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                  <text>This collection consists of 20 samples taken from Panoche Pass, California.  These samples are representative of rocks that can be found in the Franciscan assemblage throughout California.  These rocks made up the accretionary wedge during the Nevadan Orogeny and were accreted onto the west coast of North America. Rocks in this suite range from seafloor sediments all the way to eclogite facies metamorphics.</text>
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                <text>&lt;a href="Êºhttp://www.geosciencecollections.milne-library.org/items/show/162Êº"&gt;Panoche Pass, California Western Minerals Supplemental Materials&lt;/a&gt;</text>
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                  <text>The suite consists of samples from an ophiolite suite that outcrops in 3 locations in the Apennine mountain range in northern Italy.Â  The units are severely imbricated and folded.Â  The units are Cretaceous-Eocene in age.Â  The units consist of ultramafic rock, gabbro and peridotite instrusions, and basaltic magmas.</text>
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                  <text>Northern Apennines, Liguria Region, Italy&lt;br /&gt;Samples 1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12, 13, and 15 are taken from the region around Bargone, Italy&lt;br /&gt;Samples 14, 16, 17, 18, 19, 20, and 21 are taken from the region around Sassello, Italy&lt;br /&gt;Sample 22 is taken from outside Genoa, Italy</text>
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              <name>Date</name>
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                  <text>1982</text>
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              <name>Is Part Of</name>
              <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/" target="_blank"&gt;The Geneseo Geoscience Collection&lt;/a&gt;</text>
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                  <text>NAO-01 to NAO-22</text>
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                  <text>Triassic - Eocene</text>
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              <name>Accrual Method</name>
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                  <text>Purchased by Western Minerals, Inc.</text>
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                  <text>&lt;strong&gt;Start Here:&lt;br /&gt;&lt;/strong&gt;&lt;span class="cit-auth cit-auth-type-author"&gt;Lagabrielle, Y.,&lt;/span&gt;&lt;span class="cit-sep cit-sep-two-item-separator"&gt;Â and Cannat, M., 1990, &lt;/span&gt;&lt;span class="cit-title"&gt;Alpine Jurassic ophiolites resemble the modern central Atlantic basement: Geology, v. 18, p. 319-322&lt;br /&gt;&lt;/span&gt;Link:Â &lt;a href="http://geology.geoscienceworld.org/content/18/4/319.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This fairly short article gives some insight into the development of the North Apennine Ophiolites with a fairly recent view on the matter.&lt;/li&gt;
&lt;/ul&gt;&lt;strong&gt;&lt;br /&gt;Additional Resources&lt;/strong&gt;&lt;strong&gt;:&lt;/strong&gt;&lt;br /&gt;Garuti, G., and Zaccarini, F., 2005, Minerals of Au, Ag and U in Volcanic-Rock-Associated Massive Sulfide Deposits of the Northern Apennine Ophiolite, Italy: The Canadian Mineralogist, v. 43, p. 935-950&lt;br /&gt;DOI: &lt;a href="http://dx.doi.org/10.2113/gscanmin.43.3.935" target="_blank"&gt;10.2113/gscanmin.43.3.935&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the elemental composition of the North Apennine Ophiolite sequence and uses that to determine previous geologic events.&lt;/li&gt;
&lt;/ul&gt;
Garuti, G., Zaccarini, F., Scacchetti, M., and Bartoli, O., 2011, The Pb-rich sulfide veins in the Boccassuolo ophiolite: Implications for the geochemical evolution of the hydrothermal activity across the ocean-continent transition in the Ligurian Tethys (Northern-Apennine, Italy): Lithos, v. 124, p. 243-254&lt;br /&gt;DOI:Â &lt;a title="10.1016/j.lithos.2010.11.006" href="http://dx.doi.org/10.1016/j.lithos.2010.11.006" target="_blank"&gt;10.1016/j.lithos.2010.11.006&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article explores the chemical composition of the ophiolite sequence under a different name and ties it into the formation history.&lt;/li&gt;
&lt;/ul&gt;
Garzanti, E., Canclini, S., Foggia, F.M., and Petrella, N., 2002, Unraveling Magmatic and Orogenic Provenance in Modern Sand: The Back-Arc Side of the Apennine Thrust Belt, Italy: Journal of Sedimentary Research, v. 72, p. 2-17&lt;br /&gt;DOI:Â &lt;a title="10.1306/051801720002" href="http://dx.doi.org/10.1306/051801720002" target="_blank"&gt;&lt;span&gt;10.1306/051801720002&lt;/span&gt;&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into great detail on the provenance characteristics for a number of sands. including sands originating from the North Apennine Ophiolite sequence.&lt;/li&gt;
&lt;/ul&gt;
Cibin, U., Spadafora, E., Zuffa, G.G., and Castellarin, A., 2001, Continental collision history from arenites of episutural basins in the Northern Apennines, Italy: Geological Society of America Bulletin, v. 113, p. 4-19&lt;br /&gt;Link: &lt;a title="GeoScienceWorld" href="http://bulletin.geoscienceworld.org/content/113/1/4.full.pdf" target="_blank"&gt;GeoScienceWorld&lt;/a&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;This article goes into detail about the deformations experienced by the North Apennine Ophiolites after the Eocene.&lt;/li&gt;
