Newsletter

Newsletter
Author: Cornell University. Engineering Library
Publisher:
Total Pages: 576
Release: 1979
Genre: Engineering
ISBN:

Theory and Practice of Hydrocarbon Generation within Space-Limited Source Rocks

Theory and Practice of Hydrocarbon Generation within Space-Limited Source Rocks
Author: Defan Guan
Publisher: Springer
Total Pages: 198
Release: 2016-11-15
Genre: Science
ISBN: 9811024073

This book analyzes hydrocarbon generation and accumulation within space-limited source rocks. The authors draw conclusions based on the principles of basin formation, hydrocarbon generation and accumulation, coupled with the practice of terrigenous basins in eastern China. Hydrocarbon generation and expulsion have been quantitatively assessed in space-limited source rock systems. This book explores new hydrocarbon generation and expulsion models to reflect real geological situations more accurately. The theory and practice proposed in this book challenge the traditional theory of kerogen thermal degradation and hydrocarbon generation.

Petroleum Source Rocks Characterization and Hydrocarbon Generation

Petroleum Source Rocks Characterization and Hydrocarbon Generation
Author: Nabil Mohammed Al-Areeq
Publisher:
Total Pages:
Release: 2018
Genre: Technology
ISBN:

This chapter is proposed to give the principal learning on the application of the formation of petroleum source rocks and hydrocarbon generation to exploration activities. The evaluation of petroleum source rocks and hydrocarbon generation is a very important skill for explorationists to define the location and type of petroleum prospects in a region. In this chapter, subsurface samples from case study (Sayun-Masilah basin) were used to determine the source rock characteristics and petroleum generative potentials of prospective source rocks. Qualitative and quantitative evaluation of the source rock in this basin was done by means of geochemical and geophysical approaches for four rock units. It is clear that Madbi Formation is considered the main source, in which the organic carbon content reached up to more than 5.2 wt%. The types of organic matter from rock-eval pyrolysis data indicated that type I kerogen is the main type, in association with type II, and a mixture of types II and III kerogens. The study of the different maturation parameters obtained from rock-eval pyrolysis, such as Tmax and vitrinite reflectance, reflects that the considered rock units are occurred in different maturation stages, ranging from immature to mature sources. One-dimensional basin modeling was performed to analyze the hydrocarbon generation and expulsion history of the source rocks in the study area based on the reconstruction of the burial and thermal maturity histories in order to improve our understanding of the hydrocarbon generation potential. Calibration of the model with measured vitrinite reflectance (%Ro) and borehole temperature (BHT) data indicates that the paleo-heat flow was high at Late Jurassic. The models also indicate that the early hydrocarbon generation in the Madbi source rock occurred during late Cretaceous and the main hydrocarbon generation has been reached approximately at Early Eocene. Therefore, the Madbi source rock can be considered as generative potentials of prospective source rock horizons in the Sayun-Masilah basin.

Origin and Chemistry of Petroleum

Origin and Chemistry of Petroleum
Author: Gordon Atkinson
Publisher: Elsevier
Total Pages: 127
Release: 2013-10-22
Genre: Nature
ISBN: 1483189775

Origin and Chemistry of Petroleum explains that petroleum is produced from exceptionally disseminated organic matter of biological origin encased in extremely buried sediments. Production of petroleum starts when such sediments are exposed to higher temperatures resulting from increased depths of entombment in the sedimentary column. The book discusses that once the petroleum is created from source rocks, the material transfers into porous reservoir rocks. Such rocks, when discovered, will give enough supply of petroleum for commercial production. An evaluation of the molecular analysis of the thermal history of sediments is also discussed in the book. Concepts such as the biological marker compounds, stereochemical conversion, and lower Toarcian sediments are covered in detail. Analysis of organic matters, such as acyclic isoprenoids, steranes, hopanes, and porphyrins, is highlighted. The molecular distributions and stereochemical ratios are also covered in the book. The text can serve as a valuable tool for geologists, chemists, miners, students, and researchers in the field of chemistry.