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                  <text>(PH) Powderhorn (Iron Hill) Carbonatite Suite -- Gunnison County, SW Colorado</text>
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                  <text>The Powderhorn (Iron Hill) Carbonatite is located in Gunnison County in about the center of the southwestern quadrant of Colorado. It is a pear-shaped body which is essentially conical at depth, and is exposed over an area of about 12 square miles. The carbonatite body covers about 2 and a half square miles; About 70 percent of the in pyroxenite which was subsequently intruded by or replaced by nepheline and melilite-bearing rocks; magnetite-perovskite, and carbonatite.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Mitchell, R.H., 2014, Primary and secondary niobium mineral deposits associated with carbonatites:Â Ore Geology Reviews,Â v. 64, p.Â 626-641,Â doi:10.1016/j.oregeorev.2014.03.010. &lt;a title="Full Article." href="http://dx.doi.org/10.1016/j.oregeorev.2014.03.010"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Focuses specifically on the formation of niobium in carbonatites but includes an excellent baseline description of carbonatites.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Nash, W.P., 1972, Mineralogy and Petrology of the Iron HillÂ &lt;span class="search-result-highlight"&gt;Carbonatite&lt;/span&gt;Â Complex, Colorado: Geological Society of America Bulletin, &lt;span class="cit-vol"&gt;&lt;span class="cit-sep cit-sep-before-article-vol"&gt;v.Â &lt;/span&gt;83&lt;span class="cit-sep cit-sep-after-article-vol"&gt;, p.Â &lt;/span&gt;&lt;/span&gt;&lt;span class="cit-pages"&gt;&lt;span class="cit-first-page"&gt;1361&lt;/span&gt;&lt;span class="cit-sep"&gt;-&lt;/span&gt;&lt;span class="cit-last-page"&gt;1382&lt;/span&gt;&lt;/span&gt;, doi:Â 10.1130/0016-7606(1972)83[1361:MAPOTI]2.0.CO;2. &lt;a title="Full Article." href="http://dx.doi.org/10.1130/0016-7606(1972)83%5B1361:MAPOTI%5D2.0.CO;2"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Bulk rock chemistry description &amp;amp; maps/diagrams showing the location of rocks in the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;
Temple, R.K., Grogran, R.M.,Â &lt;span&gt;1965, C&lt;span&gt;arbonatite and related alkalic rocks at powder horn, Colorado:Â &lt;span&gt;Economic geology and the bulletin of the Society of Economic Geologists, v. 60, p.Â &lt;span&gt;672-692, doi:Â 10.2113/gsecongeo.60.4.672. &lt;a title="Full Article" href="http://dx.doi.org/10.2113/gsecongeo.60.4.672."&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Basic information regarding the structure, geochemistry, and petrogenesis of the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Van Gosen, B. S., Lowers, H. A., 2007, Iron Hill (Powderhorn)Â carbonatiteÂ complex, Gunnison County, CO; a potential source of several uncommon mineral resources: Mining Engineering, v. 59, p. 56-62, doi: N/AÂ &lt;a title="Abstract" href="http://me.smenet.org/abstract.cfm?articleID=1143&amp;amp;page=56"&gt;Abstract.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Mineral resource potential: titanium, iron, vermiculite, vanadium, and nephaline.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Olson, J.C., Hedland, D.C., &lt;span&gt;1981&lt;/span&gt;, &lt;span&gt;Alkalic rocks and resources of thorium and associated elements in the Powderhorn District, Gunnison County, Colorado&lt;/span&gt;: &lt;span&gt;USGS Numbered Series&lt;/span&gt;, Professional Paper , v. &lt;span&gt;1049, &lt;span&gt;p. C1-C34&lt;/span&gt;Â &lt;/span&gt;Â doi: N/A. &lt;a title="Full Article" href="http://pubs.usgs.gov/pp/1049c/report.pdf"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Extensive report by the USGS regarding rock type and history of formation (geologic ages).&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/show/33"&gt;Powderhorn Carbonatite Minerals Supplementary Information&lt;/a&gt;</text>
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                  <text>(PH) Powderhorn (Iron Hill) Carbonatite Suite -- Gunnison County, SW Colorado</text>
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                  <text>The Powderhorn (Iron Hill) Carbonatite is located in Gunnison County in about the center of the southwestern quadrant of Colorado. It is a pear-shaped body which is essentially conical at depth, and is exposed over an area of about 12 square miles. The carbonatite body covers about 2 and a half square miles; About 70 percent of the in pyroxenite which was subsequently intruded by or replaced by nepheline and melilite-bearing rocks; magnetite-perovskite, and carbonatite.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Mitchell, R.H., 2014, Primary and secondary niobium mineral deposits associated with carbonatites:Â Ore Geology Reviews,Â v. 64, p.Â 626-641,Â doi:10.1016/j.oregeorev.2014.03.010. &lt;a title="Full Article." href="http://dx.doi.org/10.1016/j.oregeorev.2014.03.010"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Focuses specifically on the formation of niobium in carbonatites but includes an excellent baseline description of carbonatites.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Nash, W.P., 1972, Mineralogy and Petrology of the Iron HillÂ &lt;span class="search-result-highlight"&gt;Carbonatite&lt;/span&gt;Â Complex, Colorado: Geological Society of America Bulletin, &lt;span class="cit-vol"&gt;&lt;span class="cit-sep cit-sep-before-article-vol"&gt;v.Â &lt;/span&gt;83&lt;span class="cit-sep cit-sep-after-article-vol"&gt;, p.Â &lt;/span&gt;&lt;/span&gt;&lt;span class="cit-pages"&gt;&lt;span class="cit-first-page"&gt;1361&lt;/span&gt;&lt;span class="cit-sep"&gt;-&lt;/span&gt;&lt;span class="cit-last-page"&gt;1382&lt;/span&gt;&lt;/span&gt;, doi:Â 10.1130/0016-7606(1972)83[1361:MAPOTI]2.0.CO;2. &lt;a title="Full Article." href="http://dx.doi.org/10.1130/0016-7606(1972)83%5B1361:MAPOTI%5D2.0.CO;2"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Bulk rock chemistry description &amp;amp; maps/diagrams showing the location of rocks in the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;
