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Geochemical implications from torbanite

 

Speaker: Shun-Wen Yu

 

Abstract

Torbanite are exinite-riched coals with massive appearance and conchoidal fractures. Geochemical analysis were performed characterize their geochemical implications. By using density gradient centrifugation, we can sparate torbanite into alginate and amorphous organic matrix. In addition, H/C and O/C atomic ratios were evaluated after elemental analysis. Furthermore, the results from Flash pyrolysis-gas chromatography/mass spectrometry indicate that the higher hopanes, linear and non-linear carbon skeletons of matrix implied an origin of multiple precursors. Finally, the stable hydrogen isotopic compositions of individual hydrocarbons analysis approved to be a useful method to reflect and reconstruct the depositional of samples studied.

 

Reference

Han Z., Kruge M. A., Crelling J. C. and Stankiewicz B. A. (1995) Organic Geochemical characterization of the density fractions of a Permian tobanite. Org. Geochem. Vol. 21, No. 1, pp. 39-50.

(Abstract) (Full text)

Dawson D., Grice K., Wang S. X., Alexander R. and Radke J. (2004) Stable hydrogen isotopic composition of hydrocarbons in torbanites ( Late Carboniferous to Late Permian ) deposited under various climatic conditions. Org. Geochem. Vol. 35, pp. 189-197.

(Abstract) (Full text)