Abstract
Abstract Critical examination of the data on elemental compositions of humic substances and the corresponding kerogens reported by various investigators led to a modified scheme of formation of kerogens. According to the proposed route, only the humic substances rich in carboxyl groups, such as soil fulvic acids, can, in principle, contribute together with lipids to the formation of type II hydrogen-rich kerogen, whereas soil humic acids contribute to the formation of type III kerogen.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.