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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
Magnitude
Resulting from the Main Generating Mechanisms
from:
Chapter 1
Comparision of Overpressure Magnitude
Resulting from the Main Generating Mechanisms
Richard E. Swarbrick
University of Durham
Durham, England
Mark J. Osborne
University of Durham
Durham, England
BP Exploration
Sunbury on Thames, England
Gareth S. Yardley
Heriot-Watt University
Edinburgh, Scotland
ABSTRACT
magnitude
overpressure from stress are a high sedimentation (loading) rate and/or strong lateral compressive
forces. A high sedimentation rate, as a means to create rapid increase in temperature, also favors high-
magnitude
overpressure from fluid expansion mechanisms. An alternative method to achieve a rapid
increase in temperature is a thermal pulse associated with tectonic or magmatic processes.
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