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                  <text>&lt;strong&gt;Start Here&lt;/strong&gt;: &lt;br /&gt;Currie, K.L., Whalen, J.B., Davis, W.J., Longstaffe, F.J., and Cousens, B.L., 1998, Geochemical evolution of peraluminous plutons in southern Nova Scotia, Canada-a pegmatite-poor suite:Lithos, v. 44, p.117-140, doi:&lt;a href="http://dx.doi.org/10.1016/S0024-4937(98)0051-6"&gt;10.1016/S0024-4937(98)0051-6&lt;/a&gt; â€¢ This paper gives information on the geology of southern Nova Scotia and provides a strong example for the rock suite present. &lt;strong&gt;&lt;br /&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;: &lt;br /&gt;&lt;br /&gt;Cambell, D., Shimeld, J., Deptuck, M.E., Mosher, J.C., Seismic Stratigraphic framework and depositional history of a large Upper Cretaceous and Cenozoic depocenter off southwest Nova Scotia, Canada: Marine and Petroleum Geology, v. 65, p. 22-42, doi: &lt;a href="http://dx.doi.org/10.1016/j.marpetgeo.2015.03.016"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1016/j.marpetgeo.2015.03.016&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;Â  &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful as it outlines the stratrigraphy and depositional history of the region. This is key in understanding much of the regions history and allows geologists to better understand what exactly is metamorphosed and why.&lt;br /&gt;&lt;br /&gt;Greenough, J.D., Jone, M.L., and Mossman, D.J., 1989, The Sr isotopic composition of early Jurassic mafic rocks of Atlantic Canada: Implications for assimilation and injection mechanism affecting mafic dykes: Chemical Geology, v. 80, p. 17-26, doi: &lt;a href="http://dx.doi/org/10.1016/0168-9622(89)90044-4"&gt;10.1016/0168-9622(89)90044-4&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for describing the dykes in Atlantic Canada as well as injections that formed much of the suite. &lt;br /&gt;&lt;br /&gt;Merle, R., Marzoli, A., Reisberg, L., Bertrand, H., Nemchin, A., Chiaradia, M., Callegaro, S., Jourdan, F., Bellieni, G., Kontak, D., Puffer, J., Mchone, J., 2014, Sr, Nd, Pb, and Os isotope systematics of CAMP tholeiites from Eastern North America (ENA): Evidence of a subduction-enriched mantle source: Journal of Petrology, v. 55, p. 133-180, doi: &lt;a href="http://dx.doi.org/10.1093/petrology/egt063"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1093/petrology/egt063&lt;/span&gt;&lt;/span&gt;&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper outline the subduction in the region as well as outling the petrologic controls on the region, specifically with an eye on Seldon, Nova Soctia. this is particularly imporant when considering the pegmatites in the suite and other igneous bodies.&lt;br /&gt;&lt;br /&gt;Muecke, G. K., Pride, C., and Sarkar, P., 1979, Rare-earth element geochemistry of regional metamorphic rocks: Physics and Chemistry of the Earth, v. 11, p. 449-464, doi:&lt;a href="http://dx.doi.org/10.1016/0079-1946(79)90043-0"&gt;10.1016/0079-1946(79)90043-0&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for as it describes the geochemistry of the suite on a large scale and provides reference for what should be seen in the suite.</text>
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                  <text>Samples are Cambrian to lower Ordovician greywackes and shales that were regionally metamorphosed and intruded by granites during the Devonian. &#13;
Samples taken in 1988. </text>
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                  <text>&lt;strong&gt;Start Here&lt;/strong&gt;: &lt;br /&gt;Currie, K.L., Whalen, J.B., Davis, W.J., Longstaffe, F.J., and Cousens, B.L., 1998, Geochemical evolution of peraluminous plutons in southern Nova Scotia, Canada-a pegmatite-poor suite:Lithos, v. 44, p.117-140, doi:&lt;a href="http://dx.doi.org/10.1016/S0024-4937(98)0051-6"&gt;10.1016/S0024-4937(98)0051-6&lt;/a&gt; â€¢ This paper gives information on the geology of southern Nova Scotia and provides a strong example for the rock suite present. &lt;strong&gt;&lt;br /&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;: &lt;br /&gt;&lt;br /&gt;Cambell, D., Shimeld, J., Deptuck, M.E., Mosher, J.C., Seismic Stratigraphic framework and depositional history of a large Upper Cretaceous and Cenozoic depocenter off southwest Nova Scotia, Canada: Marine and Petroleum Geology, v. 65, p. 22-42, doi: &lt;a href="http://dx.doi.org/10.1016/j.marpetgeo.2015.03.016"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1016/j.marpetgeo.2015.03.016&lt;/span&gt;&lt;/span&gt;&lt;/a&gt;Â  &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful as it outlines the stratrigraphy and depositional history of the region. This is key in understanding much of the regions history and allows geologists to better understand what exactly is metamorphosed and why.