Temple, R.K., Grogran, R.M.,Â &lt;span&gt;1965, C&lt;span&gt;arbonatite and related alkalic rocks at powder horn, Colorado:Â &lt;span&gt;Economic geology and the bulletin of the Society of Economic Geologists, v. 60, p.Â &lt;span&gt;672-692, doi:Â 10.2113/gsecongeo.60.4.672. &lt;a title="Full Article" href="http://dx.doi.org/10.2113/gsecongeo.60.4.672."&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Basic information regarding the structure, geochemistry, and petrogenesis of the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Van Gosen, B. S., Lowers, H. A., 2007, Iron Hill (Powderhorn)Â carbonatiteÂ complex, Gunnison County, CO; a potential source of several uncommon mineral resources: Mining Engineering, v. 59, p. 56-62, doi: N/AÂ &lt;a title="Abstract" href="http://me.smenet.org/abstract.cfm?articleID=1143&amp;amp;page=56"&gt;Abstract.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Mineral resource potential: titanium, iron, vermiculite, vanadium, and nephaline.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Olson, J.C., Hedland, D.C., &lt;span&gt;1981&lt;/span&gt;, &lt;span&gt;Alkalic rocks and resources of thorium and associated elements in the Powderhorn District, Gunnison County, Colorado&lt;/span&gt;: &lt;span&gt;USGS Numbered Series&lt;/span&gt;, Professional Paper , v. &lt;span&gt;1049, &lt;span&gt;p. C1-C34&lt;/span&gt;Â &lt;/span&gt;Â doi: N/A. &lt;a title="Full Article" href="http://pubs.usgs.gov/pp/1049c/report.pdf"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Extensive report by the USGS regarding rock type and history of formation (geologic ages).&lt;/li&gt;
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&#13;
Coarse grained pyroxenite showing heavy traces of oxidation on every weathered face of the rock. Large clusters (5-8 mm) of biotite appear throughout the rock.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Mitchell, R.H., 2014, Primary and secondary niobium mineral deposits associated with carbonatites:Â Ore Geology Reviews,Â v. 64, p.Â 626-641,Â doi:10.1016/j.oregeorev.2014.03.010. &lt;a title="Full Article." href="http://dx.doi.org/10.1016/j.oregeorev.2014.03.010"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Focuses specifically on the formation of niobium in carbonatites but includes an excellent baseline description of carbonatites.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;Nash, W.P., 1972, Mineralogy and Petrology of the Iron HillÂ &lt;span class="search-result-highlight"&gt;Carbonatite&lt;/span&gt;Â Complex, Colorado: Geological Society of America Bulletin, &lt;span class="cit-vol"&gt;&lt;span class="cit-sep cit-sep-before-article-vol"&gt;v.Â &lt;/span&gt;83&lt;span class="cit-sep cit-sep-after-article-vol"&gt;, p.Â &lt;/span&gt;&lt;/span&gt;&lt;span class="cit-pages"&gt;&lt;span class="cit-first-page"&gt;1361&lt;/span&gt;&lt;span class="cit-sep"&gt;-&lt;/span&gt;&lt;span class="cit-last-page"&gt;1382&lt;/span&gt;&lt;/span&gt;, doi:Â 10.1130/0016-7606(1972)83[1361:MAPOTI]2.0.CO;2. &lt;a title="Full Article." href="http://dx.doi.org/10.1130/0016-7606(1972)83%5B1361:MAPOTI%5D2.0.CO;2"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Bulk rock chemistry description &amp;amp; maps/diagrams showing the location of rocks in the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;
Temple, R.K., Grogran, R.M.,Â &lt;span&gt;1965, C&lt;span&gt;arbonatite and related alkalic rocks at powder horn, Colorado:Â &lt;span&gt;Economic geology and the bulletin of the Society of Economic Geologists, v. 60, p.Â &lt;span&gt;672-692, doi:Â 10.2113/gsecongeo.60.4.672. &lt;a title="Full Article" href="http://dx.doi.org/10.2113/gsecongeo.60.4.672."&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
&lt;ul&gt;&lt;li&gt;Basic information regarding the structure, geochemistry, and petrogenesis of the Powderhorn Carbonatite.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Van Gosen, B. S., Lowers, H. A., 2007, Iron Hill (Powderhorn)Â carbonatiteÂ complex, Gunnison County, CO; a potential source of several uncommon mineral resources: Mining Engineering, v. 59, p. 56-62, doi: N/AÂ &lt;a title="Abstract" href="http://me.smenet.org/abstract.cfm?articleID=1143&amp;amp;page=56"&gt;Abstract.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Mineral resource potential: titanium, iron, vermiculite, vanadium, and nephaline.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Olson, J.C., Hedland, D.C., &lt;span&gt;1981&lt;/span&gt;, &lt;span&gt;Alkalic rocks and resources of thorium and associated elements in the Powderhorn District, Gunnison County, Colorado&lt;/span&gt;: &lt;span&gt;USGS Numbered Series&lt;/span&gt;, Professional Paper , v. &lt;span&gt;1049, &lt;span&gt;p. C1-C34&lt;/span&gt;Â &lt;/span&gt;Â doi: N/A. &lt;a title="Full Article" href="http://pubs.usgs.gov/pp/1049c/report.pdf"&gt;Full Article.&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Extensive report by the USGS regarding rock type and history of formation (geologic ages).&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/show/33"&gt;Powderhorn Carbonatite Minerals Supplementary Information&lt;/a&gt;</text>
