Citation: | SHI Jizhong, LU Jincai, WEI Jianshe, NIU Yazhuo, JIANG Ting, HAN Xiaofeng, XU Wei. 2018: Petrology, geochemistry and sedimentary environment of Permian siliceous rocks in Yingen-Ejin basin and its adjacent areas. Geological Bulletin of China, 37(1): 120-131. DOI: 10.12097/gbc.dztb-37-1-120 |
The geochemical characteristics and depositional environment of Permian siliceous rocks were studied based on the petrological characteristics, major elements and rare earth elements. According to the test results, Hangwula sectional siliceous rocks' Al/(Al+Fe+Mn)values are 0.68~0.78, with an average of 0.73; δCe values are 0.89~0.94, with an average of 0.90; Erduanjing sectional siliceous rocks' Al/(Al+Fe+Mn)values are 0.50~0.67, with an average of 0.60; δCe values are 0.85~0.90, with an average of 0.88. In the Al-Fe-Mn triangular diagram, samples fall into biochemically-deposited area, which indicates a biochemically-deposited origin for these rocks. Hangwula sectional siliceous rocks' Al2O3/(Al2O3+Fe2O3)values are 0.78~0.86, with an average of 0.83; MnO/TiO2 values are 0.04~0.40, with an average of 0.16;(La/Ce)N values are 1.02~1.15, with an average of 1.10; Ceanom values are -0.041~-0.001, with an average of -0.029. Erduanjing sectional siliceous rocks' Al2O3/(Al2O3+Fe2O3)values are 0.82~ 0.91, with an average of 0.87; MnO/TiO2 values are 0.05~0.47, with an average of 0.24;(La/Ce)N values are 1.00~1.12, with an average of 1.06; Ceanom values are -0.058~-0.033, with an average of -0.045. All these geochemical characteristics suggest that these siliceous rocks were deposited in a continental margin setting where the sea water in the period of deposition was under an anoxic condition.
杨水源, 姚静.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[J].高校地质学报, 2008, 14(1):39-48. https://www.wenkuxiazai.com/doc/209c8ed8ce2f0066f533229b-2.html
|
唐世荣, 王东安.硅岩研究的进展[J].地球科学进展, 1994, 9(6): 71-74. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ406.010.htm
|
雷卞军, 阙洪培, 胡宁, 等.鄂西古生代硅质岩的地球化学特征及沉积环境[J].沉积与特提斯地质, 2002, 22(2):70-79. https://www.wenkuxiazai.com/doc/2476c7fdaef8941ea76e0571-4.html
|
冯胜斌, 周洪瑞, 燕长海, 等.东秦岭二郎坪群硅质岩地球化学特征及其沉积环境意义[J].现代地质, 2007, 21(4):675-682. https://www.wenkuxiazai.com/doc/ffd4e4280912a216147929c3.html
|
谢力, 尹海权, 周洪瑞, 等.内蒙古阿拉善地区恩格尔乌苏缝合带二叠纪放射虫及其地质意义[J].地质通报, 2014, 33(5):691-697. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?file_no=20140510&flag=1
|
尚庆华.北方造山带内蒙古中、东部地区二叠纪放射虫的发现及意义[J].科学通报, 2004, 49(24):2574-2579. doi: 10.3321/j.issn:0023-074X.2004.24.014
|
冯庆来.放射虫古生态的初步研究[J].地质科技情报, 1992, 11 (2):41-46. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkq199202011&dbname=CJFD&dbcode=CJFQ
|
夏林圻, 夏祖春, 徐学义, 等.天山及邻区石炭纪—早二叠世裂谷火山岩岩石成因[J].西北地质, 2008, 41(4):1-68. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz200804001
|
卢进才, 陈高潮, 李玉宏, 等.银额盆地及邻区石炭系—二叠系油气地质条件与资源前景[M].北京:地质出版社, 2012.
|
金玉玕, 范影年, 王向东, 等.中国地层典:二叠系[M].北京:地质出版社, 2000.
|
卢进才, 魏仙样, 陈高潮, 等.内蒙古西部额济纳旗及其邻区石炭—二叠系沉积建造与生烃条件——油气地质条件研究之一[J].地质通报, 2011, 30(6):811-826. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?file_no=20110602&flag=1
|
史冀忠, 陈高潮, 李玉宏, 等.内蒙古西部额济纳旗雅干地区二叠系埋汗哈达组的岩石学特征及沉积环境[J].地质通报, 2011, 30 (6):972-982. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?file_no=20110619&flag=1
|
杨建民, 王登红, 毛景文, 等.硅质岩岩石化学研究方法及其在"镜铁山式"铁矿床中的应用[[J].岩石矿物学杂志, 1999, 18(2): 108-118. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz199902002
|
刘家军, 郑明华.热水沉积硅质岩的地球化学[J].四川地质学, 1993, 13(2):110-118.
|
Adachi M, Yamamoyo K, Sugisaki R. Hydrothermal chert and associated siliceous rocks from the Northern Pacific:Their geological significance as indication of ocean ridge activity[J]. Sedimentary Geology, 1986, 47(1/2):125-148. http://www.sciencedirect.com/science/article/pii/0037073886900758
|
Murray R W, Brink M R, Gerlach D L, et al. Rare earth, major, and trace elements in chert from the Franciscan complex and Monterey group, California:assessing REE sources to fine-grained marine sediments[J]. Geochimica et Cosmochimica Acta, 1991, 55 (7): 1975-1985. https://www.sciencedirect.com/science/article/pii/0016703791900309
|
梁斌, 王全伟, 冯庆来, 等.川西鲜水河断裂带三叠系如年各组放射虫硅质岩的地球化学特征[J].地质科技情报, 2004, 23(1):16-120. http://www.docin.com/p-740810480.html
|
Sugisaki R, Yamamoto K, Adachi M. Triassic bedded cherts in central Japan are not pelagic[J]. Nature, 1982, 298 (5875):644-647. doi: 10.1038/298644a0
|
Wright J, Holler W T. Paleoredox variation in ancient oceans recorded by rare earth elements in fossil apatite [J]. Geochim Cosmochim Acta, 1987, 51:631-644. doi: 10.1016/0016-7037(87)90075-5
|
卜建军, 吴俊, 段先锋, 等.银根-额济纳旗盆地恩格尔乌苏一带二叠系腕足类动物群及其意义[J].地质科技情报, 2013, 32 (3): 1-5. http://www.docin.com/p-865966626.html
|
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