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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>Spotted Spaulding Granite, member of the Spaulding Quartz Diorite.  Part of an irregular sill, not the major facies.  Spotted appearance, extends through more mafic facies.  Thin section contains quartz, alkali feldspar, plagioclase, mica, and garnet.  Hand sample contains quartz, feldspars, mica, and garnet. </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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                <text>Concord Quad, On Highway 202, 1 mile E of the West edge of the Quad.</text>
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                  <text>This collection is composed of igneous volcanic and intrusive rocks from the St. Francois Mountains of Missouri. The variation within the collection can be used to explain the geologic history of the area. The St. Francois Mountains batholith was formed by granitic intrusions into Precambrian rhyolites, tuffs, and breccias. Then basalt, diabase, and porphyritic intrusions cut the granitoids.</text>
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                  <text>Start here:Â &lt;br /&gt;&lt;br /&gt;Bickford, M.E. and Mose, D.G., 1974, Geochronology of Precambrian rocks, St. Francois Mountains, South eastern Missouri: GSA Special Papers 1975, v. 165, p. 1-48 doi: &lt;a href="http://dx.doi.org/10.1130/SPE165-p1" target="_blank"&gt;http://dx.doi.org/10.1130/SPE165-p1&lt;br /&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Early study of the geochronology of the Precambrian rocks within the St. Francois mountains. Provides further insight upon the sequence discussed in the dscription.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Meert, J.G. and Stuckey, W., 2002, Revisiting the paleomagnetism of the 1.476 Ga St. Francois Mountains igneous province, Missouri: Tectonics v. 21, Issue 2, p. 1-19 doi: &lt;a href="http://dx.doi.org/10.1029/2000TC001265%20" target="_blank"&gt;http://dx.doi.org/10.1029/2000TC001265 &lt;br /&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Information acquired from paleomagnestism studies of the St. Francois igneous provence has proven fruitful for determining an acient paleomagnetic pole for Laurentia.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Menuge, J.F, Brewer, T.S., and Seeger, C.M., 2002, Petrogenesis of metaluminous A-type rhyolites from the St. Francois Mountains, Missouri and the Mesoproterozoic evolution of the southern Laurentian Margin: Precambrian Research, volume 113, issues 3-4, p. 269-291 doi: &lt;a href="http//dx.doi.org/10.1016/S0301-9268(01)00211-X%20" target="_blank"&gt;http//dx.doi.org/10.1016/S0301-9268(01)00211-X &lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Trace elemental analysis of Precambrian rocks from the SFM provide insight into the condition of crystallization and the elemental constituents which played a role into the interesting history of this rhyolitic provence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Rohs, R. C, and Van Schmus, W.R., 2006, Isotopic connection between basement rocks exposed in the St. Francois Mountains and the arbucks Mountains southern mid-continent, North America: International Journal of Earth Sciences, volume 96, Issue 4, p. 599-611 &lt;br /&gt;doi: &lt;a href="http://dx.doi.org/10.1007/s00531-006-0123-5" target="_blank"&gt;http://dx.doi.org/10.1007/s00531-006-0123-5&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;&lt;span style="color:#000000;"&gt;Radiometric study of the SFM provence and the Arbuckle mountains of southern Oklahoma suggests a common source.Â &lt;/span&gt;&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Wenner, D. and Taylor Jr., H.P., 1976, Oxygen and hydrogen isotope studies of a Precambian granite-rhyolite terrane, ST. Francois Mountains, southeastern Missouri: Geological Society of America bulletin v. 87, no. 11, p.1587-1598 &lt;br /&gt;doi: &lt;a href="http://dx.doi.org/10.1130/0016-7606" target="_blank"&gt;http://dx.doi.org/10.1130/0016-7606&lt;br /&gt;&lt;/a&gt;
&lt;ul&gt;&lt;li&gt;Isotopic analysis of oxygen isotope content within mineral grains within the Precambrian rhyolitic rocks of the SFM yields data that suggests Precambrian oceans were similar to modern day meteoric oceans.&lt;/li&gt;
&lt;/ul&gt;</text>
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&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Vollmer, F. W., and Walker, J., 2009, The classic Barrovian metamorphic sequence of Dutchess County and its structural and stratigraphic context in the Taconic Orogeny. In Guidebookâ€”New York State Geological Association Meeting, v. 81, p. 11-1.Â &lt;br /&gt;&lt;a href="http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf"&gt;http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf&lt;/a&gt;Â (accessed March 15th, 2015)&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A useful field trip guide across the Barrovian metamorphic sequence of Dutchess county. Good general introduction to the geology of the area.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Keuhner, S.M., and Dilek, Y.R., 1996, Progressive metamorphism of pelitic rocks from protolith to granulite facies, Dutchess County, New York, USA: constraints on the timing of fluid infiltration during regional metamorphism, Journal of Metamorphic Geology, v. 14, p. 163-181. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1046/j.1525-1314.1996.05836.x&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A fairly general look at the progressive metamorphism in Dutchess County by one of the foremost workers in the area.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Knopf, E.B., 1927, Some recent work in the Taconic area: American Journal of Science, v. 41, p. 42-458. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.2475/ajs.s5-14.84.429&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;One of the first articles to describle the Dutchess County rocks as a "classic" Barrovian sequence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Ghent, E.D., Stout, M.Z., 1981, Geobarometry and geothermometry of plagioclase-biotite-garnet-muscovite assemblages, Contributions to Mineralogy and Petrology, v. 76, p. 92-97. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1007/BF00373688&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work constraining the pressure and temperature paths of metamorphism in the sequence through equilibrium assemblages. This work was found to be in agreement with other equilibrium assemblage PT paths.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Dilek, Y.R., and Keuhner, S.M., 1996, Modification of garnet during regional metamorphism in garnet through sillimanite-zone rocks, Dutchess County, New York, American Mineralogist, v. 81, p. 696-705. &lt;a href="http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf"&gt; http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work by Whitney on changes in PTX conditions leading to modification of garnet in the metamorphic sequence. Garnet is widely distributed through the sequence, which makes it a useful marker for tracking these changes.&lt;/li&gt;
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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&#13;
The thin section shows large chloritoid grains with staurolite (an assemblage not in equilibrium). Fine grained muscovite and biotite are also present, along with micro-crystalline quartz and several graphite strings.&#13;
&#13;
This rock is right at the transition between the garnet-staurolite zones in the Barrovian metamorphic sequence (intermediate (increasing) metamorphism).</text>
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                <text>Staurolite Schist</text>
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                <text>Little Falls, MN</text>
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                <text>Mineralogy: quartz, feldspar, biotite, staurolite. Foliated. Foliation caused by biotite, staurolite is porphyroblastic. Biotite-staurolite-schist. Staurolite Zone. </text>
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                    <text>DUCO-9 hand sample of staurolite schist</text>
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                <description>A name given to the resource</description>
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                  <text>(DUCO) Barrovian Metamorphic Sequence -- Dutchess County, New York</text>
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              <name>Contributor</name>
              <description>An entity responsible for making contributions to the resource</description>
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                <elementText elementTextId="17801">
                  <text>Western Minerals, Inc.</text>
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              <description>The method by which items are added to a collection.</description>
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                <elementText elementTextId="17802">
                  <text>Purchased from Western Minerals, Inc.</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                <elementText elementTextId="17809">
                  <text>A classic example of Barrovian-type metamorphism in Dutchess County, NY associated with the Taconic orogeny. A Barrovian metamorphic sequence displays gradual pressure and temperature increase along the metamorphic gradient, and occurs during regional metamorphism. These zones of pressure and temperature increase are recognizable by the characteristic minerals that accompany them. Dutchess County, NY contains an unusually complete sequence.&#13;
&#13;
This collection contains metamorphic rocks from chlorite grade to sillimanite grade in a tight spatial window which records the regional metamorphic gradient increasing  from WNW to ESE. This collection also contains some rocks that mirror the protoliths of the schists and quartzites of the sequence (shales and graywacke). </text>
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              <name>Date</name>
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                  <text>1970</text>
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              <name>Spatial Coverage</name>
              <description>Spatial characteristics of the resource.</description>
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                  <text>Dutchess County, New York</text>
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            <element elementId="116">
              <name>Temporal Coverage</name>
              <description>Temporal characteristics of the resource.</description>
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                <elementText elementTextId="17812">
                  <text>450-430 Ma</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>
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                <elementText elementTextId="17970">
                  <text>&lt;strong&gt;Start Here:&lt;/strong&gt; &lt;br /&gt;Vollmer, F. W., and Walker, J., 2009, The classic Barrovian metamorphic sequence of Dutchess County and its structural and stratigraphic context in the Taconic Orogeny. In Guidebookâ€”New York State Geological Association Meeting, v. 81, p. 11-1.Â &lt;br /&gt;&lt;a href="http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf"&gt;http://www2.newpaltz.edu/~vollmerf/papers/Vollmer_and_Walker_2009_NYSGA.pdf&lt;/a&gt;Â (accessed March 15th, 2015)&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A useful field trip guide across the Barrovian metamorphic sequence of Dutchess county. Good general introduction to the geology of the area.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;Additional Resources:&lt;/strong&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Keuhner, S.M., and Dilek, Y.R., 1996, Progressive metamorphism of pelitic rocks from protolith to granulite facies, Dutchess County, New York, USA: constraints on the timing of fluid infiltration during regional metamorphism, Journal of Metamorphic Geology, v. 14, p. 163-181. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1046/j.1525-1314.1996.05836.x&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;A fairly general look at the progressive metamorphism in Dutchess County by one of the foremost workers in the area.