<?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>Richard F. Marvin</dc:contributor>
  <dc:contributor>John W. McGonigle</dc:contributor>
  <dc:contributor>David H. McIntyre</dc:contributor>
  <dc:contributor>Cleaves Lincoln Rogers</dc:contributor>
  <dc:creator>Dennis P. Cox</dc:creator>
  <dc:date>1977</dc:date>
  <dc:description>&lt;p&gt;Potassium-argon ages of hornblende, biotite, and whole rocks in Puerto Rico include the following: 126 m.y. for amphibolites in the southwest part of the island; 109 m.y. for the oldest known quartz diorite plutons; 88 to 65 m.y. for emplacement of various quartz diorite and granodiorite batholiths and stocks; 38 to 46 m.y. for intrusions of quartz diorite porphyry stocks and their hydrothermal alteration and mineralization. These intrusions are the youngest known igneous rocks in Puerto Rico. &lt;/p&gt;&lt;p&gt;In addition, a 35-m.y. age was determined for hornblende and biotite from the Virgin Gorda batholith. &lt;/p&gt;&lt;p&gt;Although widespread hydrothermal alteration as old as 75 m.y. is known in Puerto Rico, all important copper deposits are related to the 38- to 46-m.y. old intrusions.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Potassium-argon geochronology of some metamorphic, igneous, and hydrothermal events in Puerto Rico and the Virgin Islands</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>