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&#13;
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                  <text>The Tanzawa Mountains in Japan were created in an arc-arc collision, when the Izu-Bonin-Mariana Arc was subducted beneath the Honshu Arc. This eventually  accreted into the Tanzawa Mountains.  The samples in this collection were found in and around the Tanzawa Mountains.  The suite includes hornfels, amphibolites, quartz diorite, granophyres, and other basaltic rocks.  The samples range from fine to coarse grained.  An interesting feature found on many of the samples was a flow-like swirl of minerals in the thin section, visible in XPL.  The quartz diorite  samples had crystalline, powdery substances on them, which were analyzed using a Scanning Electron Microscope (SEM). The chemical compositions of the mentioned powdery substances were calcium, aluminum, silicon, and oxygen. </text>
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                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Kawate, S., and Makoto, A., 1998, Petrogenesis of the Tanzawa plutonic complex, central Japan; exposed felsic middle crust of the Izu-Bonin-Mariana Arc: Island Arc, v. 7, p. 342-358, &lt;br /&gt;link: http://dx.doi.org/10.1111/j.1440-1738.1998.00194.x.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper explains the chemical variation and high SiO&lt;sub&gt;2Â &lt;/sub&gt;percentage of rocks within Tanzawa region, and describes in some depth the tectonic events that uplifted the Tanzawa Mountains. Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Kitamura, K., Ishikawa, M., and Arima, M., 2003, Petrological model of the northern Izu-Bonin-Mariana Arc crust; constraints from high-pressure measurements of elastic wave velocities of the Tanzawa plutonic rocks, central Japan: Tectonophysics, v. 371, p.213-221,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1016/S0040-1951(03)00229-4&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper researchs the variations in acoustic impedance between different hornblende-gabbroic rocks from Tanzawa, Japan.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Mikami, K., 1953, Metamorphic rocks in the southeastern margin of the Tanzawa quartz-diorite mass: Science Reports of Yokohama National University, v. 2, p. 34-49&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper studies the chemical analysis of amphibolites resulting from contact metamorphism of the quartz-diorite mass in the Tanzawa Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Tani, K., Dunkley, D. J., Kimura, J., Wysoczanski, R.J., Yamada, K., and Tatsumi, Y.,2010,Â Syncollisional rapid granitic magma formation in an arc-arc collision zone: Evidence from the Tanzawa plutonic complex, Japan:Â Geology [Boulder], v. 38, p.215-218,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1130/G30526.1&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper discusses the collison that exposed the gabbroic rocks of the Tanzawa plutonic complex, and overall gives the reader an in-depth sturctural history of the Tanzawa Mountains.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Yoshimura, T., 1997, Ca-Al silicates in low-grade metavolcanic rocks from southern Tanzawa Mountains, Central Japan: Journal of Mineralogy Petrology and Economic Geology, Â v. 92, p. 363-378, &lt;br /&gt;link: http://dx.doi.org/10.2465/ganko.92.363.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper explains prevalence of greenschist facies within the Tanzawa Mountain region, and gives the mineral composition of rocks from southern region of Tanzawa Mountains.&lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;&lt;br /&gt;&lt;br /&gt;&lt;/p&gt;</text>
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                  <text>The samples were found in the Tanzawa Mountains of Kanto, Japan. &#13;
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                  <text>The Tanzawa Mountains were formed during the late Pliocene. </text>
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                <text>Rock Sample:&#13;
The sample has black to green phenocrysts with a greenish white matrix.  It has phaneritic grains with a aphanetic matrix.  Phenocrysts are coarse to fined grained ranging from 0.1~1cm in size.  There is a chalk like powder on the outside of the sample (white).  There are deep fractures running to the center of the sample.  It is likely that the  sample underwent chemical weathering by oxidation.  The chemical weathering is evident due to the orange brown tint.  Overall the sample has a smooth weathered outside with rough gritty inside.&#13;
&#13;
Thin Section:&#13;
Minerals are either medium in size.  All the minerals seem to have intergrown in the quartz crystals.&#13;
-Quartz (50%)&#13;
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/10"&gt;Tanzawa Mountains--Metamorphic Suite, Japan&lt;/a&gt;</text>
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                <text>Tanzawa Mountains, Japan  South of North Contact</text>
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                <text>Purchased from Western Minerals Inc.</text>