&lt;/ul&gt;</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/items/show/34"&gt;Northern Apennines Ophiolites Western Minerals Supplementary Information&lt;/a&gt;</text>
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                <text>Basalt</text>
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                  <text>Samples were collected from various locations on the islands of Hawaii and Oahu. </text>
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                  <text>Purchased from Western Minerals, Inc. </text>
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                  <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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                <text>Hand Sample: On cut face, aphanitic, gray basalt with light colored phaneritic crystals (~0.1 cm in size). Subparallel fractures noted across sample. Exterior of sample has been heavily weathered, resulting in the red and orange discoloration.</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>
              <description>An entity responsible for making contributions to the resource</description>
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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>
              <elementTextContainer>
                <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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              <description>Spatial characteristics of the resource.</description>
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                  <text>The samples were found in the Tanzawa Mountains of Kanto, Japan. &#13;
</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>
                </elementText>
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                <text>Rock Sample:&#13;
The sample is brown to white to green in color. It is porphyritic and has foliations that fan out.  There are also wide fractures (â‰¤1mm in length).  There is a brownish orange coating which is evidence of chemical weathering.  There are some holes around the oxidation zones which suggest deep weathering by a liquid.  The sample does not react with acid.  It has a silty yet jagged texture.&#13;
&#13;
Thin Section:&#13;
There are micro-fractures that are non-uniform.  The sample is holocrystalline.  The majority of the matrix intergrows within many of the larger crystals.  The rest of the thin section has a matrix that cannot be identified from a standard microscope.&#13;
-Chlorite (30%)&#13;
-Muscovite (10%)&#13;
-Serpentine (5%)&#13;
-Epidote (5%)&#13;
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              <elementText elementTextId="10184">
                <text>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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              <name>References</name>
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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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                  <text>The Tanzawa Mountains were formed during the late Pliocene. </text>
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                <text>Rock Sample:&#13;
The overall matrix is a dark green blue but there are many different colored clasts that give it a mixture of colors.  The color of the clasts range from brick red, pink, white, and green (non-reactant to acid). The texture of the rock is silty. There are massive, very coarse grained clasts that are up to 3cm in length.  There are clasts within other clasts.  There is one fracture spanning across the rock.  There is evidence of  minor chemical weathering.  The overall shape of the rock is an octahedral.  It has eight faces and forms into a jagged ball.  &#13;
&#13;
&#13;
Thin Section:&#13;
The matrix has many globular, navy blue crystals, with an outer shell around them (XPL).   Some plagioclase crystals experience tartan twinning.  Also,  some of the plagioclase is intergrown within other plagioclase crystals.  The matrix has a variety of colors in XPL (navy blue, yellow, and brown in various shades), and makes up the majority of the thin section.  There are some smaller dark blue crystals that are in the shape of a half spoked wheel (under XPL).  There are some very fine grained sized glass crystals within the thin section.   &#13;
-Plagioclase (50%)&#13;
-Quartz (20%)&#13;
-Pyroxene (10%)&#13;
-Olivine (10%)&#13;
-Biotite (10%)&#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>&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>These samples were taken from the Shelburne area of Nova Scotia. This is the southeastern shore of Nova Scotia. </text>
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                <text>Macroscopic: Grey massive biotite, muscovite granite. Overall white and grey color. Only slightly weathered.Â  Microscopic: Abundant in alkali feldspar, plagoclase, quartz and mica. Thin section pictures in XPL unless otherwise noted in the title of the picuture. Thin sections are 3mm across.</text>
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                <text>&lt;a href="http://www.geosciencecollections.milne-library.org/collections/show/14"&gt;Pelitic Metamorphic Suite, Shelburne, Nova Scotia&lt;/a&gt;</text>
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                <text>Biotite is variable in amount, but it is always evenly distributed</text>
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