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Journal ArticleDOI

Kerogen origin, evolution and structure

M. Vandenbroucke, +1 more
- 01 May 2007 - 
- Vol. 38, Iss: 5, pp 719-833
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TLDR
A review of the main advances in kerogen studies since the comprehensive synthesis edited by Durand [Durand, B. as discussed by the authors, 1980] can be found in this paper.
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This article is published in Organic Geochemistry.The article was published on 2007-05-01. It has received 923 citations till now. The article focuses on the topics: Kerogen.

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MonographDOI

The Rock Physics Handbook

TL;DR: The third edition of the reference book as discussed by the authors has been thoroughly updated while retaining its comprehensive coverage of the fundamental theory, concepts, and laboratory results, and highlights applications in unconventional reservoirs, including water, hydrocarbons, gases, minerals, rocks, ice, magma and methane hydrates.
Journal ArticleDOI

Anaerobic digestion of microalgae as a necessary step to make microalgal biodiesel sustainable.

TL;DR: The ability of these CO2 consuming microalgae to purify biogas and concentrate methane is discussed, and anaerobic digestion of the whole biomass appears to be the optimal strategy on an energy balance basis for the energetic recovery of cell biomass.
Journal ArticleDOI

The molecular representations of coal – A review

TL;DR: Between 1942 and 2010 there were >134 proposed molecular level representations (models) of coal, and while they spanned the rank range, bituminous representations are the bulk, with far fewer lignite, and very few subbituminous or anthracite representations.
Journal ArticleDOI

Geochemical evolution of organic-rich shales with increasing maturity: A STXM and TEM study of the Posidonia Shale (Lower Toarcian, northern Germany)

TL;DR: In this article, a combination of compositional organic geochemistry and spectromicroscopy techniques, including synchrotron-based scanning transmission X-ray microscopy (STXM), was used to characterize samples of the Lower Toarcian Posidonia Shale from northern Germany at varying stages of thermal maturation.
Journal ArticleDOI

Biogeochemistry of Microbial Coal-Bed Methane

TL;DR: The anaerobic metabolism of the bacteria breaking coal down to methanogenic substrates, the likely rate-limiting step in biogenic gas production, is not fully understood and coal molecules are more recalcitrant to biodegradation with increasing thermal m...
References
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Book

Petroleum Formation and Occurrence

TL;DR: The early transformation of organic matter from organisms to geochemical fossils and Kerogen has been studied in the literature as mentioned in this paper, with a focus on the migration and accumulation of oil and gas.
Journal ArticleDOI

Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis

TL;DR: Pore water profiles of total CO 2, pH, PO 3−4, NO − 3 plus NO − 2, SO 2− 4, S 2−, Fe 2+ and Mn 2+ have been obtained in cores from pelagic sediments of the eastern equatorial Atlantic under waters of moderate to high productivity as mentioned in this paper.
Book

Petroleum Geochemistry and Geology

John M. Hunt
TL;DR: The development of petroleum geochemistry and geology carbon and origin of life petroleum and its products how oil forms -natural hydrocarbons how oil form -generated hydrocarbon models petroleum generation the origin of natural gas migration and accumulation abnormal pressures the source rock coals, shales, and other terrestrial source rocks petroleum in the reservoir seeps and surface prospecting a geochemical program for petroleum exploration crude oil correlation prospect evaluation as discussed by the authors.
Journal ArticleDOI

Enzymatic combustion: the microbial degradation of lignin

TL;DR: This paper presents a meta-analyses of IGNIN as a stimulus and its applications in medicine and physiology, and discusses the role that IGNIN plays in the development of disease and its role in medicine.
Journal ArticleDOI

Sedimentary pyrite formation: An update

TL;DR: In this article, it was shown that organic matter appears to be the major control on pyrite formation in normal (non-euxinic) terrigenous marine sediments where dissolved sulfate and iron minerals are abundant.
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