Palaeobotanical Repository@BSIP
 

HomePalaeobotanistVolume 67 (2018)


Title: Kerogen typing using palynofacies analysis in Permian Barren Measures Formation in Raniganj sub–basin, East India
Authors: Ahmed, Waquar
Bhat, G.M.
Mclennan, J.
Sinha, H.N.
Kanungo, S.
Pandita, S.K.
Singh, Y.
Hakhoo, N.
Hafiz, M.
Thusu, B.
Choudhary, N.H.
Keywords: Kerogen
Palynofacies
Thermal maturity
Barren Measures Formation
Damodar Basin
Issue Date: 2018
Citation: Palaeobotanist (2018) 67(2): 113-122
Abstract: The objective of the study is the simple assessment of kerogen type in Barren Measures Formation shale using palynofacies. The Barren Measures Formation sandwiched between the coal–rich formations consist of organic–rich black carbonaceous shales. These ̴̴ 1000 m thick, black shales are in the productive gas window having kerogen types III with excellent gas generation potential as proven in recent pyrolysis studies. In this study, the palynological analysis of the four core samples of the Barren Measures Formation shale was done. The analysis has revealed three types of kerogen assemblages, viz. palynomorphs, phytoclasts and amorphous organic matter. The palynomorph assemblage consists of spores and pollen; phytoclasts consist of secondary xylem wood macrophyte plant debris and amorphous organic matter is a higher plant decomposed product. Based on the application of published kerogen classification and correlation of Tyson (1995), the pure kerogen type in these shales is categorized as mixed type; type II (oil prone) and type III (gas prone). However, the gas–prone kerogen assemblage gets relatively dominant in the samples from greater depth in the studied borehole. Our results are analogous to the previously published outcomes of kerogen typing evaluated using Rock–Eval pyrolysis experiments.
URI: http://14.139.63.228:8080/pbrep/handle/123456789/2161
Appears in Collections:Volume 67 (2018)

Files in This Item:

File Description SizeFormat
PbV67N2_113.pdf7.75 MBAdobe PDFView/Open
View Statistics

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

 

  Maintained by Knowledge Resource Centre, BSIP