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        <identifier>oai:www.ideals.illinois.edu:2142/86522</identifier>
        <datestamp>2023-07-11</datestamp>
        <setSpec>col_2142_5131</setSpec>
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        <thesis xmlns="http://www.ndltd.org/standards/metadata/etdms/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.ndltd.org/standards/metadata/etdms/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdms11.xsd http://purl.org/dc/elements/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdmsdc.xsd">
          <dc:contributor>Marshak, Stephen</dc:contributor>
          <dc:creator>Harrison, Michael Joseph</dc:creator>
          <dc:date>2015-09-28T15:12:27Z</dc:date>
          <dc:date>2015-09-28T15:12:27Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>2002</dc:date>
          <dc:date>2002</dc:date>
          <dc:description>Mapping of the Pittston quadrangle in the central domain and structural analysis elsewhere in the synclinorium reveal that mesoscopic faults, folds, and cleavage throughout the synclinorium trend &amp;sim;075&amp;deg;; thus, these structures parallel the southern domain, but trend at high angles to the northern domain. Many of these structures are better developed in the hanging wall of a regional detachment than in the footwall. Crosscutting structures (e.g., cleavage, faults) indicate that the shortening direction rotated &amp;sim;45&amp;deg; clockwise during the Alleghanian orogeny. Heat-flow calculations suggest that the migration of hot (&amp;sim;270&amp;deg;C) brines could have induced anthracitization at shallow depths (&amp;le;5 km) in the synclinorium; thus, deep burial (6--9 km) by post-Pennsylvanian strata was not required for anthracitization. Field observations, fluid-inclusion studies, and illite-crystallinity analysis suggest that Alleghanian fluid flow was stratigraphically controlled.</dc:description>
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  Previous issue date: 2002</dc:description>
          <dc:description>Embargo set by: Seth Robbins for item 87803
Lift date: Forever
Reason: Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs</dc:description>
          <dc:description>Restricted to the U of I community idenfinitely during batch ingest of legacy ETDs</dc:description>
          <dc:description>U of I Only</dc:description>
          <dc:description>168 p.</dc:description>
          <dc:description>Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 2002.</dc:description>
          <dc:identifier>http://hdl.handle.net/2142/86522</dc:identifier>
          <dc:identifier>(MiAaPQ)AAI3070319</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:subject>Geology</dc:subject>
          <dc:title>Origin, Architecture, and Thermal State of the Lackawanna Synclinorium, Pennsylvania: Implications for Tectonic Evolution of the Central Appalachians</dc:title>
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            <department>Geology</department>
            <discipline>Geology</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Dissertation</level>
            <name>Ph.D.</name>
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