Changes in Type II Kerogen Density as a Function of Maturity: Evidence from the Kimmeridge Clay Formation-Reference-Cited by-同舟云学术

Changes in Type II Kerogen Density as a Function of Maturity: Evidence from the Kimmeridge Clay Formation

Published:2005-10-05 Issue:6 Volume:19 Page:2495-2499
ISSN:0887-0624
Container-title:Energy & Fuels
language:en
Short-container-title:Energy Fuels

Author:

Okiongbo Kenneth S.¹,Aplin Andrew C.¹,Larter Steve R.¹

Affiliation:

1. NRG, School of Civil Engineering and Geosciences, Devonshire Building, University of Newcastle, Newcastle upon Tyne, NE1 7RU, U.K., and PRG, Department of Geology and Geophysics, University of Calgary, 844 Campus Place, NW Calgary, Alberta, T2N 1N4, Canada

Publisher

American Chemical Society (ACS)

Subject

Energy Engineering and Power Technology,Fuel Technology,General Chemical Engineering

Link

https://pubs.acs.org/doi/pdf/10.1021/ef050194%2B

Reference22 articles.

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3. Durand, B.; Alpern, B.; Pittion, J. L.; Pradier, B. InThermal history ofsedimentary basins: Methods and case histories; Naeser, N. D., McCulloh, T. H., Eds.; 1989, pp 441−471.

4. The influence of mineral matter on the separation of amorphous marine kerogens using density gradient centrifugation

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