&lt;br /&gt;&lt;br /&gt;Greenough, J.D., Jone, M.L., and Mossman, D.J., 1989, The Sr isotopic composition of early Jurassic mafic rocks of Atlantic Canada: Implications for assimilation and injection mechanism affecting mafic dykes: Chemical Geology, v. 80, p. 17-26, doi: &lt;a href="http://dx.doi/org/10.1016/0168-9622(89)90044-4"&gt;10.1016/0168-9622(89)90044-4&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for describing the dykes in Atlantic Canada as well as injections that formed much of the suite. &lt;br /&gt;&lt;br /&gt;Merle, R., Marzoli, A., Reisberg, L., Bertrand, H., Nemchin, A., Chiaradia, M., Callegaro, S., Jourdan, F., Bellieni, G., Kontak, D., Puffer, J., Mchone, J., 2014, Sr, Nd, Pb, and Os isotope systematics of CAMP tholeiites from Eastern North America (ENA): Evidence of a subduction-enriched mantle source: Journal of Petrology, v. 55, p. 133-180, doi: &lt;a href="http://dx.doi.org/10.1093/petrology/egt063"&gt;&lt;span class="paddingR15"&gt;&lt;span&gt;10.1093/petrology/egt063&lt;/span&gt;&lt;/span&gt;&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper outline the subduction in the region as well as outling the petrologic controls on the region, specifically with an eye on Seldon, Nova Soctia. this is particularly imporant when considering the pegmatites in the suite and other igneous bodies.&lt;br /&gt;&lt;br /&gt;Muecke, G. K., Pride, C., and Sarkar, P., 1979, Rare-earth element geochemistry of regional metamorphic rocks: Physics and Chemistry of the Earth, v. 11, p. 449-464, doi:&lt;a href="http://dx.doi.org/10.1016/0079-1946(79)90043-0"&gt;10.1016/0079-1946(79)90043-0&lt;/a&gt; &lt;br /&gt;&lt;br /&gt;â€¢ This paper is useful for as it describes the geochemistry of the suite on a large scale and provides reference for what should be seen in the suite.</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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              <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;
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It has rough sandy feel to it.  There is some major chemical weathering.  There is some white residue on the surface which has a minor reaction to Hydrochloric acid. &#13;
-Hardness = 5.5&#13;
-Streak = The dark spots on the sample had a dark-brownish to yellow streak, while the blue part of the sample did not have a streak. &#13;
&#13;
Thin Section:&#13;
Oxidation is shown in the thin section.  The matrix has blue swells. Some of the pyroxene crystals are very fine grained and show exhibit a "swirly" texture.  The plagioclase crystals exhibit some crytsal-zoning.  The sample is hypocrystalline. Others are fractured and filled in with very fine grained matrix.  There are large fractures within the pyrozene crystals as well.  Matrix is intergrown into coarse grained quartz.  &#13;
-Quartz (40%)&#13;
-Pyroxene (25%)&#13;
-K-feldspar (20%)&#13;
-Plagioclase (15%)&#13;
-Magnification at 4x/0.10&#13;
&#13;
Scanning Electron Microscope:&#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-18</text>
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                <text>Tanzawa Mountains, Japan  Rifle range and Inn near Kajaka (SE side of intrusive)</text>
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                <text>Purchased from Western Minerals Inc.</text>
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                <text>BB-29</text>
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            <description>A name given to the resource</description>
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                <text>Andesite volcanics</text>
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                <text>Boulder, Montana</text>
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                <text>1981</text>
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                <text>Western Minerals, Inc.</text>
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            <description>A related resource in which the described resource is physically or logically included.</description>
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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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            <description>An account of the resource</description>
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                <text>possibly crystal tuff</text>
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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 Western Minerals, Inc.</text>
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                <name>Title</name>
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            <element elementId="50">
              <name>Title</name>
              <description>A name given to the resource</description>
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                  <text>(HA) Volcanic Phenomena Suite -- The Hawaiian Islands of Hawaii and Oahu</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                <elementText elementTextId="17793">
                  <text>These 31 samples comprise a collection of volcanic rocks associated with the hot-spot volcanism of the Hawaiian Islands. Samples were collected from various locations across the islands of Hawaii and Oahu. The collection contains samples of primarily tholeiitic &amp; alkalic basalts, pumice, scoria, oceanite, and hawaiite. </text>
