Challenging the Paradigm "Missing Section = Normal Fault" and Implications for Hydrocarbon Exploration - An AAPG E-Symposium
(post-event materials available - asynchronous recording of original presentation)
- Jean-Yves Chatellier, Talisman Energy, Calgary, AB, Canada
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- Ongoing, self-paced course
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Recording of original webinar, packet of independent study reading materials, PDF of original PowerPoint presentation by FTP download. (Original presentation date: August 19, 2010.) Some materials will also sent by e-mail. Expanded package for CEU credit is $100 for AAPG members, and $145 for non-members. Special Student Pricing: $25 for Webinar only; $35 for Expanded package.
- 200 people
- 1.0 What is a CEU?
Who Should Attend
All geologists and geophysicists who work in structurally complex areas.
Upon successful completion of this course, you will be able to explain where, when, and how erroneous interpretations of normal faulting have been proposed when there are missing sections in the well data. Further, you will be able to evaluate wells that have missing sections and to propose, discuss, and evaluate possible explanations. You will also be able to explain examples and discuss case studies.
Overview and Key Concepts
In structurally complex areas, seismic interpretation can be misled by wrongly interpreted well data. A common approach in the oil industry can be summarized by the Spanish sentence “pozo mata sismica” which roughly interpreted means that well data trumps seismic and that data from a well must prevail in a seismic interpretation. A major problem arises when there is a missing section in the well information (logs, cuttings, or cores), and the reason for the missing section is incorrectly attributed to normal faulting.
This presentation will show where there are cases of missing sections, but none of them can be attributed to normal faulting. All field names in the presentation are from Venezuela if not otherwise specified.
The easiest recognizable misinterpretation occurs where wells have missing sections juxtaposed to wells with coeval massive sands; with enough well control additional support comes from recognizing the typical rhomboidal shaped blocks e.g. Dunlin Field - UK. Synsedimentary activity of horst blocks in the middle of major deposition centers (e.g. Brent delta) is responsible for such occurrences.
Many tools either alone or combined, can be used to diagnose problematic missing sections e.g. hydrocarbon column anomalies associated with fault plane mapping, abnormal RFT pressure trends, detailed fault throw map or perfectly identical TVDs depths of fault cuts in different stratigraphic units.
Unusual approaches can also be successful at recognizing misinterpreted normal faults as in the Lama Field: the TDs of every well that failed to reach their targeted depths were analyzed by plotting their coordinates in 3D. This revealed the existence of three previously unrecognized steeply dipping reverse faults that only one third of the wells had been able to penetrate; each of the latter showed missing sections where crossing these faults.
While 3-D seismic is the norm, 2-D lines can be invaluable in better defining the tectonic style of very complex areas. Large amount of hydrocarbon can be present below faults which have been obliquely reactivated and which appear at first glance to have the geometry of normal faults (e.g. Western Canada Foothills).
Implications for the examples cited above range from redesign of water injection wells for pressure support (Lama Field), to major bypassed pay zone (Santa Barbara Field), change in reserve estimates (Dunlin) and finally to a new hydrocarbon discovery (near Bosque Field).
(This presentation is based on a paper co-authored by Maria Eugenia Rueda, StatoilHydro, Stavanger, Norway, and presented as a poster session at AAPG Annual Convention and Exhibition, New Orleans)
NOTE: The one hour live portion will be followed by a full day of independent study (not a live event). The one-hour live e-symposium can be accessed from any computer anywhere in the world using a high-speed internet connection. After the event is over, you will receive via email information about accessing the asynchronous segment (not live) which consists of your independent study materials, to be accessed and studied at any time. You will be able to email responses to the readings, along with your study question answers for CEU credit (if you sign up for the extended package).