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Zhong Jianhua. Investigation on Longtan Coal Series of Baohetang,Middle Hunan[J]. Acta Sedimentologica Sinica, 1993, 11(1): 75-83.
Citation: Zhong Jianhua. Investigation on Longtan Coal Series of Baohetang,Middle Hunan[J]. Acta Sedimentologica Sinica, 1993, 11(1): 75-83.

Investigation on Longtan Coal Series of Baohetang,Middle Hunan

  • Received Date: 1992-02-07
  • Publish Date: 1993-03-10
  • Longtan coal series of Baohetang, Middle Hunan, has been investigated in detail by means of sedimentalogy, coal petrology and geochemistry. It is suggested that Baohetang coal was formed in delta environment. Most of coal seam I and n was formed in water-covered swamp that developed from distributary bay. The swamp was often influenced by river and tide. Boron contents of 17 coal samples range from 10 to 500ppm, concentrated in 50- 500ppm ( 15 samples) with an average of 152ppm. Comparition Baohetang coal with those deposited in fresh-water environment shows that the former is more boron-riched and which indicates brakish to semi-brakish water environment, moreover, their rations B / Ga, V / Zr, V / Ni. V / Zn and Sr / Ba are also different obviously. Fe2O3 contents of the 17 coal samples fall in the range of 4.54-20.07% with an average of 9.7%. and SO3 contents from 0.48-10. 85% ( average 5. 85% ) , ratio of ( Fe2O3+CaO+MgO) / (Sio2+Al2O3)from 0.08-0.78 with the mean of 0.34. Baohetang coal has striking features, mainly in coal petrology and Rock- Eval. The coal is characterised by low vitrinite content (from 30% to 52% ) , high sapropel groundmass and transitional macerals content 10%-21% and 25-49%. respectively) . Sapropel groundmass and some hydrogen-rich vitrinites exhausted a great deal of exudatinite, as a result, this makes the coal series contain a little oil. The coal has a higher production of S2, ranging from 198.40-212.40 ( mg / g) , suggests its oil forming potential. The aboundant transitional macerals must have been carried into the water-covered swamp from the oxidized zone of bank-back swamp by flood or tide. The paleocurrent analysis reveals that the sediments came mainly from the east (Shuangfeng-Guandimiao ancient land ?) and the north (Longshan uplift). but not from Xuefeng ancient land. Otherwise, three kinds of sedimental structures (bunch cross-bedding, derived ripple and washing-filling structure) have been discribed in detail, A coal-forming modle of Baohetang coal has been established.
  • [1] (1) 张川波等,1983,辽宁北票附近中侏罗世晚期的沙漠沉积。沉积学报,第1卷,第4期,48-60页.

    (2) 钟建华等,1990,湘中保和堂煤的特征.科学通报,第35卷,第20期,1569-1571页。

    (3) 煤炭科学研究院地质勘探分院、山西省煤田地质勘探公司,1987,太原西山含煤地层沉积环境。北京:煤炭工业出版社,482页.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  1992-02-07
  • Published:  1993-03-10

Investigation on Longtan Coal Series of Baohetang,Middle Hunan

Abstract: Longtan coal series of Baohetang, Middle Hunan, has been investigated in detail by means of sedimentalogy, coal petrology and geochemistry. It is suggested that Baohetang coal was formed in delta environment. Most of coal seam I and n was formed in water-covered swamp that developed from distributary bay. The swamp was often influenced by river and tide. Boron contents of 17 coal samples range from 10 to 500ppm, concentrated in 50- 500ppm ( 15 samples) with an average of 152ppm. Comparition Baohetang coal with those deposited in fresh-water environment shows that the former is more boron-riched and which indicates brakish to semi-brakish water environment, moreover, their rations B / Ga, V / Zr, V / Ni. V / Zn and Sr / Ba are also different obviously. Fe2O3 contents of the 17 coal samples fall in the range of 4.54-20.07% with an average of 9.7%. and SO3 contents from 0.48-10. 85% ( average 5. 85% ) , ratio of ( Fe2O3+CaO+MgO) / (Sio2+Al2O3)from 0.08-0.78 with the mean of 0.34. Baohetang coal has striking features, mainly in coal petrology and Rock- Eval. The coal is characterised by low vitrinite content (from 30% to 52% ) , high sapropel groundmass and transitional macerals content 10%-21% and 25-49%. respectively) . Sapropel groundmass and some hydrogen-rich vitrinites exhausted a great deal of exudatinite, as a result, this makes the coal series contain a little oil. The coal has a higher production of S2, ranging from 198.40-212.40 ( mg / g) , suggests its oil forming potential. The aboundant transitional macerals must have been carried into the water-covered swamp from the oxidized zone of bank-back swamp by flood or tide. The paleocurrent analysis reveals that the sediments came mainly from the east (Shuangfeng-Guandimiao ancient land ?) and the north (Longshan uplift). but not from Xuefeng ancient land. Otherwise, three kinds of sedimental structures (bunch cross-bedding, derived ripple and washing-filling structure) have been discribed in detail, A coal-forming modle of Baohetang coal has been established.

Zhong Jianhua. Investigation on Longtan Coal Series of Baohetang,Middle Hunan[J]. Acta Sedimentologica Sinica, 1993, 11(1): 75-83.
Citation: Zhong Jianhua. Investigation on Longtan Coal Series of Baohetang,Middle Hunan[J]. Acta Sedimentologica Sinica, 1993, 11(1): 75-83.
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