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                  <text>(TMJ) Quartz-rich Metamorphic Suite -- Tanzawa Mountains, Kanto, Japan</text>
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                  <text>The Tanzawa Mountains in Japan were created in an arc-arc collision, when the Izu-Bonin-Mariana Arc was subducted beneath the Honshu Arc. This eventually  accreted into the Tanzawa Mountains.  The samples in this collection were found in and around the Tanzawa Mountains.  The suite includes hornfels, amphibolites, quartz diorite, granophyres, and other basaltic rocks.  The samples range from fine to coarse grained.  An interesting feature found on many of the samples was a flow-like swirl of minerals in the thin section, visible in XPL.  The quartz diorite  samples had crystalline, powdery substances on them, which were analyzed using a Scanning Electron Microscope (SEM). The chemical compositions of the mentioned powdery substances were calcium, aluminum, silicon, and oxygen. </text>
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              <name>Contributor</name>
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                <elementText elementTextId="17776">
                  <text>Western Minerals, Inc.</text>
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              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
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                <elementText elementTextId="17996">
                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Kawate, S., and Makoto, A., 1998, Petrogenesis of the Tanzawa plutonic complex, central Japan; exposed felsic middle crust of the Izu-Bonin-Mariana Arc: Island Arc, v. 7, p. 342-358, &lt;br /&gt;link: http://dx.doi.org/10.1111/j.1440-1738.1998.00194.x.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper explains the chemical variation and high SiO&lt;sub&gt;2Â &lt;/sub&gt;percentage of rocks within Tanzawa region, and describes in some depth the tectonic events that uplifted the Tanzawa Mountains. Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Kitamura, K., Ishikawa, M., and Arima, M., 2003, Petrological model of the northern Izu-Bonin-Mariana Arc crust; constraints from high-pressure measurements of elastic wave velocities of the Tanzawa plutonic rocks, central Japan: Tectonophysics, v. 371, p.213-221,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1016/S0040-1951(03)00229-4&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper researchs the variations in acoustic impedance between different hornblende-gabbroic rocks from Tanzawa, Japan.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Mikami, K., 1953, Metamorphic rocks in the southeastern margin of the Tanzawa quartz-diorite mass: Science Reports of Yokohama National University, v. 2, p. 34-49&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper studies the chemical analysis of amphibolites resulting from contact metamorphism of the quartz-diorite mass in the Tanzawa Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Tani, K., Dunkley, D. J., Kimura, J., Wysoczanski, R.J., Yamada, K., and Tatsumi, Y.,2010,Â Syncollisional rapid granitic magma formation in an arc-arc collision zone: Evidence from the Tanzawa plutonic complex, Japan:Â Geology [Boulder], v. 38, p.215-218,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1130/G30526.1&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper discusses the collison that exposed the gabbroic rocks of the Tanzawa plutonic complex, and overall gives the reader an in-depth sturctural history of the Tanzawa Mountains.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Yoshimura, T., 1997, Ca-Al silicates in low-grade metavolcanic rocks from southern Tanzawa Mountains, Central Japan: Journal of Mineralogy Petrology and Economic Geology, Â v. 92, p. 363-378, &lt;br /&gt;link: http://dx.doi.org/10.2465/ganko.92.363.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper explains prevalence of greenschist facies within the Tanzawa Mountain region, and gives the mineral composition of rocks from southern region of Tanzawa Mountains.&lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;&lt;br /&gt;&lt;br /&gt;&lt;/p&gt;</text>
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                  <text>The samples were found in the Tanzawa Mountains of Kanto, Japan. &#13;
</text>
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              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
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                  <text>The Tanzawa Mountains were formed during the late Pliocene. </text>
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          <name>Unit</name>
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              <text>N/A</text>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>Quartz Diorite</text>
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                <text>Plagioclase - Quartz - Diorite</text>
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                <text>Rock Sample:&#13;
The samples color has a white matrix with dark green phenocrysts.  It is phaneritic.  There is evidence of chemical weathering due to the presence of a dark brownish orange film on the sample--may be oxidation.  There is a sandy smooth feeling film above the TMJ-6 tag.  Phenocrysts are medium to coarse grained ranging from 0.1~1cm in length.  It has a rough feel overall.&#13;
&#13;
Thin Section:&#13;
