<?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>R.D. Markiewicz</dc:contributor>
  <dc:contributor>T.R. Rademacker</dc:contributor>
  <dc:contributor>R. Hopkins</dc:contributor>
  <dc:contributor>R.J. Rawcliffe</dc:contributor>
  <dc:contributor>J. Paquin</dc:contributor>
  <dc:creator>R. D. Miller</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Benefits of shallow water settings (0.1 to 0.5 m) are pronounced on shallow, high-resolution seismic reflection images and, for examples discussed here, range from an order of magnitude increased signal-to-noise ratio to resolution potential elevated by more than 8 times. Overall data quality of high-resolution seismic reflection data at three sites notorious for poor near-surface reflection returns was improved by coupling the source and/or receivers to a well sorted and fully saturated surface. Half-period trace-to-trace static offsets evident in reflections from receivers planted into a creek bank were eliminated by moving the geophones to the base of a shallow creek at the toe of the bank. Reflections from a dipping bedrock were recorded with a dominant frequency approaching 1 KHz from hydrophones in 0.5 m of water at the toe of a dam using a hammer impact source. A tamper impacted by a dead blow hammer in a shallow (10-20 cm) deep creek produced reflections with a dominant frequency over 400 Hz at depths as shallow as 6 ms. ?? 2007 Society of Exploration Geophysicists.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1190/1.2792615</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Advantages of wet work for near-surface seismic reflection</dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>