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LIU Zu-fa, XIAO Xian-ming, FU Jia-mo, R W T Wilkins. Characteristics of Laser-induced Fluorescence of Some Typical Coals From China and Their R-I-VRo Model[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 687-690.
Citation: LIU Zu-fa, XIAO Xian-ming, FU Jia-mo, R W T Wilkins. Characteristics of Laser-induced Fluorescence of Some Typical Coals From China and Their R-I-VRo Model[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 687-690.

Characteristics of Laser-induced Fluorescence of Some Typical Coals From China and Their R-I-VRo Model

  • Received Date: 1999-02-05
  • Rev Recd Date: 1999-04-20
  • Publish Date: 1999-12-10
  • The Characteristics of fluorescence alteration of some typical coals from China has been investigated by means of laser microprobe. The results show that there are three fluorescence alteration patterns for telocolli- nite. They are positive alteration, negative alteration and negative -positive alteration,depending on the thermal maturation levels of these samples. They occur at VRo less than 0.60%,more than 1.10%,0.60-1.10%,respectively. Two alteration parameters:I4oo and R have been selected to differentiate the fluorescence alteration between Chinese coals and Australian coals. The results indicated that the R-I curve of the Chinese coals is quite similar to that of the Australian coals. However, I400 of telocollinite in the Chinese coals is higher than that of the Australian coals, up to 1000-2000 relative intensity units. The measured VRo of the Chinese coals is different from EqVRo(equivalent vitrinite reflectance) which was derived from their fluorescence parameters in the R-I-VRo model based on the Australian coals, with a higher EqVRo value by 0.0l%-0.04%.According to this,a R-I-VRo model based on the fluorescence characteristics of the Chinese coals has been suggested. This model can be used to correct the measuring vitrinite reflectance for source rocks from Chinese petroliferous basins more correctly than the model of the Australian model. A case study was given for some typical samples from Tuha Basin. The results are plotted to this model. It presents that EqVRo is very close to the measured VRo.
  • [1] 1 Wilkins R W T,et al. Fluorescence alteration and the suppression ofvitrinite reflectance[J].Org. Geochem.,1992,18, 629-640

    2 Wilkins R W T,et al. Should fluorescence alteration replace vitrinite reflectance as a major tool for thermal maturity determination in oil exploration?[J]. Org. Geochem.,1995, 22,191-209

    3 肖贤明,刘德汉,傅家漠等.海相镜质体—海相烃源岩中一种重要生烃母质CJ).石油学报,1997,C1):44-48

    4 赵师庆,王飞宇,刘德汉等.不同煤相中煤和镜质组特征的初步研究[J].中国科学院地球化学研究所有机地球化学开放室研究年报(1987)[C].北京:科学出版社,1988, 23-44

    5 Davis A, Rathbone R F, RuiLin, et al. Observation concerning thenature of maceral fluorescence alteration with time[J]. Org.Geochem.,1990,16: 897-906

    6 肖贤明.有机岩石学及其在油气评价中的应用[M].广州:广东科技出版社,1992. 113-122

    7 Veld H, Wilkins R W T,Xiao Xianming,et al. A fluorescence alteration of multiple macerals (FAMM) study of Netherland coal with "Normal" and "deviating" vitrinite reflectance[J].Org. Geochem.,1997,26,247-255
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  • Received:  1999-02-05
  • Revised:  1999-04-20
  • Published:  1999-12-10

Characteristics of Laser-induced Fluorescence of Some Typical Coals From China and Their R-I-VRo Model

Abstract: The Characteristics of fluorescence alteration of some typical coals from China has been investigated by means of laser microprobe. The results show that there are three fluorescence alteration patterns for telocolli- nite. They are positive alteration, negative alteration and negative -positive alteration,depending on the thermal maturation levels of these samples. They occur at VRo less than 0.60%,more than 1.10%,0.60-1.10%,respectively. Two alteration parameters:I4oo and R have been selected to differentiate the fluorescence alteration between Chinese coals and Australian coals. The results indicated that the R-I curve of the Chinese coals is quite similar to that of the Australian coals. However, I400 of telocollinite in the Chinese coals is higher than that of the Australian coals, up to 1000-2000 relative intensity units. The measured VRo of the Chinese coals is different from EqVRo(equivalent vitrinite reflectance) which was derived from their fluorescence parameters in the R-I-VRo model based on the Australian coals, with a higher EqVRo value by 0.0l%-0.04%.According to this,a R-I-VRo model based on the fluorescence characteristics of the Chinese coals has been suggested. This model can be used to correct the measuring vitrinite reflectance for source rocks from Chinese petroliferous basins more correctly than the model of the Australian model. A case study was given for some typical samples from Tuha Basin. The results are plotted to this model. It presents that EqVRo is very close to the measured VRo.

LIU Zu-fa, XIAO Xian-ming, FU Jia-mo, R W T Wilkins. Characteristics of Laser-induced Fluorescence of Some Typical Coals From China and Their R-I-VRo Model[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 687-690.
Citation: LIU Zu-fa, XIAO Xian-ming, FU Jia-mo, R W T Wilkins. Characteristics of Laser-induced Fluorescence of Some Typical Coals From China and Their R-I-VRo Model[J]. Acta Sedimentologica Sinica, 1999, 17(S1): 687-690.
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