There is tartan twinning on some irregular-shaped plagioclase.  It is a large crystal with intergrowths  and many micro-tartan twinning crystal within it.  Many of the irregular shaped plagioclase have many fractures or scratches in them.  There is some amphibole that intergrew into some augite.&#13;
-Quartz (30%)&#13;
-Augite (25%)&#13;
-Amphibole (25%)&#13;
-Plagioclase (20%)&#13;
-Magnification at 4x/0.10</text>
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                <text>Western Minerals, Inc.</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/10"&gt;Tanzawa Mountains--Metamorphic Suite, Japan&lt;/a&gt;</text>
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                <text>Tanzawa Mountains, Japan - North of South Contact</text>
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            <description>Temporal characteristics of the resource.</description>
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                <text>N/A</text>
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                <text>Purchased from Western Minerals Inc.</text>
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                  <text>The Tanzawa Mountains in Japan were created in an arc-arc collision, when the Izu-Bonin-Mariana Arc was subducted beneath the Honshu Arc. This eventually  accreted into the Tanzawa Mountains.  The samples in this collection were found in and around the Tanzawa Mountains.  The suite includes hornfels, amphibolites, quartz diorite, granophyres, and other basaltic rocks.  The samples range from fine to coarse grained.  An interesting feature found on many of the samples was a flow-like swirl of minerals in the thin section, visible in XPL.  The quartz diorite  samples had crystalline, powdery substances on them, which were analyzed using a Scanning Electron Microscope (SEM). The chemical compositions of the mentioned powdery substances were calcium, aluminum, silicon, and oxygen. </text>
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                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Kawate, S., and Makoto, A., 1998, Petrogenesis of the Tanzawa plutonic complex, central Japan; exposed felsic middle crust of the Izu-Bonin-Mariana Arc: Island Arc, v. 7, p. 342-358, &lt;br /&gt;link: http://dx.doi.org/10.1111/j.1440-1738.1998.00194.x.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper explains the chemical variation and high SiO&lt;sub&gt;2Â &lt;/sub&gt;percentage of rocks within Tanzawa region, and describes in some depth the tectonic events that uplifted the Tanzawa Mountains. Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Kitamura, K., Ishikawa, M., and Arima, M., 2003, Petrological model of the northern Izu-Bonin-Mariana Arc crust; constraints from high-pressure measurements of elastic wave velocities of the Tanzawa plutonic rocks, central Japan: Tectonophysics, v. 371, p.213-221,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1016/S0040-1951(03)00229-4&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper researchs the variations in acoustic impedance between different hornblende-gabbroic rocks from Tanzawa, Japan.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Mikami, K., 1953, Metamorphic rocks in the southeastern margin of the Tanzawa quartz-diorite mass: Science Reports of Yokohama National University, v. 2, p. 34-49&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper studies the chemical analysis of amphibolites resulting from contact metamorphism of the quartz-diorite mass in the Tanzawa Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Tani, K., Dunkley, D. J., Kimura, J., Wysoczanski, R.J., Yamada, K., and Tatsumi, Y.,2010,Â Syncollisional rapid granitic magma formation in an arc-arc collision zone: Evidence from the Tanzawa plutonic complex, Japan:Â Geology [Boulder], v. 38, p.215-218,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1130/G30526.1&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper discusses the collison that exposed the gabbroic rocks of the Tanzawa plutonic complex, and overall gives the reader an in-depth sturctural history of the Tanzawa Mountains.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Yoshimura, T., 1997, Ca-Al silicates in low-grade metavolcanic rocks from southern Tanzawa Mountains, Central Japan: Journal of Mineralogy Petrology and Economic Geology, Â v. 92, p. 363-378, &lt;br /&gt;link: http://dx.doi.org/10.2465/ganko.92.363.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper explains prevalence of greenschist facies within the Tanzawa Mountain region, and gives the mineral composition of rocks from southern region of Tanzawa Mountains.&lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;&lt;br /&gt;&lt;br /&gt;&lt;/p&gt;</text>
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                  <text>The samples were found in the Tanzawa Mountains of Kanto, Japan. &#13;
</text>
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                  <text>The Tanzawa Mountains were formed during the late Pliocene. </text>
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The color of the crystals within the sample is half-white and half-black in color. The internal part of the sample feels rough, but the outside layer of the sample feels more like a fine-grained. This could be due to erosion on the exterior of the sample.  There are dark and white crystals that are â‰¤1cm in length.  There are some areas of small, light green crystal blotches.  Minor chemical weathering has taken place on this sample.&#13;
