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Tang Shirong, Wang Dongan, Li Renwei. Organic Petrology of the CambriarrSinian Chert from the Xiangchuan Region[J]. Acta Sedimentologica Sinica, 1997, 15(1): 54-58.
Citation: Tang Shirong, Wang Dongan, Li Renwei. Organic Petrology of the CambriarrSinian Chert from the Xiangchuan Region[J]. Acta Sedimentologica Sinica, 1997, 15(1): 54-58.

Organic Petrology of the CambriarrSinian Chert from the Xiangchuan Region

  • Received Date: 1996-06-21
  • Publish Date: 1997-03-10
  • The Xiangchuan regionis referred to Shoushan County,Sichuan Province and the western and middle parts of Hunan Province where Sinian-Cambrian bedded cher is are w ell-dev eloped. T he orgyic car-bon content in the chert samples is relatively high, ranging from 0. 06 to 9. 00% and averaging 1. 91%.The linear positive relationship between organic carbon concentrations and some trace element contentsis not clear. Microscopic studies of the kerogen from the chert samples show that the main componentsprobably take place; and 3) that the chert is formed in a shallow continertal-margin stagnant basin.results sug-gent that the primary mother materials basically belong to Type一I amorphous kerogen. On the Van Krevelen diagram,all samples fall into the metagenesis field. Stable carbon isotopes of kerogen from the chert samples range from一29. 30 t0,一3 5. 84%.Analysis of thefeatures of organic petrology mentionedabove suggests 1)that organisms and their degraded products contribute much to the formation of chert, 2) that in the formation of the chert a scalled elimination of impurity matters”processes may
  • [1] 1 王东安.扬子地台晚元古代以来硅岩地球化学特征及其成因地质科学.1994, 29( 1): 41-54.

    2 夏文杰.周浩达.工熙林等.中国南方震旦纪岩相古地理与成矿作用北京:地质出版社.1994.107.

    3 唐世荣.工东安.硅岩研究的进展.地球科学进展.1994, ( 6): 71一75.

    4 蒲心纯.张继庆.殷积成等.上扬子区晚震旦世沉积岩沉积相及矿产.重庆出版社,1984, 1-25.
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  • Received:  1996-06-21
  • Published:  1997-03-10

Organic Petrology of the CambriarrSinian Chert from the Xiangchuan Region

Abstract: The Xiangchuan regionis referred to Shoushan County,Sichuan Province and the western and middle parts of Hunan Province where Sinian-Cambrian bedded cher is are w ell-dev eloped. T he orgyic car-bon content in the chert samples is relatively high, ranging from 0. 06 to 9. 00% and averaging 1. 91%.The linear positive relationship between organic carbon concentrations and some trace element contentsis not clear. Microscopic studies of the kerogen from the chert samples show that the main componentsprobably take place; and 3) that the chert is formed in a shallow continertal-margin stagnant basin.results sug-gent that the primary mother materials basically belong to Type一I amorphous kerogen. On the Van Krevelen diagram,all samples fall into the metagenesis field. Stable carbon isotopes of kerogen from the chert samples range from一29. 30 t0,一3 5. 84%.Analysis of thefeatures of organic petrology mentionedabove suggests 1)that organisms and their degraded products contribute much to the formation of chert, 2) that in the formation of the chert a scalled elimination of impurity matters”processes may

Tang Shirong, Wang Dongan, Li Renwei. Organic Petrology of the CambriarrSinian Chert from the Xiangchuan Region[J]. Acta Sedimentologica Sinica, 1997, 15(1): 54-58.
Citation: Tang Shirong, Wang Dongan, Li Renwei. Organic Petrology of the CambriarrSinian Chert from the Xiangchuan Region[J]. Acta Sedimentologica Sinica, 1997, 15(1): 54-58.
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