Advanced Search

Liu Min, Chen Zhiming, Chin Qiying. The Role of Organic Matter in the Genesis of Siderite from the Xuanlong Area[J]. Acta Sedimentologica Sinica, 1997, 15(3): 96-102,66.
Citation: Liu Min, Chen Zhiming, Chin Qiying. The Role of Organic Matter in the Genesis of Siderite from the Xuanlong Area[J]. Acta Sedimentologica Sinica, 1997, 15(3): 96-102,66.

The Role of Organic Matter in the Genesis of Siderite from the Xuanlong Area

  • Received Date: 1996-07-11
  • Based on the analysis of siderite distribution, occurrence, chemical composition, structural character-istics, carbon- oxygen isotope characteristics and relationship between siderite and hematite, the papermade a systematic study of siderite in the region, and refered that the genesis of siderite in the Xuanlongarea is the result ofganic matter reducing primary hematite during diagenesis. The ferric and ferreous re-lation depends directely on organic Contents which can comvert the ferreous into the ferric by erduction.The above conclusion was also proved by organic geochemistry data.
  • [1] 朱世兴.河北宣龙区的铁质叠层石及其意义.中国地质科学院院报,天津地质矿产研究所分刊, 1980, 1( 1): 70 ~ 90.
    [2] 杜汝霖,李凤臣,李培菊等.冀西北长城纪宣龙式铁矿层中微体植物化石的发现及其意义.地质论评, 1992, 38(20): 184 ~ 188.
    [3] 刘敏,叶连俊,陈其英等.宣龙铁矿地质地球化学特征及成因探讨.沉积学及岩相古地理学新进展, 1995, 644 ~ 646.
    [4] 刘敏,陈其英,陈志明等.宣龙铁矿生物成铁作用的初步研究.沉积学及岩相古地理学新进展, 1995, 642 ~ 644.
    [5] 汪本善,陈丽容.宣龙区鲕状铁矿的若干特点.地质科学, 1959,8: 232 ~ 240.
    [6] 陈志明,于洁,候奎.冀西北宣龙地区菱铁矿成因.地质科学,1983, 4: 337 ~ 342.
    [7] 王濮,潘兆橹等.系统矿物学.北京: 地质出版社, 1987.
    [8] 刘敏.宣龙铁矿稳定同位素地球化学特征,生物成矿作用研究.北京: 海洋出版社, 1993, 150 ~ 157.
    [9] 陈志明,李菊英,王秀兰.有机质在綦江式菱铁矿床形成过程中的作用,生物成矿作用研究.北京: 海洋出版社, 1993, 119~126.
    [10] Hodgson, G W et al. Geochimistry of Porthy rins. Chlorins andpolycyclic aromatics in soils and sedimentary rocks, Geochim.Cosmochim. Acta, 1968, 32: 732 ~ 772.
    [11] Berger, W H, and Vincent, E, Deep sea catbonaters: Readingthe carbon- iso tope signal. Geologische Rundschan, 1986, 75:249 ~ 269.
    [12] Okita, P M et al. Geochim. Cosmochiml. Acta, 1988, 52: 2679~ 2685.
    [13] Walker, J C G. Suboxic diag enesis in bandediron formation,Na- ture, 1984, 309: 340 ~ 342.
    [14] Froelich, P N et al. Early oxidation of o rganic matter in101pelagisedimets of the eastem epuatorial Altantic suboxic diage-nesis, Geochim. Cosmochim. Acta, 1979, 43: 1075 ~ 1099.
    [15] Coleman, M L, Geochemisty of diagenetic nonsilicate miner-als: Kinetic considerations. Phil Trans. Roy, Soc. 1985, A 315:39 ~ 56.
    [16] C. D.柯蒂斯等.沉积铁矿物的生成,铁的地球化学. 北京: 地质出版社, 1980, 82 ~ 89.
    [17] 朱世兴,邢裕盛等.华北地台中上元古界生物地层序列. 北京: 地质出版社, 1994.
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(692) PDF downloads(309) Cited by()

Proportional views
Related
Publishing history
  • Received:  1996-07-11

The Role of Organic Matter in the Genesis of Siderite from the Xuanlong Area

Abstract: Based on the analysis of siderite distribution, occurrence, chemical composition, structural character-istics, carbon- oxygen isotope characteristics and relationship between siderite and hematite, the papermade a systematic study of siderite in the region, and refered that the genesis of siderite in the Xuanlongarea is the result ofganic matter reducing primary hematite during diagenesis. The ferric and ferreous re-lation depends directely on organic Contents which can comvert the ferreous into the ferric by erduction.The above conclusion was also proved by organic geochemistry data.

Liu Min, Chen Zhiming, Chin Qiying. The Role of Organic Matter in the Genesis of Siderite from the Xuanlong Area[J]. Acta Sedimentologica Sinica, 1997, 15(3): 96-102,66.
Citation: Liu Min, Chen Zhiming, Chin Qiying. The Role of Organic Matter in the Genesis of Siderite from the Xuanlong Area[J]. Acta Sedimentologica Sinica, 1997, 15(3): 96-102,66.
Reference (17)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return