Petroleum Geoscience From Sedimentary Environments to Rock Physics
Book Details :
LanguageEnglish
Pages518
FormatPDF
Size32.2 MB



Petroleum Geoscience From Sedimentary Environments to Rock Physics



Petroleum Geoscience: From Sedimentary Environments to Rock Physics by Knut Bjorlykke | PDF Free Download.

Petroleum Geoscience Contents


  • Introduction to Petroleum Geology
  • Introduction to Sedimentology
  • Sedimentary Geochemistry
  • Sandstones and Sandstone Reservoirs 
  • Carbonate Sediments
  • Shales, Silica Deposits and Evaporites
  • Stratigraphy
  • Sequence Stratigraphy, Seismic Stratigraphy, and Basin Analysis
  • Heat Transport in Sedimentary Basins
  • Subsurface Water and Fluid Flow in Sedimentary Basins
  • Introduction to Geomechanics: Stress and Strain in Sedimentary Basin
  • The Structure and Hydrocarbon Traps of Sedimentary Basins
  • Compaction of Sedimentary Rocks Including Shales, Sandstones, and Carbonates 
  • Source Rocks and Petroleum Geochemistry
  • Petroleum Migration
  • Well Logs: A Brief Introduction
  • Seismic Exploration
  • Explorational Rock Physics – The Link Between Geological Processes and Geophysical Observables
  • 4D Seismic 
  • Production Geology
  • Unconventional Hydrocarbons: Oil Shales, Heavy Oil, Tar Sands, Shale Gas, and Gas Hydrates
  • Geology of the Norwegian Continental Shelf

Introduction to Petroleum Geoscience From Sedimentary Environments to Rock Physics


Petroleum geology comprises those geological disciplines which are of the greatest significance for the finding and recovery of oil and gas. Since most of the obvious and “easy to find” petroleum already has been discovered it is necessary to use sophisticated methods in the exploration of sedimentary basins.

These include advanced geophysical techniques and basin modeling. There is also much more emphasis now on enhanced recovery from the producing fields.

Petroleum technology has made great progress and many new tools and modeling programs have been developed, both in exploration and production.

It is, however, important to understand the geological processes which determine the distribution of different sedimentary rocks and their physical properties.

This knowledge is fundamental to being able to successfully apply the methods now available. It is difficult to know where to start when teaching petroleum geology because nearly all the different disciplines build on each other.

This introductory chapter will provide a short and rather simple overview of some aspects of petroleum geology to introduce the subject and the problems.

Most of the other chapters will then expand on what is presented here to provide a better background in relevant subjects.

Since practically all petroleum occurs in sedimentary rocks, sedimentary geology forms one of the main foundations of petroleum geology.

Sedimentological models are used to predict the location of different facies in the sedimentary basins and from that the likely presence of source rocks with a high content of organic matter, reservoir rocks, and cap rocks.

The distribution and geometry of potential sandstones or carbonate reservoirs require detailed sedimentological models, and sequence stratigraphy has been a useful tool in such reconstructions.

The biostratigraphic correlation of strata encountered in exploration wells is achieved by micropalaeontology (including palynology), a field developed very largely by the oil industry.

Due to the small size of the samples obtained during drilling operations, one cannot rely on macrofossils; even in core samples, the chance of finding good macrofossils is poor.

By contrast, a few grams of rock from the drill cuttings may contain several hundred microfossils or palynomorphs.

These also usually provide better stratigraphic resolution than macrofossils. Reservoir rocks are mostly sandstones and carbonates which are sufficiently porous to hold significant amounts of petroleum. The composition and properties of other rock types such as shales and salt are also important.

The sedimentary environments (sedimentary facies) determine the distribution of reservoir rocks and their primary composition.

Sediments do, however, alter their properties with increasing overburden due to diagenesis during burial. Diagenetic processes determine the porosity, permeability, and other physical properties such as velocity, in both sandstone and limestone reservoirs. Chemical processes controlling mineral reactions are important.

Organic geochemistry, which includes the study of organic matter in sediments and its transformation into hydrocarbons, has become another vital part of petroleum geology.

Tectonics and structural geology provide an understanding of the subsidence, folding, and uplift responsible for the creation and dynamic history of a basin.

The timing of the folding and faulting that forms structural traps is very important in relation to the migration of hydrocarbons.

Seismic methods have become the main tool for mapping sedimentary facies, stratigraphy, sequence stratigraphy, and tectonic development.

Marine seismic recorded from ships has become very efficient and seismic lines are shot at only a few 100 m spacing or less.

Because of the rapid improvement in the quality of seismic data processing techniques, geological interpretation of seismic data has become an entirely new and expanding field.

Seismic and other geophysical data are often the only information we have, particularly for offshore exploration where drilling is very costly.

Shooting seismic lines with a close spacing allow high-resolution 3D seismic imagery to be produced for critical parts of sedimentary basins. By repeating a 3D reservoir seismic survey during production, one can observe how the gas/oil and oil/water contacts move as the reservoir is depleted.

This is called 4D seismic because time provides the fourth dimension. Geophysical measurements may include gravimetry and magnetometry; electromagnetic methods that were used mostly in ore exploration have also been applied to oil exploration.

Electromagnetic methods have been used to detect sediments with low resistivity due to the presence of oil instead of saline water.

This method requires a few 100 m of water and relatively shallow accumulation. Seismic surveys are more expensive on land than by ship at sea because geophones have to be placed in a grid, often on uneven and difficult land surfaces.

Drilling on land, however, costs much less than from offshore rigs, and a much denser well spacing can be used during both exploration and production.

Indirect methods of mapping rock types employing geophysical aids are becoming increasingly important in petroleum geology, but it is still necessary to take samples and examine the rocks themselves.

A petroleum geologist should have broad geological training, preferably also from fieldwork. Geophysical well-logging methods have developed equally rapidly, from simple electric and radioactive logs to highly advanced logging tools that provide detailed information about the sequence penetrated by the well.

Logs provide continuity of information about the rock properties which one can seldom obtain from exposures or core samples.

This information makes it possible to interpret not only the lithological composition of the rocks and the variation of porosity and permeability but also the depositional environment.

Image logs make it possible also to detect bedding and fractures inside the wells. Practical petroleum geology is not only based on many different geological and geophysical disciplines.

A good background in basic chemistry, physics, mathematics, and computing is also required, particularly for different types of basin modeling.

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