&#13;
Thin Section:&#13;
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-Clinopyroxene (30%)&#13;
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/10"&gt;Tanzawa Mountains--Metamorphic Suite, Japan&lt;/a&gt;</text>
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                  <text>(TMJ) Quartz-rich Metamorphic Suite -- Tanzawa Mountains, Kanto, Japan</text>
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                  <text>The Tanzawa Mountains in Japan were created in an arc-arc collision, when the Izu-Bonin-Mariana Arc was subducted beneath the Honshu Arc. This eventually  accreted into the Tanzawa Mountains.  The samples in this collection were found in and around the Tanzawa Mountains.  The suite includes hornfels, amphibolites, quartz diorite, granophyres, and other basaltic rocks.  The samples range from fine to coarse grained.  An interesting feature found on many of the samples was a flow-like swirl of minerals in the thin section, visible in XPL.  The quartz diorite  samples had crystalline, powdery substances on them, which were analyzed using a Scanning Electron Microscope (SEM). The chemical compositions of the mentioned powdery substances were calcium, aluminum, silicon, and oxygen. </text>
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              <name>Contributor</name>
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                  <text>Western Minerals, Inc.</text>
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              <name>References</name>
              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
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                <elementText elementTextId="17996">
                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Kawate, S., and Makoto, A., 1998, Petrogenesis of the Tanzawa plutonic complex, central Japan; exposed felsic middle crust of the Izu-Bonin-Mariana Arc: Island Arc, v. 7, p. 342-358, &lt;br /&gt;link: http://dx.doi.org/10.1111/j.1440-1738.1998.00194.x.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper explains the chemical variation and high SiO&lt;sub&gt;2Â &lt;/sub&gt;percentage of rocks within Tanzawa region, and describes in some depth the tectonic events that uplifted the Tanzawa Mountains. Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;&lt;/p&gt;
&lt;p&gt;Kitamura, K., Ishikawa, M., and Arima, M., 2003, Petrological model of the northern Izu-Bonin-Mariana Arc crust; constraints from high-pressure measurements of elastic wave velocities of the Tanzawa plutonic rocks, central Japan: Tectonophysics, v. 371, p.213-221,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1016/S0040-1951(03)00229-4&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper researchs the variations in acoustic impedance between different hornblende-gabbroic rocks from Tanzawa, Japan.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Mikami, K., 1953, Metamorphic rocks in the southeastern margin of the Tanzawa quartz-diorite mass: Science Reports of Yokohama National University, v. 2, p. 34-49&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This paper studies the chemical analysis of amphibolites resulting from contact metamorphism of the quartz-diorite mass in the Tanzawa Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Tani, K., Dunkley, D. J., Kimura, J., Wysoczanski, R.J., Yamada, K., and Tatsumi, Y.,2010,Â Syncollisional rapid granitic magma formation in an arc-arc collision zone: Evidence from the Tanzawa plutonic complex, Japan:Â Geology [Boulder], v. 38, p.215-218,Â &lt;br /&gt;link:Â http://dx.doi.org/10.1130/G30526.1&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper discusses the collison that exposed the gabbroic rocks of the Tanzawa plutonic complex, and overall gives the reader an in-depth sturctural history of the Tanzawa Mountains.Â &lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Yoshimura, T., 1997, Ca-Al silicates in low-grade metavolcanic rocks from southern Tanzawa Mountains, Central Japan: Journal of Mineralogy Petrology and Economic Geology, Â v. 92, p. 363-378, &lt;br /&gt;link: http://dx.doi.org/10.2465/ganko.92.363.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;
&lt;p&gt;This paper explains prevalence of greenschist facies within the Tanzawa Mountain region, and gives the mineral composition of rocks from southern region of Tanzawa Mountains.&lt;/p&gt;
&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;Â &lt;/p&gt;
&lt;p&gt;&lt;br /&gt;&lt;br /&gt;&lt;/p&gt;</text>
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                  <text>The samples were found in the Tanzawa Mountains of Kanto, Japan. &#13;
</text>
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              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
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                  <text>The Tanzawa Mountains were formed during the late Pliocene. </text>
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                <text>Rock Sample:&#13;
The sample color has a cream colored matrix with dark green phenocrysts. The sample contains Laumontite, which is a mineral in the zeolite group.  There is a white talc-like substance on upper part of sample.  Phenocrysts are medium to coarse grained ranging from 1~8mm in length.  There are multiple fractures that span the length of the  sample.  Some of the fractures are filled in with a white talc-like powder.  The sample has an overall rough texture.&#13;