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              </elementTextContainer>
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            <element elementId="37">
              <name>Contributor</name>
              <description>An entity responsible for making contributions to the resource</description>
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                <elementText elementTextId="17794">
                  <text>Western Minerals, Inc.</text>
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              <name>Date</name>
              <description>A point or period of time associated with an event in the lifecycle of the resource</description>
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                  <text>1969</text>
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              <name>Identifier</name>
              <description>An unambiguous reference to the resource within a given context</description>
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                  <text>HA-1 - HA-31</text>
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              <name>Spatial Coverage</name>
              <description>Spatial characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17821">
                  <text>Samples were collected from various locations on the islands of Hawaii and Oahu. </text>
                </elementText>
              </elementTextContainer>
            </element>
            <element elementId="116">
              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17822">
                  <text>Samples formed from Holocene eruptions of the past 300 years. Dated samples formed between 1750 and 1960. </text>
                </elementText>
              </elementTextContainer>
            </element>
            <element elementId="117">
              <name>Accrual Method</name>
              <description>The method by which items are added to a collection.</description>
              <elementTextContainer>
                <elementText elementTextId="17823">
                  <text>Purchased from Western Minerals, Inc. </text>
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            </element>
            <element elementId="109">
              <name>References</name>
              <description>A related resource that is referenced, cited, or otherwise pointed to by the described resource.</description>
              <elementTextContainer>
                <elementText elementTextId="17997">
                  <text>&lt;p&gt;&lt;strong&gt;Start here:&lt;br /&gt;&lt;/strong&gt;Macdonald, G.A., 1949, Petrography of the Island of Hawaii, U.S.G.S. Prof. Paper 214 D&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article is a part of the general investigation of the island of Hawaii by the United States Geologic Survey. The paper describes the dominant volcanoes of the island of Hawaii (from which most of the suite's samples were collected) and describes the petrographic phenomena observed and geochemical analyses of volcanic rocks.Â &lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Ho, R.A., Garcia, M.O., 1988, Origin of differentiated lavas at Kilauea Volcano, Hawaii; implications from the 1955 eruption: Bulletin of Volcanology, v. 50, p. 35-46.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes a study of lava flows from the 1955 eruption of the Kilauea Volcano on the island of Hawaii to evaluate models of crystal fractionation or magma mixing as the processes forming differentiated magmas. Through geochemical analyses, the study concluded that crystal fractionation resulted in the observed differentiation of lavas.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Hofman, A.W., Farnetani, C.G., 2013, Two Views of Hawaiian Plume Structure: Geochemistry, Geophysics, Geosystems, v.14, p. 5308-5322, doi:10.1002/2013GC004942&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article presents two opposing views of the source of magmas for the Hawaiian volcanoes. Both views favor a deep mantle source, but try to explain differences in isotopic compositions.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Macdonald, G.A., 1968, Composition and origin of Hawaiian LavasÂ &lt;em&gt;in&lt;/em&gt; GSA Memoirs 1968, p. 477-522&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article provides geochemical analysis of major elements as well as determinations of minor elements of volcanic rocks from the island of Hawaii. The article describes the three major rock types - tholeitic, alkalic, and nephelinic - and concludes these rock suites are chemically intergradational and are likely derived from crystal differentiation of a single parent magma.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;br /&gt;Moore, J.G., Clague, D.A., 1992, Volcano growth and evolution of the Island of Hawaii: Geologic Society of America Bulletin, v. 104, p. 1471-1484&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article proposes a chronologic evolution of the island of Hawaii, from where many of the suite's samples were collected.&lt;/li&gt;
