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<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>Krishan Chopra</dc:contributor>
  <dc:contributor>Ashutosh Bhardwaj</dc:contributor>
  <dc:contributor>Ray Boswell</dc:contributor>
  <dc:contributor>William F. Waite</dc:contributor>
  <dc:contributor>A. K. Misra</dc:contributor>
  <dc:contributor>Pushpendra Kumar</dc:contributor>
  <dc:contributor>Jurgen Mienert</dc:contributor>
  <dc:contributor>Christian Berndt</dc:contributor>
  <dc:contributor>Anne M. Trehu</dc:contributor>
  <dc:contributor>Angelo Camerlenghi</dc:contributor>
  <dc:contributor>Char-Shine Liu</dc:contributor>
  <dc:creator>Timothy S. Collett</dc:creator>
  <dc:date>2022</dc:date>
  <dc:description>&lt;p id="Par1" class="Para"&gt;The analysis of 3-D seismic data has become one of the most powerful ways to identify sand-rich gas hydrate reservoir systems and to directly identify highly concentrated gas hydrate prospects. Scientific drilling programs have shown that the occurrence of highly concentrated gas hydrate accumulations in coarse-grained, sand-rich, reservoir systems has a significant impact on the physical properties of sediments, allowing gas hydrates to be “directly detected” by conventional seismic analysis techniques. One of the most diagnostic responses of a gas hydrate-bearing sand reservoir is that of a high-velocity sedimentary section and an associated high-amplitude seismic response with a reflection polarity matching that of the seafloor. Knowledge of this physical relationship guided the Indian National Gas Hydrate Program Expedition 02 (NGHP-02) in their pre-drill site review and selection effort along the eastern continental margin of India in 2016. Within the planning, operational and post-operational data analysis phases of the NGHP-02 Expedition, scientists relied heavily on the analyses of the (1) pre-expedition acquired 3-D seismic data from offshore India, (2) downhole logging data acquired during NGHP-02 and (3) core samples and data obtained from NGHP-02 conventional- and pressure-cores to identify gas hydrates and assess the geologic controls on the formation and stability of these accumulations. Data analysis has confirmed the presence of extensive sand-rich depositional systems throughout the deepwater portions of the Krishna-Godavari and Mahanadi Basins in the Bay of Bengal. Two areas of the Krishna-Godavari Basin contain substantial gas hydrate accumulations in sand-rich systems, representing candidate sites for future potential energy exploitation.&lt;/p&gt;&lt;div id="cobranding-and-download-availability-text" class="note test-pdf-link"&gt;&lt;br&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/978-3-030-81186-0_11</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Springer</dc:publisher>
  <dc:title>A review of the exploration, discovery, and characterization of highly concentrated gas hydrate accumulations in coarse-grained reservoir systems along the Eastern Continental Margin of India</dc:title>
  <dc:type>chapter</dc:type>
</oai_dc:dc>