施地区孤峰组普遍发育一套含骨针和放射虫的硅质岩夹炭质页岩。通过硅质岩岩石学和地球化学特征研究,综合判断中二叠统孤峰组硅质岩沉积环境为大陆边缘中下部与深水盆地结合部位,具有生物与热水混合成因特征,且向上热水参与作用增强,从而导致了矿物元素的分异。结合全岩样品分析结果,认为富矿层位为中上部炭质页岩含量较高的层位,建立了找矿标志,为本区地质找矿工作做出了重要贡献。
关键词(KeyWords): 岩石地层;地球化学特征;硅质岩;成因;孤峰组;二叠系;恩施;湖北
基金项目(Foundation): 中国地质调查局大调查项目(12120114066101);中国地质调查局扬子工程湘西-鄂西成矿带神农架-花垣地区地质矿产调查二级项目(No.DD20160029)
作者(Author): 李朋,胡正祥,宗维,周峰,杜小锋,吴龙
DOI: 10.19839/j.cnki.dcxzz.2017.03.013
参考文献(References):
- 何斌,徐义刚,肖龙,王雅玫,王康明,沙绍礼.2006.峨眉山地幔柱上升的沉积响应及其地质意义.地质评论,52(1):30-37.
- 雷卞军,阙洪培,胡宁,牛志军,汪华.2002.鄂西古生代硅质岩的地球化学特征及沉积环境.沉积与特提斯地质,22(2):70-79.
- 李红敬,解习农,周炼,苏明,彭伟,陈慧.2009.扬子地区二叠系硅质岩成因分析及沉积环境研究.石油实验地质,31(1):564-569.
- 刘家军,郑明华.1993.热水沉积硅质岩的地球化学.四川地质学报,(2):110-118.
- 刘新宇,颜佳新.2007.华南地区二叠纪栖霞组燧石结核成因研究及其地质意义.沉积学报,25(5):730-736.
- 孙秀凤,王国庆.2016.鄂西二叠系孤峰组层状硅质岩及硅质结核成因.铀矿地质,32(1):23-30.
- 王立亭,陆彦邦,赵时久.1994.中国南方二叠纪岩相古地理与成矿作用.北京:地质出版社.1-146.
- 韦恒叶.2012.古海洋生产力与氧化还原指标---元素地球化学综述.沉积与特提斯地质,32(2):76-88.
- 肖龙,徐义刚,梅厚钧,沙绍礼.2003.云南宾川地区峨眉山玄武岩地球化学特征:岩石类型及随时间演化规律.地质科学,38(4):478-494.
- 徐跃通.1997.鄂东南晚二叠世大隆组层状硅质岩成因地球化学及沉积环境.桂林工学院学报,(3):13-21.
- 杨水源,姚静.2008.安徽巢湖平顶山中二叠统孤峰组硅质岩的地球化学特征及成因.高校地质学报,14(1):39-48.
- 郑翔,钱汉东,吴雪枚.2006.湖北恩施双河硒矿床地球化学特征及成因探讨.高校地质学报,12(1):83-92.
- Adachi M,Yamamoto K&Sugisaki R.1986.Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication of ocean ridge activity.Sedimentary Geology,47(1):125-148.
- Bostr9m K&Peterson M.1969.The origin of zluminum-poor ferromanganoan sediments in areas of high heat flow on the East Pacific Rise.Marine geology,7(5):427-447.
- Govindaraju G.1994.Compilation of working values and sample description for geostandards.Geostandards Newslett,18:1-158.
- Jones B&Manning D A C.1994.Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones.Chemical Geology,111(1/2/3/4):111-129.
- Murchey B L&Jones D L.1992.A mid-Permian chert event:wide spread deposition of biogenetic siliceous sediments in coastal,island arc and oceanic basins.Palaeogeography,Palaeoclimatology,palaeoecology,96:161-174.
- Murray R W.1994.Chemical criteria to identify the depositional environment of chert:general principles and applications.Sedimentary Geology,90:213-232.
- Murray R W,Buchholtz Ten Brink M R&Gerlach D C.1991.Rare earth,major and trace elements in chert from the Franciscan Complex and Monterey Group,California:Assessing REEsources to fine-grained marine sediments.Geochimica et Cosmochimica Acta,55(7):1875-1895.
- Murray R W,Buchholtz Ten Brink M R&Gerlach D C.1992.Interoceanic variation in the rare earth,major and trace element depositional chemistry of chert:perspectives gained from the DSDP and ODP record.Geochimica et cosmochimica acta,56(5):1897-1913.
- Rimmer S M.2004.Geochemical paleredox indicators in DevonianMississippian black shales,Central Appalachian Basin(USA).Chemical Geology,206(3/4):373-391.
- Shimizu H&Masuda A.1977.Cerium in chert as an indication of marine environment of its formation.Nature,166(5600):346-348.