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Knopf, E.B., 1927, Some recent work in the Taconic area: American Journal of Science, v. 41, p. 42-458. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.2475/ajs.s5-14.84.429&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;One of the first articles to describle the Dutchess County rocks as a "classic" Barrovian sequence.Â &lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Ghent, E.D., Stout, M.Z., 1981, Geobarometry and geothermometry of plagioclase-biotite-garnet-muscovite assemblages, Contributions to Mineralogy and Petrology, v. 76, p. 92-97. &lt;a href="http://dx.doi.org/"&gt;http://dx.doi.org/&lt;span&gt;10.1007/BF00373688&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work constraining the pressure and temperature paths of metamorphism in the sequence through equilibrium assemblages. This work was found to be in agreement with other equilibrium assemblage PT paths.&lt;/li&gt;
&lt;/ul&gt;&lt;br /&gt;Whitney, D.L., Mechum, T.A., Dilek, Y.R., and Keuhner, S.M., 1996, Modification of garnet during regional metamorphism in garnet through sillimanite-zone rocks, Dutchess County, New York, American Mineralogist, v. 81, p. 696-705. &lt;a href="http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf"&gt; http://www.minsocam.org/MSA/AmMin/TOC/Articles_Free/1996/Whitney_p696-705_96.pdf&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;Work by Whitney on changes in PTX conditions leading to modification of garnet in the metamorphic sequence. Garnet is widely distributed through the sequence, which makes it a useful marker for tracking these changes.&lt;/li&gt;
&lt;/ul&gt;</text>
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              <text>Barrovian Metamorphic Sequence</text>
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          <description>Number of thin sections associated with this sample</description>
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                <text>Staurolite schist</text>
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                <text>Dutchess Co., NY</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/collections/show/18"&gt;Barrovian Metamorphic Sequence--Dutchess County, New York&lt;/a&gt;</text>
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                <text>Schist with coarse staurolite grains. This outcropping is approximately on the strike of the chloritoid schists (sample 7). Also contains garnet, muscovite, feldspar, and quartz. Presumed to be from the Everett Schist.&#13;
&#13;
The thin section shows staurolite, biotite, muscovite (noticeable by pleochroism differences) and quartz.&#13;
&#13;
This rock is from the staurolite zone in the Barrovian metamorphic sequence (higher intermediate metamorphism).</text>
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                <text>Purchased from Western Minerals Inc.</text>
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                  <text>(LT) Littleton Formation Metamorphic Suite -- New Hampshire </text>
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                <text>Staurolite schist</text>
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                <text>NW outlet of Pearl Lake, NH (SW side of lake);  Near Lisbon, NH;  0.3 miles SW of old dam location.  The dam was removed in 2008.&#13;
N-Central Moosilauke quadrangle map, NH</text>
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            <description>An entity responsible for making contributions to the resource</description>
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              <elementText elementTextId="27822">
                <text>Western Minerals, Inc.</text>
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              <elementText elementTextId="27823">
                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/ab40af99a6356f6acf4cf7553cb67b6a.pdf"&gt;LT Rock Suite&lt;/a&gt;</text>
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            <description>An account of the resource</description>
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              <elementText elementTextId="27824">
                <text>Mica-based schist with porphyroblasts of staurolite.</text>
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          <element elementId="117">
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                <text>Purchased from Western Minerals, Inc.</text>
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              <elementText elementTextId="36678">
                <text>1980</text>
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                  <text>(NM) Northern Michigan Metamorphic Suite -- Michigan</text>
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      <description>A physical material with a mineral composition.</description>
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                <text>NM-18</text>
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                <text>Staurolite schist</text>
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                <text>Kenton, Michigan</text>
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              <elementText elementTextId="28234">
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/4ee10b43b24c8c4757ea46f6ecefea71.pdf"&gt;NWME Rock Suite&lt;/a&gt;</text>
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                <text>NWME-14</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/4ee10b43b24c8c4757ea46f6ecefea71.pdf"&gt;NWME Rock Suite&lt;/a&gt;</text>
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                <text>Some remnants of andalusite</text>
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                <text>Staurolite schist</text>
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                <text>&lt;a href="http://geosciencecollections.milne-library.org/files/original/4ee10b43b24c8c4757ea46f6ecefea71.pdf"&gt;NWME Rock Suite&lt;/a&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>Moslty conglomerates, but partly staurolite rimmed with muscovite</text>
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