<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>J.C. Pashin</dc:contributor>
  <dc:contributor>B. Chai</dc:contributor>
  <dc:contributor>R.D. Schneeflock</dc:contributor>
  <dc:creator>R.H. Groshong Jr.</dc:creator>
  <dc:date>2003</dc:date>
  <dc:description>A reservoir that appears to lack faults at one scale of resolution or at one sampling density may nevertheless contain faults that are below the resolution of the observations. The area-depth relationship from a balanced cross-section is shown to contain the necessary information for predicting the sub-resolution fault heave. Existing area-depth theory is extended to include growth units, allowing structural length and thickness changes to be separated from the depositional changes. The technique is validated with a numerical model of a growth full graben and a sand-box model of a half graben; then field tested in the Gilbertown graben, a growth structure within the regional peripheral fault trend along the northern margin of the Gulf of Mexico. A cross-section developed from wells alone is used to infer the abundance of sub-resolution faults by the area-balance technique. A small but significant amount of sub-resolution extension is predicted and then confirmed with a high-resolution seismic line. ?? 2003 Elsevier Science Ltd. All rights reserved.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1016/S0191-8141(03)00002-6</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Predicting reservoir-scale faults with area balance: Application to growth stratigraphy</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>