<?xml version="1.0" encoding="UTF-8"?>
<rss xmlns:taxo="http://purl.org/rss/1.0/modules/taxonomy/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/" version="2.0">
  <channel>
    <title>DSpace collection: GEO Graduate Student Conference Papers</title>
    <link>http://hdl.handle.net/10057/479</link>
    <description />
    <textInput>
      <title>The collection's search engine</title>
      <description>Search the Channel</description>
      <name>s</name>
      <link>http://soar.wichita.edu:8080/dspace/simple-search</link>
    </textInput>
    <item>
      <title>Reservoir characterization of microbial reef reservoirs at Little Cedar Creek Field, Conecuh County, Alabama</title>
      <link>http://hdl.handle.net/10057/1357</link>
      <description>title: Reservoir characterization of microbial reef reservoirs at Little Cedar Creek Field, Conecuh County, Alabama authors: Koralegadara, Ganaganath; Parcell, William C.
&lt;br&gt;abstract: Little Cedar Creek Field (LCCF) in Conecuh County, Alabama is the largest Smackover field discovered in the&#xD;
northern U.S. Gulf Coast in the last three decades. It is now the most productive field in the State of Alabama. The LCCF&#xD;
gives an opportunity to identify the characteristics of microbial (thrombolite) developments in shallow water deposits and&#xD;
differentiate it from the nearby reef reservoirs which grow directly on Paleozoic basement paleohighs. Previous studies from&#xD;
this area have indicated that Jurassic microbial buildups are associated with Paleozoic basement paleohighs. In contrast,&#xD;
microbial buildups at LCCF apparently developed in shallow subtidal environment without the influence of basement&#xD;
rockgrounds.&#xD;
The objective of this project is to examine the microbial reef reservoirs at Little Cedar Creek in order to identify any&#xD;
relationship between depositional fabric type and reservoir quality distribution. Furthermore this study compares these&#xD;
nearshore thrombolite facies to microbial fabric types identified at Appleton and Vocation fields, Alabama and will focus on&#xD;
the types of Jurassic microbial developments in this field and the poor reservoir rock fabric types identified in other fields&#xD;
and characterized as lagoon, and subtidal facies.&#xD;
This study will improve the understanding of Upper Jurassic Smackover microbial development, its lithologic&#xD;
fabrics and controls on reservoir quality. The results will improve the exploration strategy to find other stratigraphic&#xD;
microbial carbonate reservoirs worldwide. Examining the controls on reservoir quality distribution at LCCF will provide&#xD;
new insights into this unique and prolific petroleum reservoir facies
&lt;br&gt;description: Paper presented to the 4th Annual Symposium on Graduate Research and Scholarly Projects (GRASP) held at the Hughes Metropolitan Complex, Wichita State University, April 25, 2008.
&lt;br&gt;</description>
      <pubDate>Thu, 24 Apr 2008 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>300-million-year-old soils and their implications on predicting ancient climate conditions</title>
      <link>http://hdl.handle.net/10057/469</link>
      <description>title: 300-million-year-old soils and their implications on predicting ancient climate conditions authors: Turner-Williams, Monica M.; Yang, Wan
&lt;br&gt;description: Paper presented to the 1st Annual Symposium on Graduate Research and Scholarly Projects (GRASP) held at the Hughes Metropolitan Complex, Wichita State University, April 22, 2005.
&lt;br&gt;</description>
      <pubDate>Thu, 21 Apr 2005 22:58:59 GMT</pubDate>
    </item>
  </channel>
</rss>

