<?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>C.B. Raleigh</dc:contributor>
  <dc:creator>W.H.K. Lee</dc:creator>
  <dc:date>1969</dc:date>
  <dc:description>&lt;div id="Abs1-section" class="c-article-section"&gt;&lt;div id="Abs1-content" class="c-article-section__content"&gt;&lt;p&gt;THE peninsular shield of India has long been regarded as a stable region. The area had not been subject to orogenic deformation since the Pre-Cambrian, although a vast area (5 × 10&lt;sup&gt;5&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;square km) was flooded by basalts during Late Cretaceous to the Eocene—the Deccan Trap. Several years ago, a small dam was built across the Koyna river, some 200 km south-east of Bombay (Fig. 1). The dam reservoir filled in stages, beginning with the monsoon of 1962, and reached a capacity of 2 × 10&lt;sup&gt;9&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;m&lt;sup&gt;3&lt;/sup&gt;&lt;span&gt;&amp;nbsp;&lt;/span&gt;and a maximum depth of about 70 m&lt;sup&gt;1&lt;/sup&gt;.&lt;/p&gt;&lt;/div&gt;&lt;/div&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1038/223172a0</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>Nature</dc:publisher>
  <dc:title>Fault-plane Solution of the Koyna (India) Earthquake</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>