<?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>Christopher D. Henry</dc:contributor>
  <dc:contributor>David A. John</dc:contributor>
  <dc:creator>Joseph P. Colgan</dc:creator>
  <dc:date>2011</dc:date>
  <dc:description>&lt;p&gt;The Eocene (34 Ma) Caetano caldera in north-central 
Nevada offers an exceptional opportunity to study the 
physical and petrogenetic evolution of a large (20 km by 
10–18 km pre-extensional dimensions) silicic magma 
chamber, from precursor magmatism to caldera collapse 
and intrusion of resurgent plutons. Caldera-related rocks 
shown on this map include two units of crystal-rich 
intracaldera tuff totaling over 4 km thickness, caldera 
collapse breccias, tuff dikes that fed the eruption, 
hydrothermally altered post-eruption rocks, and two 
generations of resurgent granitic intrusions (John et al., 
2008). The map also depicts middle Miocene (about 16–12 
Ma) normal faults and synextensional basins that 
accommodated &gt;100 percent extension and tilted the 
caldera into a series of ~40° east-dipping blocks, 
producing exceptional 3-D exposures of the caldera 
interior (Colgan et al., 2008). &lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;This 1:75,000-scale map is a compilation of published 
maps and extensive new mapping by the authors (fig. 1), 
and supersedes a preliminary 1:100,000-scale map 
published by Colgan et al. (2008) and John et al. (2008). 
New mapping focused on the margins of the Caetano 
caldera, the distribution and lithology of rocks within the 
caldera, and on the Miocene normal faults and sedimentary 
basins that record Neogene extensional faulting. The 
definition of geologic units and their distribution within 
the caldera is based entirely on new mapping, except in the 
northern Toiyabe Range, where mapping by Gilluly and 
Gates (1965) was modified with new field observations. 
The distribution of pre-Cenozoic rocks outside the caldera 
was largely compiled from existing sources with minor 
modifications, with the exception of the northeastern 
caldera margin (west of the Cortez Hills Mine), which was 
remapped in the course of this work and published as a 
stand-alone 1:6000-scale map (Moore and Henry, 2010).&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Nevada Bureau of Mines and Geology</dc:publisher>
  <dc:title>Geologic map of the Caetano caldera, Lander and Eureka counties, Nevada</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>