&lt;/ul&gt;</text>
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          <name>Number of Thin Sections</name>
          <description>Number of thin sections associated with this sample</description>
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                <text>Ankaramite</text>
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              <elementText elementTextId="15391">
                <text>Ankaramites are dark porphyritic basalts that contain abundant pyroxene and olivine phenocrysts. Lesser amounts of biotite, and plagioclase may also be present. </text>
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                <text>Hand Sample: Aphanitic dark gray vesicular Ankaramite. Sample contains abundant vesicles ranging in size from less than 0.05cm to 0.8cm. Sample also contains numerous larger crystals with iridescent luster ranging in size from 0.1cm to 0.8cm. Phenocrysts of olivine approximately 0.2cm in diameter can also be found throughout the sample.</text>
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                <text>Thin Section: Groundmass made up of microcrystals of clinopyroxenes, glass, plagioclase. Phenocrysts of olivine and pyroxenes are present in addition to some accessory biotite grains. </text>
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                <text>HA-19</text>
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                <text>Western Slope of Mauna Kea - Island of Hawaii&#13;
Sample collected from a roadcut  on Kamuela-Kona Road 2.2 miles north of Popoo Gulch</text>
              </elementText>
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                <text>Volcanic Phenomena Suite - The Hawaiian Islands of Hawaii and Oahu</text>
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              <elementText elementTextId="18557">
                <text>Sample collected in January, 1969.</text>
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                <text>Ano Nuevo, Calif.</text>
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                <text>Ano Nuevo, CA Quadrangle</text>
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                <text>Army Map Service</text>
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                <text>1948</text>
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                  <text>(ADK) Anorthosite-Charnockite and Metamorphic Suite --&#13;
 Adirondack Mountains, New York</text>
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                  <text>The Adirondack Mountains of northern New York State are underlain by approximately 20,000 square miles of complexly deformed, high grade metamorphic rocks which are believed to represent a southern outlier of the much larger Grenville Province.The Adirondacks can be divided into the "Lowlands" and the "Highlands" . The Lowlands comprise the northwestern quarter of the belt and are characterized by amphibolite facies metamorphism. The Highlands appear to consist entirely of granulite facies rocks.  All rocks in this suite have been collected from the Highlands and predominantly from the southern quarter of the Adirondacks.  &#13;
&#13;
This suite of rocks is designed to be representative of the Highlands in general. Therefore it includes both metasedimentary and metaigneous rocks.  The latter are very common throughout the Adirondacks and contain the often-discussed anorthosite-charnockite suite of rocks. Almost all rocks in the Adirondack Highlands are strongly foliated. This is the result of intense polyphase deformation that has affected this area.&#13;
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                  <text>&lt;strong&gt;Start here:Â &lt;br /&gt;&lt;/strong&gt;McLelland, J., and Selleck, B.W.,2011,Â Megacrystic Gore Mountain-type garnets in the Adirondack Highlands; age, origin, and tectonic implications:Geosphere, v.7, no. 5, p.1194-1208, doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00683.1" target="_blank"&gt;10.1130/GES00683.1&lt;/a&gt;.&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article describes the formation of the megacrystic garnet amphibolites in the Gore Mountain section of the Adirondack Mountains. The authors conclude that three main factors influenced the garnet development: collapse of the Ottawan orogeny, intrusion of Lyon Mountain Granite, and fluid-related alteration at high temperature.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;&lt;strong&gt;Additional resources:&lt;br /&gt;&lt;/strong&gt;McLelland, J.M., Bickford, M.E., Hill, B.M., Clechenko, C.C., Valley, J.W., and Hamilton, M.A., 2004,Â Direct dating of Adirondack Massif anorthosite by U-Pb SHRIMP analysis of igneous zircon; implications for AMCG complexes:Â Geological Society of America Bulletin, v.116, no. 11-12, p.1299-1317, doi:Â &lt;a href="http://dx.doi.org/10.1130/B25482.1" target="_blank"&gt;10.1130/B25482.1&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes techniques used to more accurately date the Adirondack Massif anorthosite.The authors concluded that the massifsÂ &lt;span&gt;constitute a single, composite anorthosite-mangerite-charnockite-granite (AMCG) suite intruded at ca. 1155 Ma. Although the rock suite is considered to be coeval, the authors conclude the rocks are not comagmatic.&lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Bickford, M.E., Spear, F., and Storm, L., 2002, Geology and geochronolgy of the eastern Adirondacks inÂ &lt;span&gt;New England Intercollegiate Geological Conference, 94th, New York State Geological Association 74th: guidebook for field trips in New York and Vermont : Lake George, New York&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This field trip guide provides for nine stops in the eastern Adirondacks. It also include some thin sections images and zircon images from sample rocks of the field trip stops.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Daly, J.S., and McLelland, J.M., 1996,Â The Grenville orogenic cycle (ca. 1350-1000 Ma); an Adirondack perspective: Tectonophysics, v.265, issue 1-2, p.1-28, doi: &lt;a href="http://dx.doi.org/10.1016/S0040-1951(96)00144-8" target="_blank"&gt;10.1016/S0040-1951(96)00144-8&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article provides a detailed geochronological account of the Grenville orogeny (ca. 1350-1000 Ma) with emphasis on the impact it had on the formation of the Adirondack Mountains.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;McLelland, J., Lewis, A., and Moore, L., 1994,Â Composition and petrogenesis of oxide-, apatite-rich gabbronorites associated with Proterozoic anorthosite massifs: examples from the Adirondack Mountains, New York: Contributions to Mineralogy and Petrology, v.116, p.225-238, doi:Â &lt;a href="http://dx.doi.org/10.1007/BF00310702" target="_blank"&gt;10.1007/BF00310702&lt;/a&gt;.&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article investigates the occurence of oxide-, apatite-rich gabbronorites with anorthosite massifs of the Adirondacks. The authors describe a multilple-step process of plagioclase crystal fractionation that ultimately leads to high concentrations of P, Fe, and Ti.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;New York State Geological Survey&lt;br /&gt;&lt;a href="http://www.nysm.nysed.gov/nysgs/nygeology/mineralogy/adirondacks/index.html"&gt;http://www.nysm.nysed.gov/nysgs/nygeology/mineralogy/adirondacks/index.html&lt;br /&gt;&lt;/a&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;The NYS Geological Survey is a division of the New York State Museum system. This web page provides some details about the Adirondack Highlands and pictures of various minerals found in this region.&lt;/li&gt;
&lt;/ul&gt;&lt;p&gt;Regan, S.P., Chiarenzelli, J.R., McLelland,Â J.M., and Cousens, B. L., 2011,Â Evidence for an enriched asthenospheric source for coronitic metagabbros in the Adirondack Highlands: Geosphere, v.7, issue 3, p.&lt;span&gt;Â 694-709, doi:Â &lt;a href="http://dx.doi.org/10.1130/GES00629.1" target="_blank"&gt;10.1130/GES00629.1&lt;/a&gt;.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;
&lt;ul&gt;&lt;li&gt;This article describes the formation of coronitc metagabbros through tectonic processes involving the asthenosphere. Through geochemical and isotopic analyses, the authors provide a timeline of tectonic and petrologic events that supports an asthenospheric source for coronitic metagabbros.&lt;/li&gt;
&lt;/ul&gt;</text>
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                  <text>The Adirondack Mountains were formed approximately 1.1- 1.3 billion years ago during the Grenville Orogeny (Precambrian eon, Proterozic era).</text>
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                <text>Adirondack Highlands-collected from a road cut on NY Route 30, 1/2 mile south of junction old route 30 and about 2 miles north of junction NY Route 8.</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/7"&gt;Anorthosite-Charnockite and Metamorphic Suite-Adirondack Mountains, New York&lt;/a&gt;</text>
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                <text>The specimen was collected from the Oregon Dome Massif. The Oregon Dome is similar in all respects to the anorthosites described and analyzed by Buddington (1939) for the Adirondack High Peaks region (Marcy Massif). Texturally, the present specimens are partly granulated and are fairly typical of Adirondack anorthosites situated near the margins of the massifs. Of particular interest in this specimen is the occurrence of garnet. In general, this rims both oxides, usually ilmenite and clinopyroxene (and sometimes cored by orthopyroxene). The assemblage is typical of garnet-clinopyroxene subfacies of the granulite (deWaard, 1965).&#13;
&#13;
The following information is from the original OCR document: The reactions producing this assemblage have been discussed by McLelland and Whitney, "Origin of Garnet in the Anorthosite-Charnockite Suite of the Adirondacks" 1977, Contributions to Mineralogy and Petrology, v. 60, p.161-181.&#13;
Thin section shows plagioclase and orthopyroxene.</text>
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