&#13;
Thin Section:&#13;
Small fractures are evident within the thin section.  There are some blue minerals that have a birefringence of 0.004, that are biaxial (-).  It somewhat swirls. &#13;
-Quartz (50-55%)&#13;
-Amphibole (25%)&#13;
-Augite (25%)&#13;
-Magnification at 4x/0.10&#13;
&#13;
Scanning Electron Microscope:&#13;
The white talc like filling found in the fractures of the sample is made up of calcium, aluminum, silicon, and oxygen--this substance could be the Laumontite. </text>
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                <text>1969</text>
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              <elementText elementTextId="10267">
                <text>Western Minerals, Inc.</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/10"&gt;Tanzawa Mountains--Metamorphic Suite, Japan&lt;/a&gt;</text>
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                <text>TMJ-05</text>
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            <description>The method by which items are added to a collection.</description>
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                <text>Purchased from Western Minerals Inc.</text>
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                <text>7/21/1971</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/4ee10b43b24c8c4757ea46f6ecefea71.pdf"&gt;SE Rock Suite&lt;/a&gt;</text>
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            <description>An account of the resource</description>
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              <elementText elementTextId="28679">
                <text>Plagioclase altered to epidote and flaky sericite, rock has undergone slight metamorphism</text>
              </elementText>
            </elementTextContainer>
          </element>
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            <name>Accrual Method</name>
            <description>The method by which items are added to a collection.</description>
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                <text>Purchased from Geoscience Service &amp; Supplies</text>
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                <text>Quartz latite </text>
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                <text>Western Minerals, Inc.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/5e22b0725bdf1cee9c3642dded438a46.pdf"&gt;BB Rock Suite&lt;/a&gt;</text>
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                  <text>(NH) Plutonic Magma Series -- Southwestern New Hampshire</text>
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                  <text>A sampling of the four plutonic stages of the New Hampshire series. This encompasses the Bethlehem Gneiss, the Kinsman Quartz Monzonite, the Spaulding Quartz Diorite and the Concord Granite.  The rocks cover the Mascoma, Sunapee, Mt. Kearsarge, Penacook, Hillsboro, and Concord Quadrangles.  The ages of the series range from 359-411 Ma.</text>
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                  <text>Western Minerals Inc.</text>
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                  <text>Purchased from Western Minerals Inc.</text>
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                  <text>August 1979</text>
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                  <text>Southwestern New Hampshire: Mascoma, Sunapee, Mt. Kearsarge, Penacook, Hillsboro, and Concord Quadrangles</text>
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                  <text>&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Dorais, M.J., 2003, The petrogenesis and emplacement of the New Hampshire Plutonic Suite: American Journal of Science, v. 303, pp. 447-487,Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of each of the four series in the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;/strong&gt;Clark, R.G., and Lyons, J.B., 1986, Petrogenesis of the Kinsman intrusive suite; peraluminous granitiods of western New Hampshire: Journal of Petrology, v. 27, pp. 1365-1393&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of the Kinsman Quartz Monzonite in detail.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Duke, E.F., 1978, Petrology of Spaulding Group tonalites from Penacook Quadrangle, New Hampshire [Ph.D. Thesis], Dartmouth College, 117 p.Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This thesis details the emplacement, formation, and petrology of the Spaulding Quartz Diorite.&lt;/li&gt;
&lt;/ul&gt;
Lathrop, A.S., Blum, J.D., and Chamberlain, C.P., 1996, Nd, Sr and O isotopic study of the petrogeneseis of two syntectonic members of the New Hampshire plutonic series: Contributions to Mineralogy and Petrology, v. 124, pp. 126-138.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the elemental and isotopic analyses of the New Hampshire magma series in order to better understand the petrogenesis of the suite.&lt;/li&gt;
&lt;/ul&gt;
Lyons, J.B., and Livingston, D.E., 1977, Rb-Sr age of the New Hampshire Plutonic Series: Geological Society of America Bulletin, v. 88, pp. 1808-1812&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper uses Rb-Sr isotopic analyses in order to age date the four different members of the New Hampshire magma series.&lt;/li&gt;
