Difference between revisions of "Using conventional well logs to estimate richness"

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==Limestone response example==
 
==Limestone response example==
  
[[file:evaluating-source-rocks_fig6-3.png|300px|thumb|{{figure number|2}}From Meyer and Nederlof.<ref name=Meyerandnederlof_1984 />]]
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[[file:evaluating-source-rocks_fig6-3.png|300px|thumb|{{figure number|2}}Composite log of the Upper Jurassic Hanifa limestone in the Middle East. From Meyer and Nederlof.<ref name=Meyerandnederlof_1984 />]]
  
 
The composite log in [[:file:evaluating-source-rocks_fig6-3.png|Figure 2]] of the Upper Jurassic Hanifa limestone in the Middle East displays a typical response of organic matter in a limestone section. No shale is present in this interval. Note the high gamma ray and resistivity readings. Core analysis of this well indicates the source rock (indicated by dots with dashes through them) is mature and generating oil.
 
The composite log in [[:file:evaluating-source-rocks_fig6-3.png|Figure 2]] of the Upper Jurassic Hanifa limestone in the Middle East displays a typical response of organic matter in a limestone section. No shale is present in this interval. Note the high gamma ray and resistivity readings. Core analysis of this well indicates the source rock (indicated by dots with dashes through them) is mature and generating oil.

Revision as of 13:20, 18 September 2014

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Critical elements of the petroleum system
Chapter Evaluating source rocks
Author Carol A. Law
Link Web page
Store AAPG Store

Conventional well logs are useful for estimating source rock richness both qualitatively and quantitatively. Well logs allow a qualitative identification of organic-rich formations and a quantitative analysis of the amount of organic matter. The advantages of using well logs over cuttings are continuous sampling, more accurate depth control, and greater vertical resolution.[1]

Using well logs

The use of conventional well logs to predict organic richness of a unit of rock requires calibrating well log intervals to samples measured for total organic carbon (TOC) using pyrolysis or another suitable measurement technique. Using the calibrated logs, we can extrapolate TOC values to uncalibrated logs to estimate source rock richness over large areas.

Note: Consider changes in depositional environment and maturity when applying these techniques.

Effects of organic matter on well logs

The increasing concentration of organic matter in a rock directly affects its properties by lowering density slowing sonic velocity increasing radioactivity raising resistivity and raising hydrogen and carbon contents. All of these attributes can be measured using density sonic, neutron, gamma ray, and resistivity logs. The table below (from [1]) summarizes log responses to organic matter.

Log/Property Response/Value for Organic Matter (OM) Comments
Gamma ray (GR) or uranium (U) High High GR caused by U; can be linear with OM; U not always present
Density Low (approx. 1 g/cm3 ) Similar to pore fluids
Neutron High Due to hydrogen in OM
Sonic High transit time Estimates vary from 150 to more than 200 μsec/ft
Resistivity High May not affect log response unless generated hydrocarbons occupy pores
Pulsed neutron High carbon-oxygen ratio Most direct measurement of carbon; needs inorganic correction

Shale response example

Figure 1 Composite log of Kimmeridge shale, North Sea. From Meyer and Nederlof.[2]

In Figure 1, the composite log of Kimmeridge shale, North Sea is a typical log response to a high concentration of organic matter in a shale section. The underlying Heather Formation is very silty. The source rock interval is indicated by dots with dashes through them. Note the high sonic and gamma ray readings and the low density readings. The resistivity log reads only slightly higher than the overlying shale section.

Limestone response example

Figure 2 Composite log of the Upper Jurassic Hanifa limestone in the Middle East. From Meyer and Nederlof.[2]

The composite log in Figure 2 of the Upper Jurassic Hanifa limestone in the Middle East displays a typical response of organic matter in a limestone section. No shale is present in this interval. Note the high gamma ray and resistivity readings. Core analysis of this well indicates the source rock (indicated by dots with dashes through them) is mature and generating oil.

Limitations

Well-log signals are recorded for an interval thickness, which varies depending on the type of logging tool. Averaged values may not give a true picture of the richness of the source rock.

See also

References

  1. 1.0 1.1 Herron, S., L., 1991, In situ evaluation of potential source rocks by wireline logs, in Merrill, R., K., ed., Source and Migration Processes and Evaluation Techniques: AAPG Treatise of Petroleum Geology, Handbook of Petroleum Geology No. 1, p. 127–134.
  2. 2.0 2.1 Meyer, B. L., and M. H. Nederlof, 1984, Identification of source rocks on wireline logs by density/resistivity and sonic transit time/resistivity crossplots: AAPG Bulletin, v. 68, no. 2, p. 121-129. Discusses the principles and application of well log analysis to identify source rocks.

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