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                  <text>&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Dorais, M.J., 2003, The petrogenesis and emplacement of the New Hampshire Plutonic Suite: American Journal of Science, v. 303, pp. 447-487,Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of each of the four series in the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;/strong&gt;Clark, R.G., and Lyons, J.B., 1986, Petrogenesis of the Kinsman intrusive suite; peraluminous granitiods of western New Hampshire: Journal of Petrology, v. 27, pp. 1365-1393&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of the Kinsman Quartz Monzonite in detail.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Duke, E.F., 1978, Petrology of Spaulding Group tonalites from Penacook Quadrangle, New Hampshire [Ph.D. Thesis], Dartmouth College, 117 p.Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This thesis details the emplacement, formation, and petrology of the Spaulding Quartz Diorite.&lt;/li&gt;
&lt;/ul&gt;
Lathrop, A.S., Blum, J.D., and Chamberlain, C.P., 1996, Nd, Sr and O isotopic study of the petrogeneseis of two syntectonic members of the New Hampshire plutonic series: Contributions to Mineralogy and Petrology, v. 124, pp. 126-138.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the elemental and isotopic analyses of the New Hampshire magma series in order to better understand the petrogenesis of the suite.&lt;/li&gt;
&lt;/ul&gt;
Lyons, J.B., and Livingston, D.E., 1977, Rb-Sr age of the New Hampshire Plutonic Series: Geological Society of America Bulletin, v. 88, pp. 1808-1812&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper uses Rb-Sr isotopic analyses in order to age date the four different members of the New Hampshire magma series.&lt;/li&gt;
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                  <text>&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Dorais, M.J., 2003, The petrogenesis and emplacement of the New Hampshire Plutonic Suite: American Journal of Science, v. 303, pp. 447-487,Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of each of the four series in the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;/strong&gt;Clark, R.G., and Lyons, J.B., 1986, Petrogenesis of the Kinsman intrusive suite; peraluminous granitiods of western New Hampshire: Journal of Petrology, v. 27, pp. 1365-1393&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of the Kinsman Quartz Monzonite in detail.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Duke, E.F., 1978, Petrology of Spaulding Group tonalites from Penacook Quadrangle, New Hampshire [Ph.D. Thesis], Dartmouth College, 117 p.Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This thesis details the emplacement, formation, and petrology of the Spaulding Quartz Diorite.&lt;/li&gt;
&lt;/ul&gt;
Lathrop, A.S., Blum, J.D., and Chamberlain, C.P., 1996, Nd, Sr and O isotopic study of the petrogeneseis of two syntectonic members of the New Hampshire plutonic series: Contributions to Mineralogy and Petrology, v. 124, pp. 126-138.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the elemental and isotopic analyses of the New Hampshire magma series in order to better understand the petrogenesis of the suite.&lt;/li&gt;
&lt;/ul&gt;
Lyons, J.B., and Livingston, D.E., 1977, Rb-Sr age of the New Hampshire Plutonic Series: Geological Society of America Bulletin, v. 88, pp. 1808-1812&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper uses Rb-Sr isotopic analyses in order to age date the four different members of the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Dorais, M.J., 2003, The petrogenesis and emplacement of the New Hampshire Plutonic Suite: American Journal of Science, v. 303, pp. 447-487,Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of each of the four series in the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;&lt;strong&gt;Additional Resources:&lt;br /&gt;&lt;/strong&gt;Clark, R.G., and Lyons, J.B., 1986, Petrogenesis of the Kinsman intrusive suite; peraluminous granitiods of western New Hampshire: Journal of Petrology, v. 27, pp. 1365-1393&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the formation of the Kinsman Quartz Monzonite in detail.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Duke, E.F., 1978, Petrology of Spaulding Group tonalites from Penacook Quadrangle, New Hampshire [Ph.D. Thesis], Dartmouth College, 117 p.Â &lt;br /&gt;&lt;ul&gt;&lt;li&gt;This thesis details the emplacement, formation, and petrology of the Spaulding Quartz Diorite.&lt;/li&gt;
&lt;/ul&gt;
Lathrop, A.S., Blum, J.D., and Chamberlain, C.P., 1996, Nd, Sr and O isotopic study of the petrogeneseis of two syntectonic members of the New Hampshire plutonic series: Contributions to Mineralogy and Petrology, v. 124, pp. 126-138.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper describes the elemental and isotopic analyses of the New Hampshire magma series in order to better understand the petrogenesis of the suite.&lt;/li&gt;
&lt;/ul&gt;
Lyons, J.B., and Livingston, D.E., 1977, Rb-Sr age of the New Hampshire Plutonic Series: Geological Society of America Bulletin, v. 88, pp. 1808-1812&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This paper uses Rb-Sr isotopic analyses in order to age date the four different members of the New Hampshire magma series.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/11"&gt;New Hampshire Magma Series&lt;/a&gt;</text>
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